Recommended citation

Sauchyn, D., Davidson, D., and Johnston, M. (2020): Prairie Provinces; Chapter 4 in Canada in a Changing Climate: Regional Perspectives Report, (ed.) F.J. Warren, N. Lulham and D.S. Lemmen; Government of Canada, Ottawa, Ontario.

Collaborating Lead Authors

  • David Sauchyn, PhD (Director, Prairie Adaptation Research Collaborative and Professor of Geography and Environmental Studies, University of Regina)
  • Debra Davidson, PhD (Professor, Department of Resource Economics and Environmental Sociology, University of Alberta)
  • Mark Johnston, PhD (Senior Research Scientist, Environment Division, Saskatchewan Research Council)

Contributing Authors

  • Mike Flannigan, PhD (Professor, Department of Renewable Resources, University of Alberta)
  • Amber Fletcher, PhD (Associate Professor, Department of Sociology & Social Studies, University of Regina)
  • Kendra Isaac (Manager of Adaptation, Alberta Environment and Parks)
  • Suren Kulshreshtha, PhD (Professor, Department of Agricultural and Resource Economics, University of Saskatchewan)
  • Twyla Kowalczyk (Integrated Water Management, Southern Alberta Institute of Technology, (previously Climate Change Engineer, Water Resources, City of Calgary))
  • Ian Mauro, PhD (Principal, Richardson College for the Environment, and Co-Director, Prairie Climate Centre, University of Winnipeg)
  • Jeremy Pittman, PhD (Assistant Professor, School of Planning, University of Waterloo)
  • Maureen G. Reed, PhD (Professor and UNESCO Co-Chair in Biocultural Diversity, Sustainability, Reconciliation and Renewal, School of Environment and Sustainability, University of Saskatchewan)
  • Richard Schneider, PhD (Research Associate, Biological Sciences, University of Alberta)
  • Megan Van Ham, (Leader Regional Program, Watershed Planning, City of Calgary)
  • Elaine Wheaton, PhD (Adjunct Professor, University of Saskatchewan and Emeritus Researcher, Saskatchewan Research Council)
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Key Messages

Prairie ecosystems will shift and transform as the climate warms

As species respond to climate change, large regions of boreal forest could transition to aspen parkland and grassland ecosystems, while entire mountain ecosystems could disappear. Although biodiversity could increase overall, some species will be lost if the rate of warming exceeds their ability to adapt. Adaptation interventions are based mainly on standard conservation strategies—such as reduction of anthropogenic and other stressors and disturbances—and minimizing barriers to movement.

Floods, drought and wildfires are getting worse

Extreme weather events of amplified severity will likely be the most challenging consequence of climate change in the Prairie Provinces. The impacts of flooding, drought and wildfire in recent years are unprecedented, and climate models suggest an increased risk of these events in the future. Provincial and municipal governments have responded by proposing policies, structures and practices to reduce the impacts of future extreme weather events.

Collaborative water management reduces negative impacts

Regional land-use policy and planning, as well as emergency preparedness, are critical for reducing the impacts of flooding and drought in the Prairie provinces. Collaboration is needed among all levels of government, and with stakeholders such as watershed stewardship groups, rural municipalities and conservation districts, to implement these adaptation measures and to promote practices that prevent or minimize adverse effects of water excesses and shortages.

Climate change brings both benefits and threats to agriculture

Prairie agriculture, particularly crop production, may benefit from higher temperatures and a longer growing season. Achieving net benefits will require adaptation to limit the impacts of climate extremes, including on water availability, and the increased risk of pests, vector-borne diseases and invasive species. Although agricultural producers are highly adaptable to fluctuations in weather and climate, barriers to adaptation include limited information and awareness of climate change impacts, combined with limited financial resources and institutional support.

Social groups have unique vulnerabilities and strengths

The impacts of climate change may exacerbate existing societal inequities, especially among Indigenous peoples, women, people of low socio-economic status, youth and the elderly. Public policy and adaptation planning should consider the unique vulnerabilities and strengths of these social groups, and also the means by which race, age, gender and poverty amplify vulnerability or resilience to climate hazards.

Adaptation planning helps to reduce climate risks

Cities are at the forefront of adaptation and resilience planning in the Prairie provinces. While governments and businesses have begun to assess climate risks and develop adaptation strategies, few plans and policies consider future climate risks, leaving some firms, governments and sectors unprepared. Best practices for assessing the effectiveness of adaptation include meaningful reporting of progress towards achieving climate-resilient communities and local economies.

Foreword

Three years ago, when we started working on Canada’s national assessment process, Canada in a Changing Climate: Advancing our Knowledge for Action, we could never have imagined how different the world would be when we released this first chapter. Over the past eight months, we have lived through rapid and unprecedented change as the global population has struggled to respond to the COVID-19 pandemic. All aspects of our lives have been affected—our health and well-being, social connections, jobs, economic stability and more.

Although dealing with the COVID-19 pandemic has dominated the world’s attention, climate change remains firmly embedded in global, national and sub-national dialogues. Indeed, while we are still trying to understand the pandemic shocks that are rippling through our social, economic and environmental systems, some encouraging insights are emerging with respect to responding to climate change. The response to COVID-19 has shown that once individuals, businesses and governments understand the risks, they are willing to make major changes to protect lives and livelihoods, even in the face of uncertainty. It has also demonstrated the advantages that can be realized through cooperation, the progress that can be achieved through aligned efforts, and the critical role that the private sector and civil society play in responding to global challenges.

There is now abundant research indicating that the window to take action to avoid severe climate change impacts is rapidly closing. The research also suggests that current efforts to adapt are not enough to prevent the rapidly accelerating human and financial losses from current and future climate change impacts. Urgent action is needed to reduce greenhouse gas emissions and increase our resilience to climate change through adaptation. Our decisions and actions today will determine our ability to survive and thrive under a changing climate. Informed decisions, based on the best available science and knowledge, are imperative.

Within this context, we are pleased to release the Prairie Provinces chapter of the Regional Perspectives Report. This report, led by Natural Resources Canada, is part of Canada’s national assessment process, Canada in a Changing Climate: Advancing our Knowledge for Action. The chapter assesses climate change impacts and adaptation in Canada’s Prairie Provinces. It is structured around six key messages, which reflect the priorities of the region, as determined through a series of scoping activities and engagement with key stakeholders and partners. The key messages focus on shifting ecosystems, extreme weather events, water management, agriculture, social considerations and the need for enhanced adaptation planning in the region. The key messages approach allows authors to address questions of greatest importance to adaptation decision-making in the region, rather than assessing all relevant issues.

Within the larger national assessment process, the Prairie Provinces chapter follows the release of Canada’s Changing Climate Report in 2019 and precedes the National Issues Report, which will be available in early 2021. Other regional chapters—including Northern Canada, British Columbia, Ontario, Quebec and Atlantic Canada—will also be released over the coming year.

The overarching goal of the national assessment process is to assess, synthesize and share the latest knowledge on climate change impacts and adaptation in Canada. We hope that this chapter on the Prairie Provinces, as well as those that follow, will inspire and equip you with the information needed to take rapid and meaningful actions to adapt to climate change.

 

The National Assessment Advisory Committee 

Gord Beal, Chartered Professional Accountants Canada
Robert Capozi, New Brunswick Climate Change Secretariat
Stewart Cohen, Independent Climate Scientist (Environment and Climate Change Canada, retired)
Ellen Curtis, Physical and Health Education Canada
Susan Evans, Ontario Ministry of Agriculture and Rural Affairs
Elaine Fox, Government of Manitoba
Pierre Gosselin,    Institut national de santé publique du Québec
Ewa Jackson, ICLEI Canada
Caroline Larrivée, Ouranos
David Lapp, Engineers Canada (retired)
Fred Lipschultz, U.S. Global Change Research Program
Patricia Manuel, Dalhousie University
Linda Mortsch, University of Waterloo
Graeme Reed, Assembly of First Nations
Marjorie Shepherd, Environment and Climate Change Canada
Jim Vanderwal, Fraser Basin Council
Fiona Warren (Chair), Natural Resources Canada
Thomas White, Government of British Columbia

4.1

Introduction

The provinces of Alberta, Saskatchewan and Manitoba represent about one third of the area of Canada and lie south of 60 degrees latitude. This large region is known as the “Prairie provinces” or simply the “Prairies”, although only about 30% of the region lies within the Prairie Ecozone (see Figure 4.1). The ecosystems and landscapes of the Prairie provinces include the Rocky Mountains, boreal and cordilleran forests, semiarid interior plains, aspen parkland, subarctic shield and Hudson Bay lowlands (see Figure 4.1). The region features considerable economic and social diversity—including Canada’s third largest provincial economy (Alberta) and the nation’s fourth and fifth most populated cites (Calgary and Edmonton, respectively)—in contrast to the rural agricultural communities of the southern prairies, and the mining and forestry industries and remote, mostly Indigenous communities of the northern part of the region. Extraction and processing of non-renewable resources (e.g., oil and gas, mining) are a major economic driver, representing the largest contributing sector to the economies of Alberta and Saskatchewan (Western Economic Diversification Canada, 2018), whereas Manitoba’s economy is more varied. The economies of all three Prairie provinces are becoming more diverse, with a downturn in the oil and gas sector in recent years and more local manufacturing and high-tech industries.

Figure 4.1

Map of the Ecozones of the Prairie Provinces also showing the Aboriginal Lands of Canada Legislative Boundaries, and major cities, rivers, and lakes.

Figure 4.1

Map of the Ecozones of the Prairie Provinces also showing the Aboriginal Lands of Canada Legislative Boundaries, and major cities, rivers, and lakes.

Source

Prairie Adaptation Research Collaborative

In assessing existing knowledge of climate change impacts and adaptation, the following characteristics of the Prairie provinces emerge as important determinants of vulnerability to climate change:

  • The Prairies, and western Canada generally, have had the strongest warming to date across southern Canada, especially in winter;
  • More than 80% of Canada’s agricultural land and most of the country’s irrigated agriculture is located in the Prairies;
  • Water resources, ecosystems and resource economies are subject to large seasonal and interannual variations in climate, and especially to departures from normal conditions (e.g., drought);
  • Historically, the region has seen a population shift from rural to urban areas, and in-migration from other provinces and beyond Canada in response to economic opportunities. From 2007‒2017, the four fastest growing cities in Canada were the major cities in Alberta and Saskatchewan. Western Canada has led the nation in the highest rate of employment of landed immigrants (Statistics Canada, 2018a);
  • Most of the population and commercial activity is in the southern Prairies, which is also the part of the region with the most limited and variable water supply. Most rural communities depend on local runoff and groundwater. Urban communities access water from the major rivers and lakes, which also support the main industries, such as oil sand mining in northern Alberta;
  • The Prairies are home to 39.2% (656,970) of Canada’s Indigenous population—including 45.8% (246,485) of Canada’s Métis population—with the majority of Indigenous people living off-reserve (Statistics Canada, 2019a). More than 10% of the Indigenous population in the region lives in Winnipeg and Regina (Statistics Canada, 2019b). The Prairie provinces are entirely covered by numbered treaties, which are the basis for the relationship between First Nations and the Government of Canada.

Recent extreme weather events in the Prairie provinces include the most costly natural disasters in Canadian history (see Figure 4.2; SeaFirst Insurance Brokers, 2018). The 20 most costly weather events in Canada since 1983 are listed in Table 4.1; of these events, 13 occurred in the Prairies. Six of the top 10 have occurred in the Prairies region since 2010. The concentration of losses in Alberta largely reflects the fact that its population is more than four times larger than Saskatchewan’s or Manitoba’s. While the cost associated with damage from recent storms, flooding events and fires—notably the 2013 flood in Calgary and 2016 wildfire in Fort McMurray—is in the billions of dollars, drought is the most costly type of weather event in terms of loss and damage in the Prairies. The dollar amounts listed in Table 4.1 represent insured losses. On the other hand, the socio-economic impacts of drought are widespread, both geographically and throughout the economy. During the drought year of 2002, crop losses alone were in the billions of dollars, with negative net farm income in Saskatchewan and zero farm income in Alberta (Wheaton et al., 2008).

Table 4.1

The twenty most damaging Canadian weather events since 1983

Date Place Event type Losses
($ million)*
May 3–19, 2016 Fort McMurray, AB Fire 3,899.1
January 1998 Southern Quebec Ice storm 2,022.3
June 19–24, 2013 Southern Alberta Flooding, water 1,737.4
July 8, 2013 Greater Toronto Area, ON Flooding, lightning, water 1,004.6
August 19, 2005 Southern Ontario Hail, tornadoes, wind 779.7
May 4, 2018 Hamilton, ON; Greater Toronto Area, ON; Southern Quebec Windstorm, water 680.0
May 15–16, 2011 Slave Lake, AB Fire, windstorm 587.6
August 7, 2014 Central Alberta Hail, lightning, water, windstorm 582.3
August 12, 2012 Calgary, AB Hail, lightning, water 571.8
July 12, 2010 Calgary, AB Hail, flooding, lightning, windstorm 557.7
September 7, 1991 Calgary, AB Hail 552.2
July 30–August 1, 2016 Calgary, AB; Fort McMurray, AB; Yorkton, SK; Melville SK; Winnipeg, MB Hail, lightning, water, windstorm 480.5
August 1–3, 2009 Calgary, AB; Camrose AB Hail, lightning, water, windstorm 404.1
June 6–8 and 17–19, 2005 Alberta Flooding 374.0
September 21, 2018 Dunrobin, ON; Nepean, ON; Ottawa, ON; Gatineau, QC Flooding, hail, water, windstorm 334.0
July 23, 1996 Outaouais, QC Hail, wind 310.9
July 25–August 14, 1993 Winnipeg, MB Flooding 288.1
July 31, 1987 Edmonton, AB Tornado 282.5
July 21, 2015 Central Alberta Flooding, hail, water, windstorm 273.3
Summer 2003 British Columbia Forest fire 259.5
*Losses are in 2018 $.

Source: IBC Weather Facts, 2019.

Figure 4.2

Economic impacts of the most damaging extreme weather events to date in the Prairie provinces. Costs represent insured losses in 2018 $. Total costs are generally much higher.

Economic impacts of the most damaging extreme weather events to date in the Prairie provinces. Costs represent insured losses in 2018 $. Total costs are generally much higher.
Figure 4.2

Economic impacts of the most damaging extreme weather events to date in the Prairie provinces. Costs represent insured losses in 2018 $. Total costs are generally much higher.

Source

Insurance Bureau of Canada, 2019.

With climate change, the Prairie provinces are projected to be much less cold than at present, with increased total precipitation, although mostly in winter and spring (Zhang et al., 2019). Evaporation and transpiration will also increase with warmer temperatures, leading to more frequent and intense droughts and soil moisture deficits over the southern Prairies during summer (Cohen et al., 2019). There will be far fewer cold days, higher maximum temperatures and heavier rainfall events, as warming amplifies the already wide variability in the prairie hydroclimate (see Figure 4.3). This natural variability underlies the changes caused by a warming climate, and accounts for differences among future projections of temperature and precipitation that cannot be explained by the use of different models and greenhouse gas emissions scenarios (Barrow and Sauchyn, 2019).

Figure 4.3

Variable
Month
Scenario
Decade
Figure 4.3

Regional map of the Prairie region illustrating historical and projected data using RCP8.5 for key climate change variables—minimum winter temperature, growing degree days and maximum one-day precipitation—from 1951 to 2100.

Source

This chapter builds on the Prairies chapter in the previous national assessment (Sauchyn and Kulshreshtha, 2008) by emphasizing adaptation processes and planning, and highlighting progress made over the past 10 years. It focuses on knowledge that enables better adaptation, resilience planning and policy development. A recurring theme in this chapter is the distinction between the impacts of and adaptation to slow-onset climate change—such as changes in average temperature and precipitation patterns—versus shifts in climate variability and the occurrence of extreme weather events, which are associated with natural hazards such as floods, drought and wildfire.

4.2

Prairie ecosystems will shift and transform as the climate warms

As species respond to climate change, large regions of boreal forest could transition to aspen parkland and grassland ecosystems, while entire mountain ecosystems could disappear. Although biodiversity could increase overall, some species will be lost if the rate of warming exceeds their ability to adapt. Adaptation interventions are based mainly on standard conservation strategies—such as reduction of anthropogenic and other stressors and disturbances—and minimizing barriers to movement.

Climate change will result in broad-scale ecosystem shifts across the Prairie provinces. These shifts will lag behind changes in climate by decades, and will therefore continue well into the future. The extent to which forest, grassland and parkland ecosystems shift will depend on the rate of climate change and the success of adaptation measures. Such measures include planting tree species that are adapted to dry conditions and removing human-caused barriers to range shifts, such as those caused by industrial and urban development. Some species may be lost as ecosystems transition, while in the mountains, entire ecosystems could disappear as their climate envelopes rise to higher elevations. On the other hand, the climate associated with grasslands is expected to expand, suggesting that the many at-risk species in this region could benefit, with appropriate protection and restoration of grassland habitat.

4.2.1

Ecosystem shifts

Over the long term, plants respond to climatic changes by shifting their ranges. These shifts are mediated through competition and other interspecific interactions (Hargreaves et al., 2014; HilleRisLambers et al., 2013). Competition ensures that the plants that exist in any particular area are those best adapted to the local climate and site conditions. When the climate regime changes, the competitive balance is disrupted and must be re-established (Wiens et al., 2010; Martinez-Meyer et al., 2004). At the macro scale, this manifests as a slow directional shift in the distribution of plant communities along the prevailing climatic gradient (Kelly and Goulden, 2008). This is often described as plants “tracking” their climatic envelope, although it is actually a process driven by competition (see Ecosystem Services chapter and Box 4.1).

Soil moisture levels control the broad-scale vegetation patterns in the Prairie provinces (Hogg and Hurdle, 1995; Hogg, 1994). A mixed-grass prairie occupies the driest areas of the region, transitioning to taller grasses, aspen parkland, closed aspen forests and boreal forest as moisture levels increase (Schneider, 2013; Thorpe, 2011). Warmer temperatures will increase evaporation and transpiration during the growing season, resulting in lower soil moisture unless it is offset by increases in seasonal precipitation. While annual precipitation is projected to increase across most of the region, much of this will occur early in the calendar year and is likely to be insufficient for preventing soil moisture decreases by late summer (Bonsal et al., 2019).

The northern forests of the Prairie provinces receive much less precipitation than do most forests in British Columbia and eastern Canada (Hogg and Hurdle, 1995). Lower mean temperatures and rates of evaporation explain the positive water balance and forest vegetation. However, as temperatures rise and soil moisture declines, the forest will transition to a more open ecosystem type. There is a strong likelihood that large areas of boreal forest will eventually transition to aspen parkland and grassland, even under the lowest warming scenarios (Stralberg et al., 2018; Ireson et al., 2015; Schneider et al., 2015; Hogg and Hurdle, 1995).

Vegetation communities will track their preferred climatic envelopes as they shift northward and upslope as a result of progressive warming. The rate and spatial pattern of vegetation transitions depend largely on warming rates, natural disturbance rates and the individual species’ dispersal rates (see Box 4.1). Ecosystem transitions are expected to be dramatic in Alberta (see Figure 4.4), reflecting the fact that most low-elevation areas in northern Alberta are already near the climatic threshold between forest and grassland. Open prairie and farming communities already exist along the Peace River in northern Alberta. Northern Saskatchewan and Manitoba receive more precipitation than northern Alberta, and are therefore less likely to undergo similar transitions. However, the southern fringe of the boreal forest will move substantially northward, and island forests in the southern parts of these provinces are unlikely to remain forested (Ireson et al., 2015; Hogg and Bernier, 2005; Henderson et al., 2002). As the climate warms, southern parts of the Prairie provinces will remain as grassland ecosystems, but the species composition will shift in areas that have not been converted to agriculture. Under a low emissions scenario, the grassland ecosystems in this region may eventually resemble the grassland communities of Montana and North Dakota (Thorpe, 2011). Higher levels of warming may result in an influx of species that are not native to Canada (see International Dimensions chapter; Thorpe, 2011).

Figure 4.4

2005 2050
Figure 4.4

The distribution of Alberta’s major ecosystem types in 2005 (left) and bioclimatic envelope model projections of these ecosystems for the 2050s (right), under a medium emissions scenario (ECHAM5-A2).

Source

Adapted from Schneider and Bayne, 2015.

Bioclimatic envelope model projections, such as those presented in Figure 4.4, predict the equilibrium redistribution of ecosystems under future climatic conditions for a medium emissions scenario. However, since the climate is expected to continue changing until at least well into the next century, we can expect a prolonged period of transition. Ecosystems will be complex mixtures of old and new elements, blurring ecosystem boundaries and increasing habitat diversity in most regions (Savage and Vellend, 2015; Berteaux et al., 2010).

Increased evaporation and a longer snow-free period will reduce the average water levels of wetlands and increase the amount of time that seasonal wetlands are dry (Johnson et al., 2010; Larson, 1995). These changes will be most pronounced in the southern grasslands, where summer moisture deficits are already the norm. In northern areas, peatlands predominate and have considerable resistance to evaporation losses (Kettridge and Waddington, 2014). Nevertheless, the overall area of peatlands will slowly contract (Schneider et al., 2015). In all areas, the amount of change will be proportional to the amount of warming.

4.2.2

Animal responses

Climate influences animal distributions both directly and indirectly, with impacts differing between habitat generalists and habitat specialists. For generalists, the direct effects of warming are likely to be most important. For example, white-tailed deer are found across many Prairie biomes, from boreal forests to grasslands. The northern extent of their range is thought to be determined mainly by winter severity, which affects survival and fecundity (Dawe and Boutin, 2016). Thus, warmer winters are likely to lead to range expansion long before vegetative communities have responded. Evidence of such climate-induced range expansion is already accumulating in the Prairie provinces and in adjacent regions to the north (Dawe and Boutin, 2016; Veitch, 2001).

For other animal species, habitat suitability is the key factor governing range shifts (Nixon et al., 2016; Kissling et al., 2010). For example, the climate envelope for the burrowing owl—an endangered grassland species at the northern extent of its range in the Prairie provinces—is projected to move northward fairly rapidly (Fisher and Bayne, 2014). However, the owls will not be able to utilize this expanded potential range until entire grassland ecosystems—including appropriate vegetation and prey species—are in place. As such, despite their high mobility, many animal species will be unable to respond to climate any faster than the plant species they ultimately depend upon (Nixon et al., 2016).

4.2.3

Biodiversity implications and adaptation strategies

Species diversity in Canada declines with increasing latitude and is, on the whole, relatively low compared to many other countries (Willig et al., 2003). A northward movement of climate envelopes is expected to boost biotic productivity and species richness at all latitudes (Savage and Vellend, 2015; Jia et al., 2009). However, not all ecosystems and species will benefit. For example, alpine ecosystems in the Rocky Mountains will be compressed as suitable climate conditions rise in elevation towards the summits of the mountain peaks. The grassland ecosystems, with the largest number of species at risk in the Prairie provinces, will benefit as they expand into the southern boreal region (Ireson et al., 2015; Hogg and Hurdle, 1995).

These expectations of biodiversity patterns are subject to a major caveat. Individual species must have the ability to keep pace with climatic and ecological changes as they occur; otherwise, warming may result in the loss of species rather than a reshuffling of species. Although Canadian species have demonstrated the ability to adapt to dramatic climate changes in the past, the current unprecedented rate of change may result in some species being unable to adapt quickly enough, especially those with low dispersal ability, low rates of reproduction and low levels of genetic variation (Pearson et al., 2014).

The landscapes of the Prairie provinces are also greatly impacted by human activities, which limit the ability of species to adapt. Concern is greatest for species at risk, which are already struggling to remain viable under current conditions. The added stress imposed by rapidly changing climatic conditions exacerbates other anthropogenic impacts on species habitats (Hof et al., 2011). For example, the burrowing owl is currently declining in abundance as its habitat is contracting southward towards the core of its range in the US (COSEWIC, 2006), despite the fact that changing climate conditions suggest it should be able to expand along the northern edge of its range as conditions become suitable. Moreover, its small remnant populations in Canada may lack the resilience needed to withstand extreme weather events (Fisher et al., 2015; Oliver et al., 2013).

Species also face physical barriers that impede range shifts (Hof et al., 2011; Melles et al., 2011). Habitat deterioration presents the most widespread barrier and, while not completely blocking movement, slows the pace of adaptation. For example, the ability of grassland species to track their preferred climate is likely to be hindered by the presence of intensively managed agricultural land (Nixon et al., 2016). For fish, stream fragmentation may reduce access into climatically optimal watercourses (Park et al., 2008).

With appropriate management support, the proportion of species that are “left behind” may be relatively small under low emission scenarios. However, widespread adaptation failure is a real possibility under high emission scenarios, which will result in unprecedented changes (Corlett and Westcott, 2013). Available adaptation measures are, for the most part, components of the standard conservation toolkit (Schneider, 2014; Heller and Zavaleta, 2009). A key approach is to reduce anthropogenic stressors—such as habitat loss—to improve the general vitality and resilience of species, thereby enhancing their adaptive capacity.

Management strategies designed to minimize the impacts of human disturbances are paramount. In managing forest and grassland ecosystems, it is important that conservation objectives be dynamic, rather than planned based on historical conditions. The challenge is to develop a planning system that embraces flexibility, while safeguarding against activities that are inconsistent with the aims of conservation. There is also a need to incorporate climate change into the regulatory and policy frameworks supporting conservation. The Canadian Council of Forest Ministers developed a toolbox to assist forest managers in determining the vulnerability of their forest management systems to climate change. The centrepiece of the toolbox is a guidebook (Edwards et al., 2015) that walks forest managers through vulnerability assessment and adaptation planning.

Another important strategy is to remove or minimize barriers to movement, such as by restoring previously disturbed landscapes. Strategically placed protected areas can also facilitate species movements (Nantel et al., 2014; Nunez et al., 2013). Species that are unable to effectively track climatic changes may require active support in the form of assisted migration (Gallagher et al., 2015; Warren and Lemmen, 2014). Assisted migration is a feasible adaptation option that can be implemented now in preparation for future impacts—such as drought or warmer temperatures—and resulting changes in habitat (Warren and Lemmen, 2014; Ste-Marie et al., 2011). This form of migration can comprise the following: i) assisted population expansion, by moving populations (i.e., seed) from other locations to sites within the current species range to improve productivity and health as the climate changes; ii) assisted range expansion, by moving seed to locations somewhat beyond the species’ current distribution, where the climate in the near future is expected to be suitable for the growth of the species; and iii) translocation of exotics, by moving a species far beyond its current distribution to a location in which it has not been established in the past (e.g., to a new ecoregion or a different continent) (see Ste-Marie, et al., 2011 for a comprehensive review of assisted migration in the Canadian context).

4.3

Floods, drought and wildfires are getting worse

Extreme weather events of amplified severity will likely be the most challenging consequence of climate change in the Prairie Provinces. The impacts of flooding, drought and wildfire in recent years are unprecedented, and climate models suggest an increased risk of these events in the future. Provincial and municipal governments have responded by proposing policies, structures and practices to reduce the impacts of future extreme weather events.

Recent extreme weather events in the Prairie provinces―including flooding, drought and wildfire―have been the costliest natural disasters in Canadian history. This includes record dry months and historically high water levels. An increased frequency and severity of extreme weather events will be superimposed upon a more gradual change in average conditions, requiring adaptation to prepare for a wider range of weather conditions and to shifts in the distribution of water resources. Ultimately, water shortages would be the most damaging, resulting in social and environmental impacts, along with economic losses from lost productivity in the agriculture, forestry, energy and mining sectors (i.e., extraction of oil sands and solution potash mining).  

4.3.1

Weather hazards

Extreme weather presents the most immediate climate risk for the Prairie provinces, as is evident from the catastrophic events that have taken place over the past 10 years (see Figure 4.2). Extremes in precipitation and temperature lead to impacts, such as flooding, drought and wildfire (see Box 4.2). Given the vast size and hydroclimatic diversity of the Prairie provinces, it is not unusual for parts of the region to be experiencing drought and wildfire at the same time, while other communities are being flooded (Brimelow et al., 2014). Extreme weather events superimposed on longer-term trends of changing average climate conditions have significant social and economic impacts, challenging the sustainable management of water, forests and soil.

Climate warming may have profound and immediate impacts on wildfire activity. The area of forest burned in Canada has already increased, mainly due to human-caused warming (Gillett et al., 2004). Warmer temperatures lengthen the fire season (Albert-Green et al., 2013) and are associated with increased lightning strikes (Romps et al., 2014). More importantly, higher temperatures lead to drier fuels, as moisture is lost from soil and plants to the warmer atmosphere (Flannigan et al., 2016). The amount of moisture held by the atmosphere increases almost exponentially as the temperature rises. Almost none of the future scenarios include sufficient increases in precipitation to compensate for the drying effect of warmer temperatures. Drier fuels make it easier for fires to start, spread and burn more intensely, making them more difficult to extinguish (see Video 4.1).


Video 4.1:
Métis wildland firefighters are deeply connected to the land, their culture, and the impacts of climate change across the Canadian prairies. Source: Métis National Council and Prairie Climate Centre, 2020.

 

4.3.2

Hydrological hazards

Large interannual variability and extreme hydroclimatic events are characteristic of the Prairie provinces. Simultaneous wet and dry conditions across the region are not uncommon; they occur, for example, when high pressure in the western Prairies diverts moist air masses towards the east (e.g., Szeto et al., 2011; Rannie, 2006; Liu et al., 2004).

Both gradual, long-term changes in water levels and extreme fluctuations around the changing baseline will have impacts and require adaptation. Water allocation and the design of storage and conveyance structures—such as reservoir and irrigation pipes—are based mainly on average seasonal water levels. Otherwise, water resources are managed to prevent the adverse impacts of flooding and drought.

There has been much analysis of the most recent multi-year drought in the Prairie provinces, which spanned the period from 1999‒2004 (e.g., Hanesiak et al., 2011; Bonsal et al., 2011; Wheaton et al., 2008). This was followed by a period of relatively wet conditions from 2005‒2019, with the exception of some intense droughts of seasonal duration, including from summer 2008 to winter of 2009‒2010 (Wittrock et al., 2010), summer 2015 (Szeto et al., 2016), spring/summer 2017 (Jencso et al., 2019), and spring/summer 2019 (Agriculture and Agri-Food Canada, 2019). While drought and flooding are difficult to predict, their probability is strongly linked to periodic fluctuations in sea surface temperatures in the Pacific Ocean, known as the Pacific Decadal Oscillation (PDO) and the El Niño Southern Oscillation (ENSO) (see Box 2.5 in Bush et al., 2019). Uncertainty in projected future precipitation amounts and extremes depends largely on the ability of the models to simulate the internal variability of the regional climate—such as changes in the teleconnections between ocean‒atmosphere oscillations (i.e., the ENSO and PDO) and in the regional hydroclimate (Barrow and Sauchyn, 2019)—and, to a lesser extent, on the use of different models and greenhouse gas emissions scenarios.

The impacts of water excesses and deficits differ with respect to the timing, duration, intensity and extent of flood and drought events. Meteorological drought (lack of rain) can immediately affect dryland farming, while hydrological drought (low water levels) affects irrigation, municipal and industrial water supplies. The cumulative impacts of a long period of low water levels contrast with the effect of short, intense drought. Flooding has been most damaging along the Red River in Manitoba and the rivers flowing from the Rocky Mountains, where population centres are concentrated. In the Prairies, however, inundation of agricultural land is common given the large area of depression storage (including sloughs and wetlands). A torrential rainstorm near Vanguard, SK on July 3, 2000, saw 375 mm of rain fall in 8 hours, with an estimated 62% of that water retained on the landscape (Hunter et al., 2002). While drought results in crop losses over large areas, flooding can prevent the sowing of crops, as occurred in 2011 over 5.5 million hectares, mostly in Manitoba (Brimelow et al., 2014). The Quill Lakes of east-central Saskatchewan have risen to such an extent that they are now one large lake inundating thousands of hectares of farmland, railroads and provincial highways (Water Security Agency, 2016).

Studies of the 2015 drought (Szeto et al., 2016), 2013 floods in southwestern Alberta (Teufel et al., 2017; Pomeroy et al., 2015) and of the Assiniboine River Basin in Saskatchewan and Manitoba in 2014 (Szeto et al., 2016) concluded that these naturally occurring events were intensified by human-caused climate change. The analysis of rainfall data generated by climate models indicates that a warming climate will cause a significant shift from historical values in the intensity, duration and frequency of rainfall events (Bonsal et al., 2019). For example, climate projections for Saskatoon reveal an increase in the intensity of short-duration extreme precipitation events and a decrease in the length of the return period between these events, with the most intense precipitation occurring towards the end of the 21st century under the RCP8.5 high emissions scenario (Alam and Elshorbagy, 2015).

An increase in rainfall intensity is one of the most consistent changes projected globally (IPCC, 2014), nationally (Zhang et al., 2019) and regionally (Gizaw and Gan, 2015). In the Prairies, farmland and infrastructure could be periodically inundated by excess precipitation in winter, which in future decades is increasingly likely to fall as rain. This excess water will occur as the warmer climate converges with the wet phase of the PDO and ENSO. Similarly, the amplitude of dry phases will likewise increase when there is an absence of rain, but also with higher temperatures than in the past (Tan et al., 2019). Climate projections suggest an increasing risk of drought in the Prairies, specifically in summer and fall (Bonsal et al., 2019). The worst-case future scenario for the Prairie provinces is the reoccurrence of consecutive years of severe drought, such as those that occurred in the 1930s and in preceding centuries (Sauchyn et al., 2015).

4.3.3

Societal impacts

The 2013 flooding in Calgary and the 2016 wildfire in Fort McMurray represent two of the costliest natural disasters in Canadian history, and provide dramatic examples of societal impacts arising from extreme weather. They also provide insight into actions being taken to reduce such impacts in the future (see Case Story 4.1), and highlight the linkages between climate change and natural disasters (see Case Story 4.2).

The impacts of extreme weather differ significantly between communities and social groups, depending on their livelihoods and access to social, economic and natural capital (Diaz et al., 2016). For example, Indigenous communities have suffered disproportionately from flooding as a result of living in poor housing that is frequently situated in low-lying areas and in close proximity to rivers (Wittrock et al., 2012, 2011). The health impacts of drought (Yusa et al., 2015) include the following: consequences for respiratory and mental health; risks to food and water security; and increased exposure to injury, disease and pollution, including exposure to toxins. For example, during the drought of 2001–2002, blowing dust led to various health impacts, including traffic accidents that resulted in fatalities (Wheaton et al., 2008). Multiple extreme events—such as drought, wildfire and flooding—compound the damage and costs to communities and economies, and can even result in insurance claims being made simultaneously for flood and drought damages, such as occurred in 2009 in southern Manitoba (Brimelow et al., 2014). Drought impacts are less immediate than the impacts of flooding and wildfire, but crop failures, soil drifting and dust storms have historically been some of the most serious consequences associated with drought (Wheaton et al., 2008). The extensive adoption of minimum tillage and direct seeding across the agricultural landscapes of the Prairies has nearly eliminated the occurrence of dust storms in dry summers. However, concerns exist that producers may be tempted to abandon drought adaptation measures—such as zero tillage and shelterbelts—during wet cycles, such as those that occurred in the early- to mid-2010s (Rempel et al., 2017).

The most reliable information on the impacts of extreme events is provided by those who are or have been affected, as they can offer “intense and richly contextual” experiential knowledge (Marchildon et al., 2016). Local and Indigenous knowledge can inform extreme event preparedness and response planning: “While disaster relief and climate adaptation plans at national and subnational levels of government need to focus on the scientific record … local governments responsible for smaller areas should be in a position to adjust for local differences” (Marchildon et al., 2016). Local conditions (e.g., soil and topography; social, financial and natural capital; and adaptive capacity) can exacerbate or reduce the impacts of climate extremes. For example, the vulnerability of a community to drought can depend highly on the reliability of its water supply (Wittrock et al., 2011).

4.4

Collaborative water management reduces negative impacts

Regional land-use policy and planning, as well as emergency preparedness, are critical for reducing the impacts of flooding and drought in the Prairie provinces. Collaboration is needed among all levels of government, and with stakeholders such as watershed stewardship groups, rural municipalities and conservation districts, to implement these adaptation measures and to promote practices that prevent or minimize adverse effects of water excesses and shortages.

The Prairie provinces have extensive experience dealing with water excesses and shortages, and have developed important mechanisms for adapting to climate variability. While many of these mechanisms are tailored to drought, some also address flooding and excessive moisture. The extensive management of water flows through dams, diversions and withdrawals on the Prairies makes it difficult to discern climate-related changes; adaptive management of water resources can help to compensate for changes in the availability of water supplies, while also reducing the impacts of flooding and drought. 

4.4.1

Institutional mechanisms

Interprovincial level

Canada’s decentralized approach to water governance provides the provinces with considerable autonomy over water-related decisions (Heinmiller, 2018). The Prairie Provinces Water Board (PPWB) is an enduring institution established in 1948 to foster water management cooperation among the provinces of Alberta, Saskatchewan and Manitoba. The Master Agreement on Apportionment (MAA) was created by the PPWB in 1969 (Heinmiller, 2018) and states that in any given year, each province is entitled to half of the natural flows of interprovincial rivers, as measured at the provincial boundary (Prairie Provinces Water Board, 2015). The MAA thereby removes potential uncertainties associated with interprovincial politics when dealing with water scarcity. It provides water managers in each province with a clear quota of the amount of available water that they will manage, even if the actual amount of water in the river is uncertain or highly variable.

While the PPWB and MAA provide this important mechanism to address hydroclimate extremes, particularly drought, they can also be inflexible under changing climate conditions, given the strictly defined apportionment of surface water among the Prairie Provinces. The PPWB has been examining the issue of the MAA’s resilience under various climate scenarios (Prairie Provinces Water Board, 2014). This type of strategic exercise demonstrates one benefit of the PPWB and the interprovincial governance networks that it fosters.

Provincial level

The individual Prairie provinces have differing approaches to coping with hydroclimatic extremes. For example, Alberta uses a cap-and-trade system for reallocating water licences during times of water scarcity, whereas Saskatchewan and Manitoba take a more centralized approach with strong government oversight (Heinmiller, 2018; Government of Manitoba, 2018). Alberta allows for the creation of water markets at the regional level to reallocate water from low-valued to high-valued uses when drought threatens the status quo. While this is a potentially useful institutional mechanism, concerns have been raised about fairness and equity issues that could emerge (Hurlbert and Gupta, 2017). For example, declining summer river flows from the Rocky Mountains could affect water allocations in southern Alberta, especially for junior licence holders, since the major irrigation districts hold the senior licences.

The effect of low water levels in the South Saskatchewan River Basin (SSRB) was ameliorated somewhat following the drought of 2001–2002, when the transfer of water rights was introduced and the Government of Alberta closed much of the SSRB to new surface water allocations (Government of Alberta, 2006). Saskatchewan’s more centralized approach may limit opportunities among affected stakeholders for sharing and learning about drought response mechanisms and other adaptation challenges (Hurlbert and Gupta, 2017).

The previous experiences of the Prairie provinces with water and weather extremes have led to the development of important mechanisms for adapting to climate variability. All three provinces have a plan for drought—the region’s worst threat (see Table 4.3)—and Alberta’s plan also addresses the risks of excessive moisture, demonstrating how some mechanisms tailored to drought could be repurposed to address concerns about flooding and excessive moisture. The Saskatchewan plan is mostly focused on agricultural risks, as drought planning is part of the Water Security Agency’s broader mandate and 25-year plan. Manitoba’s drought planning appears to recognize the wider environmental, economic and societal impacts. All of the plans consider climate change to some extent.

Table 4.3

Provincial drought planning: Some characteristics and status

Province Most recent report  Lead Ministry/ Ministries  Climate change addressed? Next steps? (Examples) Current implementation stage? (Examples)
Alberta Alberta’s Agriculture Drought and Excess Moisture Risk Management Plan (2016) Alberta  Agriculture and Forestry Yes Continued improvement is envisioned Drought and excess moisture advisory group
Saskatchewan 25 Year Saskatchewan Water Security Plan (2012)* Ministry of Agriculture; Water Security Agency Yes Several listed, (e.g., coordination of moisture monitoring, new infrastructure) Moisture monitoring committee meets as needed
Manitoba A Made-in-Manitoba Climate and Green Plan (2017) Manitoba Sustainable Development and Stewardship (now the Ministry of Conservation and Climate) Yes Evaluate the strategy and update;

determine drought preparedness levels

Evaluate and update the strategy;

status of action items are reported (2017)

* The plan includes drought response actions.

Watershed or regional level

Across the Prairie provinces, watershed-based organizations have become an effective mechanism for local climate adaptation planning and soil water protection. In Manitoba, the Watershed Districts Program (formerly Conservation District Program) is a partnership between the province, which provides most of the funding, and more than 130 municipalities that develop and administer soil and water conservation programs. The Watershed Districts Act, proclaimed on January 1, 2020, transitioned 18 conservation districts to 14 new watershed districts, with boundaries based on drainage divides (Government of Manitoba, 2020). Integrated watershed management plans were among 30 municipal planning documents reviewed in a report commissioned by Manitoba Sustainable Development (now the Ministry of Conservation and Climate) (International Institute for Sustainable Development, 2019). Only five of the 30 documents explicitly referred to the need to adapt to climate change, and none included climate projections, nor committed to taking further actions to assess the climate change risks to their communities. Saskatchewan established local Watershed Stewardship Groups to work in collaboration with the provincial government to address a broad range of water quality-related issues. These groups constitute forums for multiple stakeholders to discuss local water issues and design locally appropriate solutions. They typically include participants from municipalities, agricultural producers, environmental NGOS and other industries in the respective watershed. While initially focusing on water quality, these groups have since branched out to tackle other water-related issues, including drought and flooding (Pittman et al., 2016). Many groups have been involved in climate change adaptation projects, including the development of extreme hydroclimate scenarios and action plans to provide watershed-specific solutions (Pittman et al., 2016). In Alberta, eleven Watershed Planning and Advisory Councils (WPACs) are independent, non-profit organizations designated by Alberta Environment and Parks to report on the health of their watersheds, lead collaborative planning, and facilitate education and stewardship activities. Each WPAC engages key stakeholders in their watershed, seeking consensus on land and water management strategies to achieve shared environmental, social and economic goals (see Case Story 4.3).

Irrigation districts across the Prairie provinces are another type of local stakeholder group that helps to manage hydroclimate extremes. While initially developed to manage local water for irrigation, they are now engaged in a broader range of issues. For example, during the 2001-2002 drought, the water markets referred to previously were coordinated by the local irrigation district in the Oldman River Basin of Alberta. Irrigation districts provide a locally-rooted mechanism for building trust and fostering collective action in the face of water-related adversity. They have been involved in participatory scenario exercises to prepare for drought (Hadarits et al., 2017) and have also voluntarily taken on new roles addressing adaptation to excessive moisture. The infrastructure managed by the irrigation districts to enhance agricultural production has also proven useful in recent years for dealing with excessively wet conditions (Hadarits et al., 2017).

4.5

Climate change brings both benefits and threats to agriculture

Prairie agriculture, particularly crop production, may benefit from higher temperatures and a longer growing season. Achieving net benefits will require adaptation to limit the impacts of climate extremes, including on water availability, and the increased risk of pests, vector-borne diseases and invasive species. Although agricultural producers are highly adaptable to fluctuations in weather and climate, barriers to adaptation include limited information and awareness of climate change impacts, combined with limited financial resources and institutional support.

Agriculture is a key employer and a major driver of the economy in the Prairies. Climate change brings both opportunities for and threats to agriculture. Direct impacts include changes in growing season length, timing and quantity of precipitation, heat units, extreme events—such as heat, hail and windstorms, flooding and drought. Indirect climate change impacts include effects on weeds, diseases, insects and soil characteristics, as well as on socio-economic factors influenced by global-scale changes in climate. These factors include effects on global food security, and trade and relations with supply industries for agricultural production and food processing. Assessing the convergence of these direct and indirect impacts is a major challenge. The overall impacts of climate change will depend on the effectiveness of adaptation not only in the Prairie provinces, but in Canada more generally and in other countries as well.

4.5.1

Impacts

Climate change has both direct and indirect impacts on agriculture in the Prairie provinces, resulting in both risks and opportunities (Kulshreshtha and Wheaton, 2013). Changing precipitation, temperatures, carbon dioxide levels and other variables will affect the following: crop and pasture productivity, quality and nutrient cycling; weeds, insects and diseases; and livestock production and reproductive rates (Sudmeyer et al., 2016). Projected biophysical impacts include increased water scarcity, more frequent extreme precipitation events, shifting and variable precipitation patterns, longer growing seasons, increasing heat units (i.e., a measure of crop development in relation to temperature), and more frequent and intense droughts (e.g., Bonsal et al., 2019; Kulshreshtha and Wheaton, 2013).

Certain crop yields and hay productivity may increase in the near term in response to climate factors, such as longer growing seasons and increased heat units (see Box 4.3). However, high temperatures, droughts and more variable precipitation negatively affect crop yields, particularly for canola and wheat (Qian et al., 2018; Meng et al., 2017). Increased exposure to high temperatures (e.g., over 30°C), especially at critical times, may also reduce yields of corn, soybean, canola and wheat (Schauberger et al., 2017; Meng et al., 2017).

Extreme events, particularly droughts, negatively affect crops, livestock and forage production, causing financial losses such as those that occurred in 2001‒2002, when drought resulted in a more than $2.97 billion reduction in agricultural production in the three Prairie provinces (Wheaton et al., 2008). Such impacts require further assessment and documentation (Craft et al., 2017), including an examination of the social aspects (see Section 4.6). Climate change extremes also affect soil and water quality through increased risk of soil erosion, soil salinization, desertification and soil degradation (Wheaton and Kulshreshtha, 2017). For example, flooding of agricultural lands due to precipitation extremes caused $1 billion in damages in the southeastern Prairies in 2014 (Szeto et al., 2014) and almost $700 million in 2011 in Manitoba alone (Public Safety Canada, 2019).

Future surface and soil water deficits (Bonsal et al., 2019) will have profound effects on the quantity and quality of surface water and on groundwater supplies. Decreased availability of river water is a concern for all producers, particularly those irrigating crops. Plant germination and reproduction are highly sensitive to moisture and heat stress corresponding with the timing for these stages in the life cycle of plants (Champagne et al., 2012). Negative impacts on water quality also result from extreme rainfall events, generating runoff with heavy nutrient loads, and from longer periods of low flow in streams and rivers (Venema et al., 2010).

4.5.2

Adaptation

While agricultural producers can benefit from longer and warmer growing seasons and increasing carbon dioxide levels, other climate change impacts, such as water scarcity, and excess moisture and heat, may be very challenging. Existing adaptive practices include the use of zero-till agriculture, feed stockpiling, increasing farm size, beneficial management practices, insurance, large-scale infrastructure such as dams (e.g., Warren, 2016a; McMartin and Hernani Merino, 2014; Smit and Skinner, 2002), earlier seeding dates, mixed farming and changes in crop varieties. Beneficial management practices include the use of methods, policies, programs and tools for improving the environmental and economic positioning of agriculture (McMartin and Hernani Merino, 2014). Unexpected social, economic and environmental consequences of adaptive practices could render some strategies maladaptive, meaning that despite attempting to reduce risk to climate change, they inadvertently increase vulnerability (Müller et al., 2017).

Agricultural systems need to adapt to a suite of climate change impacts that interact with other factors, such as economic pressures, opportunities related to an increasing global population, changing human dietary preferences, increased input costs and energy prices, competing land-use pressures and policy-related economic pressures. Agricultural producers have access to various types of adaptation options, ranging from relatively minor measures, such as growing drought-tolerant crop varieties, to more substantial or even transformative changes (i.e., major, purposeful actions at the farm level or higher), such as policies that remove obstacles to climate change adaptation or changes from dryland cropping to irrigation (Rickards and Howden, 2012). However, the cumulative impacts associated with multiple drivers of change will test overall capacity to adapt. Economics is a major motivation in the adoption of new practices (see Sector Impacts and Adaptation chapter), and the most appropriate adaptation measures will depend on a large number of factors, including capacity (see Case Story 4.4).

Mixed farms with both crops and livestock have advantages for adaptation. Drought response practices for mixed farms may include purchasing feed when necessary and early weaning of calves, combined with feeding strategies aimed at reducing both feed demand and the producer’s financial burden during drought periods (Poudel et al., 2017; Poudel and Kulshreshtha, 2016). Options that are more specific to rangeland and livestock production include herd management, raising alternative breeds and species, pest management, and changes in enterprises and geographic locations (Joyce et al., 2013).

Current barriers to adaptation include a lack of awareness of options, inadequate financial resources and institutional support mechanisms, insufficient preparation, and political resistance (e.g., Lilliston, 2018). The development of irrigated areas—a logical adaptation to increased water stress in agricultural systems—involves building dams and distribution channels, and is therefore highly capital intensive (Warren, 2016a). Water availability for irrigation may also be a limitation, as stream flows are reduced during severe droughts (see Section 4.4; Wheaton et al., 2008). Existing irrigation systems may not be able to cope with the water demands of a multi-year drought. Observed trends toward increasing farm debt (Statistics Canada, 2017b) may severely impede the ability to undertake adaptive actions.

Increases in heat units and longer growing seasons will affect agronomic management practices such as seeding dates. Heat stress may result in a shorter growing season for some crops, such as soybeans (Jing et al., 2017). For crops like canola, earlier seeding and increased fertilization are limited options because of increased heat and water stresses, which are important limiting factors for crop yields. Key adaptation measures include new heat- and drought-tolerant cultivars (Qian et al., 2018). Higher temperatures could lessen the limitations imposed by a short growing season along the northern margins of the agricultural zone. However, extending agriculture into this region will require adaptation of farming practices to yield crops in nutrient-poor forest soils.

Governance institutions play important roles in adaptation and can improve the adaptive capacity of producers and other rural residents (Hurlbert et al., 2009). However, capacity constraints and isolation exacerbate the vulnerability of many rural communities (Garschagen, 2013; Hanna, 2011; Lal et al., 2011). Institutions that deal with water management and development, including the former Prairie Farm Rehabilitation Administration, water-user groups, watershed stewards and irrigation project associations (Hurlbert and Gupta, 2017; McLeman et al., 2014; Marchildon, 2009) are instrumental in facilitating adaptation actions (see Section 4.4.1).

Farmers have relied on their understanding of local climate regimes to manage risk, and may not consider alternative farming practices without evidence of economic benefits (Wood et al., 2016; Convery and Wagner, 2015; Yusa et al., 2015; Heal and Millner, 2014). While the impacts of drought have been the subject of previous studies, impact assessments of flood, extreme heat and winter thaw events are more limited.

4.6

Social groups have unique vulnerabilities and strengths

The impacts of climate change may exacerbate existing societal inequities, especially among Indigenous peoples, women, people of low socio-economic status, youth and the elderly. Public policy and adaptation planning should consider the unique vulnerabilities and strengths of these social groups, and also the means by which race, age, gender and poverty amplify vulnerability or resilience to climate hazards.

Climate impacts interact with existing social inequalities, which are influenced by histories of oppression and/or colonization affecting different groups of people in different ways. Indigenous peoples, people of low socio-economic status, ethnic minorities, youth and elders all have unique strengths and vulnerabilities when adapting to climate change. Social inequality shapes social roles, access to resources and decision-making power. Multiple forms of inequality can intersect to create different experiences, even within certain groups; this is known as intersectionality. Social inequality and marginalization also shape people’s access to social infrastructure, such as services and facilities, and to physical infrastructure; this in turn affects their ability to cope with and adapt to climate change. By considering these interrelated social factors, we can plan for climate hazards more effectively and ensure that responses and infrastructure are inclusive and beneficial for all. 

4.6.1

Introduction

Climate change impacts will have widely divergent effects on Prairie economies and communities. The capacity to adapt to these impacts also varies widely. Although reliance on natural resources remains important for the economies of all three provinces, the business and service sectors are also important. The Prairie population is increasingly urbanized (Statistics Canada 2011b), with a small number of medium and large cities, combined with numerous rural communities of relatively low, and in many cases, ageing populations that are reliant on climate-sensitive sectors such as agriculture, forestry and tourism (see Rural and Remote Communities chapter).

The following analysis combines information available on the status of vulnerable social groups in the Prairie provinces. Due to limited data on how climate change affects vulnerable groups in the Prairies specifically, this section also presents a broader review of the literature on climate impacts and adaptation by drawing on research conducted in other regions. It also benefits from new conceptual frameworks that provide insights into understanding vulnerability (see Box 4.4).

4.6.2

Vulnerable social groups

While there is value in understanding which factors render various social groups (e.g., women, Indigenous people) more or less vulnerable to climate change, it is important to avoid portraying all members of such groups as inherently and consistently vulnerable and lacking the ability to respond to risks (e.g., Moosa and Tuana, 2014; Cameron, 2012; Arora-Jonsson, 2011; O’Shaughnessy and Krogman, 2011). The main elements of these vulnerabilities are described below, noting that unique strengths can advance adaptation action.

Indigenous peoples 

Many Indigenous peoples are disproportionately exposed to the impacts of climate change (Parlee and Furgal, 2012). Furthermore, Indigenous peoples experience significantly higher rates of poverty and unemployment, and lower average rates of income than the non-Indigenous population (see Table 4.5), while having less access to many services. Table 4.5 demonstrates income inequality at the intersection of gender and Indigeneity, showing notable income differentials not only between Indigenous women and non-Indigenous women, but also between Indigenous women and Indigenous men. Research on Indigenous vulnerability to climate change in the Prairies (Patrick, 2018a, b; Mottershead, 2017; Christianson et al., 2012; Wittrock et al., 2011) has identified how these and other interacting social factors exacerbate the impacts of climate change and compromise adaptation. Importantly, however, Indigenous communities are also leading their own climate change studies―for example, through federal programs such as the First Nation Adapt Program and the Indigenous Community-Based Climate Monitoring Program, among others.

Table 4.5

Selected socio-economic metrics for Indigenous and non-Indigenous populations in the Prairie provinces and Canada

Group Canada SK AB MB
Median annual after-tax individual income, (2016)
Male, non-Aboriginal $36,267 $42,483 $47,723 $36,826
Female, non-Aboriginal $26,811 $30,528 $30,903 $27,430
Male, Aboriginal $26,507 $22,297 $34,122 $22,673
Female, Aboriginal $22,799 $23,231 $24,414 $22,206
Unemployment rate, (2018)
Aboriginal population over 15, all education levels 10.1% 11.5%
Non-Aboriginal population over 15, all education levels 5.7% 6.1%
Sources: Statistics Canada Data Tables #98-400-x2016171 and #14-10-0359-0

Note: Census data still refers to “Indigenous” peoples as “Aboriginal”

Existing Canadian studies have shown that legacies of historic colonialism and its persistence today manifest in numerous ways, from poverty and poor living conditions, to substance abuse (Williams, 2018; Veland et al., 2013; Cameron, 2012). These conditions multiply the effects of risk, with particular implications for health status (Ford et al., 2010), and can result in reduced coping capacities during extreme events (Mottershead, 2017). The effects of the 2013 flood in the Siksika First Nation reserve in Alberta were more severe than in other communities, with one quarter of residents evacuated, 134 homes destroyed (which constituted approximately 9% of all homes in the Nation, according to 2011 Census figures), and loss of water supply to 62% of the remaining homes, despite which they were forced to wait longer than residents in other regions for recovery assistance (Patrick, 2018a). Studies of the severe flooding experienced in 2011 in the Lake St. Martin community and nearby First Nations communities in Manitoba highlight a lack of warning, forced evacuation on short notice, inadequate recovery efforts (some families remained displaced at the time of this chapter being written) and consistent lack of communication between emergency agencies and residents (e.g., Martin et al., 2017; Thompson, 2015).

Indigenous peoples rely to a greater―though varying―extent on local foods, with the result that shifts in availability of and access to those sources can directly affect food security and livelihoods. Limitations on the ability to participate in traditional land-based activities because of changes in species distributions and wildfires, as well as non-climate factors, can also affect mental well-being and can increase dependence on the cash-based economy (Bunce et al., 2016).

Treaty rights and other regulations may restrict Indigenous peoples’ access to their territories and/or constrain land-based adaptation strategies by specifying the types of activities in which Indigenous peoples can and cannot engage (McNeeley et al., 2018; Natcher et al., 2016; Wittrock et al., 2011). In addition, the remote location of some communities translates into acute risk to extreme events, such as floods and wildfires (Christianson et al., 2012), which can be exacerbated due to lack of early warning systems (Ford et al., 2010), and transportation networks (Tam et al., 2013) that are compromised or non-redundant (i.e., lacking alternative routes). For many communities in Northern Manitoba, for instance, mobility in winter via ice roads is jeopardized by a warming climate (Taylor and Parry, 2014; Blair and Sauchyn, 2010).

Research in regions outside of the Prairie provinces has found that food-sharing networks and other local institutions in Indigenous communities serve as important contributors to adaptive capacity (Ready, 2018; Baggio et al., 2016). Compromises in traditional sharing practices as a result of increased involvement in wage labour, for example, can affect food security to an even greater extent than declines in the availability of traditional foodstuffs (Baggio et al., 2016). Indigenous community residents living in their traditional homes also express high levels of place attachment, which can foster commitment to adaptation (Cunsolo Willox et al., 2012). However, this attachment to place may also interact with the acute personal and cultural consequences of both climate and non-climate impacts, affecting their ability to engage with the local landscape (Cunsolo Willox et al., 2012) or resulting in their forced relocation.

Indigenous peoples also have several unique sources of adaptive capacity. Culturally appropriate forms of community inclusion in adaptation planning, specifically those including women and youth (Reid et al., 2014; Whyte, 2014; Pennesi et al., 2012), allow for the identification and prioritization of locally determined values (Veland et al., 2013; Christianson et al., 2012). Indigenous knowledge is of tremendous value to climate science and adaptation planning (Ingty, 2017; Rosales and Chapman, 2015; Reid et al., 2014; Ignatowski and Rosales, 2013; Leonard et al., 2013; Veland et al., 2013; Pennesi et al., 2012; Downing and Cuerrier, 2011). It encompasses detailed local and historical observations of changes associated with climate (Chisholm Hatfield et al., 2018) and is noted for being more inclusive of social elements than is Western science (Ignatowski and Rosales, 2013). Many Indigenous peoples are accustomed and adaptive to environmental change, with Indigenous knowledge providing important perspectives on the relationship between human activity and the environment (see Video 4.2; Leonard et al., 2013; Veland et al., 2013). As noted in Section 4.7.2, Indigenous communities are actively building adaptation strategies based on Indigenous knowledge systems.

Video 4.2: Elder Dave Courchene is a respected Knowledge Keeper of the Anishinaabe Nation and founder of the Turtle Lodge. In this video, he shares his views on climate change, stewardship and Indigenous wisdom. Source: The Turtle Lodge and Prairie Climate Centre, 2017.

Women 

While gender analysis of climate change vulnerability and adaptation has increased substantially over the past decade, studies specific to the Prairie provinces remain limited. Existing literature from other contexts acknowledges that, in general, gender inequality produces different experiences of climate impacts between women and men (Jerneck, 2018). For example, women’s vulnerability to climate change is affected by lower average incomes (Perkins, 2017); gendered divisions of labour—especially in natural resources contexts and rural communities (Fletcher and Knuttila, 2016; Vasseur et al., 2015; Reed et al., 2014; Alston, 2013); unequal access to or control over land, technology and information (Seager, 2014); cultural norms and gender ideologies (Alston and Whittenbury, 2013; Reed et al., 2014); and less decision-making power (Pearse, 2017; Fletcher and Knuttila, 2016; Vasseur et al., 2015; Reed et al., 2014).

The intersection of gender roles and low socio-economic status, for example, may increase vulnerability for women. Income affects people’s ability to cope and adapt to climate extremes. Women across Canada continue to experience a pay gap compared to men, partly attributable to women’s disproportionate participation in part-time employment (Statistics Canada, 2018b), which itself is due in part to women’s ongoing and disproportionate responsibility for caregiving and domestic work (Moyser and Burlock, 2018). Even among full-time workers, statistics show provincial pay gaps of 24.6% in Alberta, 21.6% in Saskatchewan and 13.2% in Manitoba (Conference Board of Canada, 2017). Another major factor influencing this pay gap is the occupational division of labour, in which sectors with a larger representation of women tend to have lower pay levels than male-dominated sectors (Vincent, 2013). Women are also less likely than men to be employed. The three Prairie provinces (plus Ontario) show the highest male-to-female employment gaps in Canada, with 11.3 percentage points for Alberta, 8.8 in Manitoba, and 8.2 in Saskatchewan (Statistics Canada, 2018b).

The percentage of women living in poverty across Canada is consistently higher than the percentage of men in poverty. Of low-wage earners in Alberta, 59.6% are female. In Saskatchewan, 16.9% of women over 65 are in the low-income category, compared to 11.1% of women in the 18‒64 age category and 14.5% of men who are 65 and over (Statistics Canada, 2016). Single mothers, lesbian women, women with disabilities, Indigenous women, women of colour, and women who have been incarcerated often experience more severe financial challenges than other people living in Canada (The Women’s Centre of Calgary, 2017). Transgender people may also experience additional barriers to finding paid work (Trans PULSE, 2011), which could increase their vulnerability. No literature exists on transgender people’s experiences of climate change in the Prairie region; however, research is beginning to explore the challenges faced by lesbian, gay and transgender people experiencing climate disasters elsewhere (e.g., Gorman-Murray et al., 2017; Dominey-Howes et al., 2014; Balgos et al., 2012).

In the Prairie region, available research suggests that rigid gender roles in agriculture, forestry and other resource contexts create different experiences for women and men. Women in agriculture may have less influence over on-farm adaptation decisions, including the use of technologies like drought-resistant seed (Fletcher and Knuttila, 2016). In forestry, women and Indigenous people’s low decision-making power over natural resource management may extend to adaptation strategies (Reed et al., 2014; Reed and Davidson, 2011). Although women are more likely to experience inequality, research in the Prairies (Fletcher and Knuttila, 2016) and elsewhere (e.g., Alston, 2012) has shown that men may experience particular physical and psychological risks due to expectations of masculinity during climate disasters.

The knowledge and capacities of women and other marginalized groups (Moosa and Tuana, 2014) can be valuable contributions to adaptation. Women often play an active, but overlooked role on farms, in households and communities, and during disaster response. The particular roles played by women may give them a different level or type of environmental awareness from men (Fletcher, 2017; Bunce et al., 2016; MacGregor, 2010), yet they continue to be underrepresented in climate governance (Williams, 2018; Pearse, 2017; MacGregor, 2010).

Rural communities 

The general trend of depopulation and urbanization in the Prairie provinces has resulted in reductions in available funding for rural municipalities (Canadian Rural Revitalization Foundation, 2015), and the significant growth in farm size over the past two decades (Statistics Canada, 2017a, 2011a, 2007) has resulted in reductions in social capital and local services that are key elements of adaptive capacity (Desmarais et al., 2015; McLeman, 2010). Dependence on declining water resources for agriculture increases the risk of water conflict between industrial (e.g., oil, gas and mining), agricultural and rural household users (Clark et al., 2017). Financial precarity is an additional vulnerability factor in agriculture (Fletcher and Knuttila, 2016; Pittman et al., 2011; Wittrock et al., 2011; Patiño and Gauthier, 2009), along with lack of institutional support, including federal divestment from drought infrastructure (Shuba et al., 2016; Marchildon, 2009); fragmented flood policy instruments and planning that fails to consider climate projections (Hurlbert, 2018); and volatile markets (Diaz et al., 2016; Patiño and Gauthier, 2009; O’Brien and Leichenko, 2000).

Despite these vulnerabilities, rural residents often have significant adaptive capacity. Rural residents may be more equipped to cope with extreme events than urban residents (McLeman, 2010), and a culture of innovation has helped Prairie farmers adapt to drought over the past century (Warren, 2016a). Strong social capital exists in many rural communities across the Prairies, including cultural norms of mutual assistance during crises (Shuba et al., 2016). As noted in Section 4.7.2, some rural municipalities are carrying out their own adaptation planning processes. Priorities in adaptation planning include participatory planning with increased stakeholder involvement (Hurlbert, 2018; Lal et al., 2011); stable, coherent and consistent policy regimes (Hurlbert, 2018; Pittman et al., 2011); and consideration of climate scenarios in future planning (Hurlbert, 2018).

Low-income families 

Prairie residents living in poverty may be more sensitive to climate extremes as a result of insecure sources of employment, poor quality housing, lack of insurance, lack of financial resources for adaptation and lower representation in decision-making forums. The vulnerability and adaptive capacity of people living in poverty in the Prairies has not yet been the subject of research attention; however, information on poverty in the Prairie provinces can inform consideration of the vulnerability of this group to climate change. Youth, women, racialized and Indigenous people are more likely to hold low-wage, part-time and insecure jobs, accounting for a large proportion of the working poor. Standard poverty rates vary between 9–14% across the prairies, but a more informed measure is the prevalence of low incomes based on low-income measure after tax, which is 13.6% in Alberta, 18.1% in Saskatchewan and 20.7% in Manitoba (Statistics Canada, 2016).

Poverty tends to be concentrated in certain rural communities and also in inner cities, which in certain cases may be more exposed to climate-induced hazards than other regions; for example, when poor housing is associated with inner-city neighbourhoods or when economically depressed rural communities lack the capacity to maintain infrastructure. Lone parent families also make up a large proportion of this group, particularly female-headed households. By extension, rates of child poverty are significantly higher than poverty rates for the population as a whole. The percentage of children living in poverty is 15.7% in Alberta (Edmonton Social Planning Council, 2017a), 24% in Saskatchewan (Hunter and Sanchez, 2017) and 27.5% in Manitoba (Campaign 2000, 2017). The elderly and people with pre-existing health conditions are especially susceptible to heat waves and other climate extremes (Rapaport et al., 2015), and those with lower incomes often have no access to air conditioners (Gronlund, 2014).

Recent immigrants 

Recent immigrants are rarely studied in climate change research; however, they represent a significant number of residents in many Prairie communities and can be subject to multiple sources of vulnerability. The lack of resources and the language barriers faced by some immigrants can limit adaptive capacity (Burke et al., 2012). Seasonal migrant workers not only experience the vulnerabilities of the average migrant, but also the precarity of work in the agricultural sector under climate change. Refugees in particular may be suffering from trauma due to experiences in their native countries, and many are visible minorities who may be subject to racial discrimination; even children experience this range of effects (Oxman-Martinez et al., 2012). Many recent immigrants are unfamiliar with the sources of social support that may be available. Each of these factors enhances vulnerability to climate change, particularly extreme events.

This group is expected to grow, in part due to increases in out-migration in response to climate change impacts in other parts of the world (see International Dimensions chapter). Alberta, in particular, is becoming a preferred destination for immigrants, after Ontario and British Columbia, with landed immigrants currently making up 23.6% of the working population (Government of Alberta, 2018). In 2015, 16,739 immigrants and refugees settled in Edmonton, compared to 6,016 in 2005 (Edmonton Social Planning Council, 2017b).

4.6.3

Sources of social vulnerability

Consideration of vulnerability that focuses exclusively on exposure, sensitivity and adaptive capacity may perpetuate disempowerment rather than enabling capacity building (Veland et al., 2013). For example, depictions of Indigenous peoples as highly vulnerable may serve to reproduce the paternalistic relations reflected in colonialism (Klenk et al., 2013; Veland et al., 2013). GHG emissions reduction and adaptation strategies can reinforce Western, masculine and/or technocratic approaches and male-dominant economic sectors (Williams, 2018). For example, the dominant approach to climate change adaptation favours infrastructure and technological solutions, like dams and zero-till agriculture, over more socially integrative approaches that attend to structural inequalities, social vulnerabilities and institutional barriers (VandenBygaart, 2016; Zeitoun et al., 2016).

Intersectional analysis (see Box 4.4) draws attention to the fact that nearly 80% of single parents in Canada are female (Statistics Canada, 2015). When combined with the gender pay gap, the intersection of gender and single-parent status may also affect vulnerability and contribute to child poverty. Similarly, although older adults in general are more likely than other age categories to be low-income (Hunter, 2011), the incomes of older men (65 and over) are still 1.5 times that of older women (Statistics Canada, 2018b), and more than 30% of older women live alone compared to 16% of older men (Statistics Canada, 2018b). In the Prairie region, intersectional analysis reveals particular issues experienced by low-income Indigenous women living on reserve, as compared to their non-Indigenous, male, off-reserve counterparts: Indigenous women are more likely to be lone parents and less likely to be employed than men and non-Indigenous women; they are more likely to live in poor housing on reserve and are self-reporting worse health conditions than Indigenous men (Arriagada, 2016).

Individuals characterized by intersecting causes of vulnerability also have important knowledge to contribute to climate change adaptation because of their perspectives and experience (Whyte, 2014). Both Indigenous women and men may possess unique knowledge about the environment and climatic change (Dowsley et al., 2010), generated through their traditional gender roles and responsibilities. Indigenous women’s roles as water protectors, for example, may provide insights into climate change (Whyte, 2014). Older individuals, including male and female Indigenous Elders, hold important knowledge that corroborates and expands upon scientific climate records. The knowledge and contributions of socially marginalized groups can provide crucial insight for more effective and inclusive climate change adaptation moving forward. Furthermore, socially equitable adaptation policies and processes can go beyond inclusion, reducing the root causes of vulnerability and potentially increasing equality over time.

4.7

Adaptation planning helps to reduce climate risks

Cities are at the forefront of adaptation and resilience planning in the Prairie provinces. Governments and businesses have begun to assess climate risks and develop adaptation strategies, but few sector-specific plans and policies consider future climate risks, leaving some firms, governments and sectors unprepared. Assessing the effectiveness of adaptation measures and meaningful reporting of progress would help achieve climate-resilient communities and local economies.

Governments, industry, businesses, Indigenous communities and civil society across the Prairie provinces are slowly embracing adaptation planning. Leadership is particularly evident from municipalities in the region, while provincial governments are in the early stages. Governments and corporations have begun to assess and disclose climate risks facing public and private assets. Continuous improvement through the evaluation of progress is not common. Another limitation is the continued reliance on recent historic climate conditions for defining climate variability and extremes, rather than referring to future climate projections. 

4.7.1

Introduction

Climate change considerations are increasingly included in planning and management processes in municipalities, governments and businesses with diverse operational and management objectives (City of Regina, 2018; TransAlta Corporation, 2018; EPCOR, 2017). Ongoing adaptation projects and initiatives include fostering engagement and raising awareness, research and planning, training and skills development, and infrastructure design and construction from a climate perspective (Blackfeet Nation, 2018; Bruised Head, 2018; Austin, 2015; Zizzo, 2014).

Saskatchewan and Manitoba have climate change plans that include adaptation, reducing GHG emissions and building climate resilience. Saskatchewan’s climate change strategy (Government of Saskatchewan, 2017) emphasizes existing government practices (e.g., research to support the adoption of new crop varieties) and commits to new strategies to enhance climate resilience within the province (e.g., improving understanding of future climate trends). Manitoba’s Climate and Green Plan (Manitoba Sustainable Development, 2017) is based on four pillars: climate, jobs, water and nature. Adaptation strategies in the plan focus on climate knowledge, sustainable climate-resilient communities and sustainable agriculture.

4.7.2

Community-based adaptation planning and action

Under provincial legislation, Alberta’s two largest cities are required to develop climate change plans (see Case Story 4.5; Government of Alberta, 2018). Thirteen other municipalities in Alberta have adopted adaptation plans that were developed using the Climate Resilience Express process (Boyd et al., 2016). This streamlined adaptation planning process is based on a one-day workshop that explores climate risks to municipal assets and operations. Rather than presenting a detailed quantitative analysis, the high-level screening approach is meant to be simple and accessible to communities with limited capacity. The output is an action plan for communities that requires implementation, review and updates. The process has been used to produce plans for numerous cities, towns and counties.

The City of Saskatoon’s Climate Action Plan, which includes its Corporate Climate Adaptation Strategy, was released in 2019 (City of Saskatoon, 2019). It undertook an engagement process—focus groups, surveys, pop-up community events and expert workshops—with local businesses, not-for-profit organizations, residents and subject matter experts to inform their Climate Change Business Mitigation Plan (Lura Consulting, 2018). Stakeholders identified climate change activities of interest and potential risks of concern, as well as potential benefits. Upfront costs, lack of infrastructure or services, and lack of responsibility and support were identified as the largest barriers to greater action.

The City of Selkirk, Manitoba, developed its climate change adaptation strategy by considering the seasonal impacts of climate change on municipal assets, local services, and human health and well-being, and by prioritizing risks and associated adaptation actions. Actions were ranked for their efficacy, and costs were calculated and integrated into the City’s annual tactical budgeting process to support implementation. The City won the 2019 Tereo Award from the Canadian Network of Asset Managers in recognition of their innovative approach and commitment to climate action (City of Selkirk, 2019).

Indigenous communities in the Prairie provinces are also very active in adaptation planning (Crown-Indigenous Relations and Northern Affairs Canada, 2019). Common areas of focus among adaptation projects include food security and access to traditional foods, safety while on the land, water monitoring, and physical and mental impacts of climate change (Myers et al., 2017).

Adaptation planning in Prairie Indigenous communities often considers Indigenous and local knowledge, along with climate change science and projections (Bruised Head, 2018; Okorosobo, 2018; Patrick, 2018a). For example, the Blackfeet Climate Change Adaptation Plan (Blackfeet Nation, 2018) is informed by cultural observations of climate change impacts and Amskapi Piikani records kept through oral tradition and history. Stories of seasonal hunts, warrior activities, social obligations, gatherings of nations and many other important events have been maintained through oral retellings over hundreds of generations. Climate change is now emerging in these stories as they advance into the present and future. Science-based climate trends and projections were also used to develop the plan, which is built around sector-specific vulnerabilities and impacts. Goals, strategies and actions for climate change adaptation in eight sectors—including agriculture, water and forestry—are based on the Blackfeet understanding that people and nature are one, and that people can only be healthy if the health of the environment is also ensured. A dynamic view of the natural world and recognition of its reciprocal relationship with the Blackfeet is considered necessary to balance the needs of all (see Case Story 4.5).

Models are emerging for braiding together Indigenous knowledge and climate science in climate change adaptation planning. For example, Lynes and Boyd (2018) describe a planning process to develop a Local Early Action Plan, comprising strategies and actions to cope with and adapt to immediate priorities identified by Indigenous communities. The process includes a series of educational workshops and community dialogues, followed by an adaptation workshop. Climate change experts and local knowledge holders deliver joint workshops and dialogues with concepts translated into local oral and written language.

4.7.3

Adaptation mainstreaming

Mainstreaming is the systematic analysis of climate risk and inclusion of adaptation in decision-making and planning processes. Government staff in Manitoba and Saskatchewan assessed the adaptability of provincial policies to climate change and their ability to support sectoral adaptation. Participants identified opportunities to build the policy flexibility needed in an uncertain future climate (Bizikova, 2018). Assessments were most useful when climate change response was articulated as a policy goal, either during initial policy design or after policies had been in effect for some time, so that there was some evidence of their effectiveness.

Analysis and planning for water use and management in the Prairie provinces increasingly examine the implications of climate change (TransAlta Corporation, 2018; Patrick, 2018b). For example, a collaborative exploration of water management in the Oldman and South Saskatchewan river basins examined streamflow scenarios for the period of 2025 to 2054 (Sauchyn et al., 2016). Potential adaptation strategies, such as modifying existing infrastructure, building new infrastructure, changing operations to supplement environmental flows, reducing demand and sharing supply, were assessed in interactive modelling sessions. Findings indicate that forecast-based rationing, together with new expanded storage, could dramatically reduce water shortages. Similarly, Manitoba Hydro’s climate change strategy (Manitoba Hydro, 2014) is informed by climate change projections and numerous studies across the Nelson-Churchill Watershed that highlight important spatial and temporal patterns in how climate change may affect its core business.

Governments and corporations are also starting to disclose climate risks to public and private assets (see Climate Disclosure, Litigation and Finance chapter). For example, Suncor (Suncor Energy Inc., 2018) reported that it is managing climate risks through facility design, operational procedures and insurance for damage to, or loss of, assets, as well as production interruption. TransAlta Corporation (2018) similarly notes that it has experienced negative financial impacts from extreme climate events and is using insurance, retirement of older facilities, improved drainage infrastructure and the stockpiling of supplies to address risks. The company has used climate modelling and past costs to estimate possible future financial implications of the reduction or disruption of production capacity in a changing climate, as well as potential positive financial benefits (TransAlta Corporation, 2018). Risk controls include using dams for flood and drought control, capital maintenance, monitoring weather patterns and adjusting site operations.

4.7.4

Limitations of current adaptation and resilience planning

While most policies currently in place do not take future climate into account, adaptive management—an iterative approach to decision-making in the face of uncertainty—provides flexibility and potential for learning as climate conditions in the Prairies change. Adaptive management is designed to be more flexible and responsive to changing local conditions, and is centered on evidence-based decision-making that aims to reduce uncertainty through monitoring, experimentation and learning (Holling, 1978). For example, several energy and environmental policies governing the oil and gas sector in Alberta reflect adaptive management principles, which could allow operators to adjust as climatic conditions change (Cobb et al., 2015). However, a lack of attention to experimental design and vague or unenforceable reporting requirements can limit actual learning, and undermine the adaptive nature of this approach (Olszynski, 2017). Furthermore, widely varying opinions about climate change and its impacts on the oil and gas sector in western Canada (Wiensczyk, 2014) suggest that some firms, governments and sectors will rely on reactive adaptation measures, and may not be preparing for rapid climate change or environmental and socio-economic tipping points—which cause changes into new or different states (e.g. water for irrigation agriculture became unreliable after three dry decades, as described in Warren, 2016b).

A lack of determination or motivation to address climate change can also limit opportunities for institutional learning. An examination of the evolution of Manitoba’s emergency and disaster management system found that, while extreme events generated opportunities for significant learning, policy changes were largely reactive initiatives driven by top-down decision-making, with reduced institutional evolution relative to other policy issues (Haque et al., 2018). Moreover, certain organizations may be reluctant to disclose climate risks due to concerns about company stock value or legal liability (see Climate Disclosure, Litigation, and Finance chapter). Some industry reporting may even conceal climate change impacts, lessening incentive for a better understanding or management of climate risks (Quest, 2015).

To enhance adaptation overall, adaptation planning requires regular evaluation of effectiveness, revision based on learnings, and enhanced progress reporting of what is being learned about climate change and adaptation in the Prairies. However, the limited reporting on progress delivered thus far has primarily focused on actions taken. For example, in Manitoba, provincial reporting on climate change and independent reporting from various government departments spoke to climate change risks and adaptation activity, but did not address the extent to which actions were successful at reducing or minimizing the most significant risks (Manitoba’s Auditor General, 2017).

While adaptation-related performance metrics and the measurement of adaptation goal achievement are not yet common (Auditors General, 2018; Government of Saskatchewan, 2018), Saskatchewan has developed a framework for measuring progress achieved in making the province more resilient to climate change. Saskatchewan’s Climate Change Strategy (Government of Saskatchewan, 2017) describes climate resilience and focuses on the principles of readiness, with a commitment to annual assessment and reporting. The strategy consists of 25 indicators of climate change in five key areas: natural systems, physical infrastructure, economic sustainability, community preparedness and human well-being (Government of Saskatchewan, 2018). This framework will enable the provincial government to track and report on progress in building resilience to climate change.

Another limitation of adaptation planning is the continued reliance on recent historic climate conditions to define future climate variability and extremes. Risk assessments often do not consider extremes outside the range of recorded observation (Sauchyn et al., 2014). Prolonged droughts, such as those that occurred during the period from the 1920s to the early 1940s, are a common feature of climate history in the Prairies, but predate such major industrial allocation of surface water as is used in oil and gas extraction. Taking such extremes into account in planning processes can help in identifying adaptation measures that may be robust enough to address low-probability, high-impact climate change climate change scenarios that would have profound implications for water users (e.g., EPCOR, 2017; Sauchyn et al., 2015).

4.8

Moving forward

4.8.1

Knowledge gaps and research needs

The assessment of current knowledge presented in this chapter reveals gaps and needs for further research. Foremost among these are indicators and methodologies for assessing the effectiveness of strategies and actions that have been implemented. Other key knowledge gaps and needs include:

Best practices and guidance for:

  • Incorporating model projections of future climate scenarios into adaptation planning. Many risk assessment processes are based on the analysis of recent historical climate scenarios. Without efforts to consider future climate projections in decision-making—as well as uncertainty in the projections of future climate—some firms, governments and sectors may not be sufficiently prepared; and
  • Establishing, implementing, measuring and modifying the monitoring and evaluation of progress towards achieving climate resilience goals.

Improved understanding of:

  • New opportunities arising from climate change;
  • How agriculture could expand beyond the margins of the Prairie Ecozone and into treed zones of nutrient-poor forest soils;
  • The social, environmental and economic impacts of sustained (multi-year) drought and of prolonged inundation of land under excessive wet conditions;
  • The vulnerability and adaptive capacity of specific social groups, including low-income families and recent immigrants, and in particular differences between urban Indigenous populations and those in remote and rural communities; and
  • How Indigenous knowledge can enhance adaptation and sustainable practices, and how to integrate Indigenous knowledge into adaptation planning processes.
4.8.2

Emerging issues

This assessment of the current knowledge of climate change impacts and adaptation in the Prairie provinces indicates the following emerging issues:

Transformational adaptation

As a warming climate amplifies regional weather extremes, the severity of floods, storms and droughts will exceed the historical experience of Prairie communities. Incremental adjustments made to historical practices and policies are unlikely to deliver adequate adaptation to the evolving hydroclimate and could potentially be maladaptive over time. Therefore, a significant emerging issue is the need for transformational adaptation that challenges existing policies, structures and systems.

Adaptation in rural communities

Recent rural social and economic trends, rural depopulation and increasing farm size, in particular, are factors that undermine the adaptive capacity of rural communities. Extension services in rural areas, previously provided by Prairie universities and government agencies, have diminished. Watershed stewardship groups and rural municipalities now provide these services to some extent, but lack the resources for adaptation planning.

Social and cultural considerations in adaptation decisions

Conventional approaches to evaluating the vulnerability of social groups based on indicators of exposure and adaptive capacity do not take into account cultural understandings of values and risk, local knowledge, certain causal factors of inequality and oppression, and unique capacities for agency, including contributions and insights derived from marginalized perspectives such as Indigenous knowledge and women’s experiences.

Intersectionality perspectives

Positive emerging trends include an emphasis on climate policy and planning, and innovative approaches to accessing and interpreting knowledge to inform these processes, including integrating Indigenous understanding of climate change and adaptation (Lynes and Boyd, 2018; Myers et al., 2017). The emerging intersectionality perspective recognizes how multiple attributes and identities can intersect to affect vulnerability and adaptive capacity, while a focus on social infrastructure can draw attention to whether and how existing practices can be retained or revised for positive adaptation.

4.9

Conclusion

In the Prairie provinces, climate change is resulting in a redistribution of natural capital. It is transforming the seasons towards wetter winters and drier summers, and requiring changes to water resource management. The transition to a new distribution of water supplies and new regional ecosystems will be punctuated by phases of change as global warming interacts with regional variability and weather events. Collaboration among governments, municipalities and Indigenous communities is required to deal with the geographic shifts in the availability of water and ecological resources.

As climate change alters the frequency and intensity of extreme weather, the longer-term risks posed by climate change will include an amplified range of water levels and associated consequences: flooding, fire, water supply deficits, disturbance to ecosystems, and more variable forest and farm productivity. The increasing intensity of weather events represents an expanding deviation from a baseline climate, recognizing that the baseline, meanwhile, is also shifting. This ongoing state of change may ultimately be the most challenging scenario. Eventually temperature, precipitation and water levels will cross a threshold beyond which impacts will abruptly become more severe. Examples include the permanent loss of water stored as snow and ice, rainfall intensity that exceeds the watershed and storage capacity of infrastructure, and the loss of low temperatures that inhibit many pest and disease vectors from proliferating in agricultural and forested regions.

The response to climate change in the Prairie provinces has transitioned from recognizing to responding to potential impacts. Government agencies, private industry, Indigenous communities, municipalities and regional community organizations (e.g., watershed stewardship agencies, irrigation districts) are now engaged in resilience and adaptation planning. The net impacts of regional climate change will depend on the success, extent and scope of adaptation planning and its effective implementation. Plans have emerged in the past decade, and adaptation planning is on the agenda of many municipalities, corporations, industry associations and civic organizations. Each of the provincial governments in the Prairies has a climate strategy that incorporates adaptation, and most of the major cities are engaged in resilience planning, although implementation is in the early stages.

References

Learn more
  1. 100 Resilient Cities (2020). Retrieved June 2020, from: https://www.100resilientcities.org/
  2. Adger, W.N., Barnett, J., Brown, K., Marshall, N., and O’Brien, K. (2012). Cultural dimensions of climate change impacts and adaptation. Nature Climate Change, 3(2), 112‒117. Retrieved June 2020, from https://doi.org/10.1038/nclimate1666
  3. Agriculture and Agri-Food Canada (2017). What we heard: First Nation outreach sessions, spring 2017. Government of Canada, Ottawa, Ontario. Retrieved June 2020 from http://www.agr.gc.ca/eng/about-us/key-departmental-initiatives/working-with-indigenous-peoples-in-canadian-agriculture/building-relationships-with-indigenous-peoples/what-we-heard-first-nation-outreach-sessions-spring-2017/?id=1527720564716
  4. Agriculture and Agri-Food Canada (2019). Drought Watch Website. Retrieved June 2020, from http://www.agr.gc.ca/DW-GS/historical-historiques.jspx?lang=eng&jsEnabled=true,
  5. Alam, M.S. and Elshorbagy, A. (2015) Quantification of the climate change-induced variations in Intensity-Duration-Frequency curves in the Canadian Prairies. Journal of Hydrology 527 (2015), 990‒1005. Retrieved June 2020, from https://doi.org/10.1016/j.jhydrol.2015.05.059
  6. Alberta Agriculture and Forestry (2016). Alberta’s Agriculture Drought and Excess Moisture Risk Management Plan. Government of Alberta. 36p. Retrieved June 2020, from https://open.alberta.ca/publications/alberta-s-agriculture-drought-and-excess-moisture-risk-management-plan
  7. Albert-Green, A., Dean, C.B., Martell, D.L., and Woolford, D.G. (2013). A methodology for investigating trends in changes in the timing of the fire season with applications to lightning-caused forest fires in Alberta and Ontario, Canada. Canadian Journal of Forest Research, 43(1), 39-45. Retrieved June 2020, from https://doi.org/10.1139/cjfr-2011-0432
  8. Alston, M. (2012). Rural male suicide in Australia. Social Science & Medicine, 74(4), 515-522. Retrieved June 2020, from https://doi.org/10.1016/j.socscimed.2010.04.036
  9. Alston, M. (2013). Gender mainstreaming and climate change. Women’s Studies International Forum. Retrieved June 2020, from https://doi.org/10.1016/j.wsif.2013.01.016
  10. Alston, M. and Whittenbury, K. (2013). Does climatic crisis in Australia’s food bowl create a basis for change in agricultural gender relations? Agriculture and Human Values, 30(1), 115-128. Retrieved June 2020, from https://doi.org/10.1007/s10460-012-9382-x
  11. Arora-Jonsson, S. (2011). Virtue and vulnerability: Discourses on women, gender and climate change. Global Environmental Change, 21(2), 744‒751. Retrieved June 2020, from https://doi.org/10.1016/j.gloenvcha.2011.01.005
  12. Arriagada, P. (2016). First Nations, Métis and Inuit Women. Women in Canada: A Gender-Based Statistical Report No. 89-503- X. Ottawa, Ontario Statistics Canada.
  13. Auditors General (2018). Perspectives on Climate Change Action in Canada. The Auditor General of Canada. Retrieved June 2020, from https://www.oag-bvg.gc.ca/internet/English/parl_otp_201803_e_42883.html
  14. Austin, S. E., Ford, J. D., Berrang-Ford, L., Araos, M., Parker, S., and Fleury, M. D. (2015). Public health adaptation to climate change in Canadian jurisdictions. International Journal of Environmental Research and Public Health, 12(1), 623‒651. Retrieved June 2020, from https://doi.org/10.3390/ijerph120100623
  15. Baggio, J.A., BurnSilver, S.B., Arenas, A., Magdanz, J.S., Kofinas, G.P., and De Domenico, M. (2016). Multiplex social ecological network analysis reveals how social changes affect community robustness more than resource depletion. Proceedings of the National Academy of Sciences, 113(48), 13708‒13713. Retrieved June 2020, from https://doi.org/10.1073/pnas.1604401113
  16. Balgos, B., Gaillard, J.C., and Sanz, K. (2012). The warias of Indonesia in disaster risk reduction: The case of the 2010 Mt Merapi eruption in Indonesia. Gender & Development, 20(2), 337‒348. Retrieved June 2020, from https://doi.org/10.1080/13552074.2012.687218
  17. Barrow, E. and Sauchyn, D. (2019). Uncertainty in climate projections and time of emergence of climate signals in the western Canadian Prairies. International Journal of Climatology. 39(11) 4358‒4371.  Retrieved June 2020, from https://doi.org/10.1002/joc.6079
  18. Bedford, F., Whittaker, R., and Kerr, J. (2012). Systemic range shift lags among a pollinator species assemblage following rapid climate change. Botany 90, 587‒597. Retrieved June 2020, from https://doi.org/10.1139/b2012-052
  19. Berteaux, D., de Blois, S., Angers, J., Bonin, J., and Casajus, N. (2010). The CC-Bio Project: studying the effects of climate change on Quebec biodiversity. Diversity 2, 1181‒1204. Retrieved June 2020, from https://doi.org/10.3390/d2111181
  20. Bizikova, L., Swanson, D., Tyler, S., Roy, D., and Venema, H.D. (2018). Policy adaptability in practice. Policy Design and Practice 1(1), 47‒62. https://doi.org/10.1080/25741292.2018.1436376
  21. Blackfeet Nation (2018). Blackfeet Nation Climate Change Adaptation Plan. Browning, Montana. 129 p.
  22. Blair, D. and Sauchyn, D. (2010). Winter roads in Manitoba. Chapter 20 in The New Normal: The Canadian Prairies in a Changing Climate. (Eds.) D. Sauchyn, H. Diaz and S. Kulshreshtha Canadian Plains Research Center Press, Regina, Saskatchewan, 322‒325.
  23. Bonsal, B.R., Peters, D.L., Seglenieks, F., Rivera, A., and Berg, A. (2019). Changes in freshwater availability across Canada, Chapter 6 in Canada’s Changing Climate Report, (Eds.) E. Bush and D.S. Lemmen. Government of Canada, Ottawa, Ontario, 261‒342. Retrieved June 2020, from https://changingclimate.ca/CCCR2019/chapter/6-0/
  24. Bush, E., Gillett, N., Watson, E., Fyfe, J., Vogel, F. and Swart, N. (2019): Understanding observed global climate change, Chapter 2 in Canada’s Changing Climate Report, (Eds.) E. Bush and D.S. Lemmen. Government of Canada, Ottawa, Ontario, 25‒72. Retrieved June 2020, from https://changingclimate.ca/CCCR2019/chapter/2-0/
  25. Bonsal, B. R., Wheaton, E.E., Chipanshi, A.C., Lin, C., Sauchyn, D.J., and Wen, L. (2011) Drought Research in Canada: A Review, Atmosphere-Ocean 49(4) 303‒319. Retrieved June 2020, from https://doi.org/10.1080/07055900.2011.555103
  26. Boucher, D., Boulanger, Y., Aubin, I., Bernier, P., and Beaudoin, A. (2018). Current and projected cumulative impacts of fire, drought, and insects on timber volumes across Canada. Ecological Applications 28, 1245‒1259. Retrieved June 2020, from https://doi.org/10.1002/eap.1724
  27. Bow River Water Management Project (2017). Advice to Government on Water Management in the Bow River Basin. Environment and Parks, Edmonton, Alberta. 226 p.
  28. Boyd, R., Zukiwsky, J., Reasoner, M., Stark, C., Corbett, H., et al (2016) Climate Resilience Express Action Kit and Municipal Action Plans. Retrieved June 2020, from https://www.allonesky.ca/climate-resilience-express
  29. Brimelow, J., Stewart, R., Hanesiak, J., Kochtubajda, B., Szeto, K., Bonsal, B. (2014). Characterization and assessment of the devastating natural hazards across the Canadian Prairie Provinces from 2009 to 2011, Natural Hazards 73, 761‒785. Retrieved June 2020, from https://doi.org/10.1007/s11069-014-1107-6
  30. Bruised Head, D. (2018). Building Climate Resilience and Adaptation in the Kainai First Nation. Blood Tribe Land Management, Standoff, Alberta.19 p.
  31. Bunce, A., Ford, J., Harper, S., Edge, V., and IHACC Research Team. (2016). Vulnerability and adaptive capacity of Inuit women to climate change: a case study from Iqaluit, Nunavut. Natural Hazards, 83, 1419‒1441. Retrieved June 2020, from https://doi.org/10.1007/s11069-016-2398-6
  32. Burke, S., Bethel, J.W., and Britt, A.F. (2012). Assessing Disaster Preparedness among Latino Migrant and Seasonal Farmworkers in Eastern North Carolina. International Journal of Environmental Research and Public Health, 9(9), 3115‒3133. Retrieved June 2020, from https://doi.org/10.3390/ijerph9093115
  33. Cameron, E.S. (2012). Securing Indigenous politics: A critique of the vulnerability and adaptation approach to the human dimensions of climate change in the Canadian Arctic. Global Environmental Change, 22(1), 103‒114. Retrieved June 2020, from https://doi.org/10.1016/j.gloenvcha.2011.11.004
  34. Campaign 2000 (2017). Manitoba Child and Family Report Card 2017. Waiting for the Plan. Retrieved June 2020, from https://campaign2000.ca/wp-content/uploads/2017/11/2017-MB_ChildFamilyPovReportCard_FINAL.pdf
  35. Canadian Rural Revitalization Foundation (2015). State of Rural Canada 2015. Rural Development Institute, Brandon University, Brandon, Manitoba. 114 p. Retrieved June 2020, from http://sorc.crrf.ca/wp-content/uploads/2015/09/SORC2015.pdf
  36. Champagne, C., Berg, A., McNairn, H., Drewitt, G., Huffman, T. (2012). Evaluation of Soil Moisture Extremes for Agricultural Productivity in the Canadian Prairies. Agricultural and Forest Meteorology 165, 1-11. Retrieved June 2020, from https://doi.org/10.1016/j.agrformet.2012.06.003
  37. Chisholm Hatfield, S., Marino, E., Whyte, K.P., Dello, K.D., and Mote, P.W. (2018). Indian time: time, seasonality, and culture in Traditional Ecological Knowledge of climate change. Ecological Processes, 7(1). Retrieved June 2020, from https://doi.org/10.1186/s13717-018-0136-6
  38. Christianson, A., McGee, T.K., and L’Hirondelle, L. (2012). Community support for wildfire mitigation at Peavine Métis Settlement, Alberta, Canada. Environmental Hazards, 11(3), 177‒193. Retrieved June 2020, from https://doi.org/10.1080/17477891.2011.649710
  39. City of Calgary (2017). Flood Mitigation Measures Assessment Report and 2016 Flood Resiliency Update. Report to Special Policy Committee on Utilities and Corporate Services. Presented on March 22, 2017. Retrieved June 2020, from https://www.calgary.ca/UEP/Water/Pages/Flood-Info/Stay-informed/Flood-Mitigation-Measures-Assessment.aspx
  40. City of Calgary (2018). Climate Resilience Strategy, Mitigation and Adaptation Action Plans. City of Calgary Council approval of strategy June 25, 2018. Retrieved June 2020, from http://www.calgary.ca/UEP/ESM/Documents/ESM-Documents/Climate_Resilience_Plan.PDF
  41. City of Calgary (2019a). Honouring commitments to Calgary. Retrieved June 2020, from http://www.calgary.ca/citycouncil/YYCmatters/Pages/pillar1.aspx#BuildSpringbankReservoir
  42. City of Calgary (2019b). Calgary’s Flood Resilience Plan. Retrieved June 2020, from https://www.calgary.ca/uep/water/flood-info/mitigation-and-resilience/flood-projects.html
  43. City of Regina (2018). Impact of Climate Change in Regina. Retrieved from City of Regina: https://www.regina.ca/business/environment/climate-change/climate-change-regina/
  44. City of Edmonton (2018a). Climate Resilient Edmonton: Adaptation Strategy and Action Plan. City of Edmonton, Edmonton, Alberta. Retrieved June 2020, from https://www.edmonton.ca/city_government/documents/Climate_Resilient_Edmonton.pdf
  45. City of Edmonton (2018b). Change for Climate Edmonton Declaration. Retrieved June 2020, from https://www.edmonton.ca/city_government/environmental_stewardship/change-for-climate-edmonton-declaration.aspx
  46. City of Edmonton (2018c). Climate change vulnerability and risk assessment workshops: Graphic summaries. Retrieved June 2020, from https://www.edmonton.ca/city_government/environmental_stewardship/graphic-summaries.aspx
  47. City of Selkirk (2019) Climate Change Adaptation Strategy 2019‒2029, Selkirk, Manitoba, 57 p. Retrieved June 2020, from https://www.myselkirk.ca/wp-content/uploads/2019/07/Climate-Change-Adaptation-Strategy-Final-May2019.pdf
  48. Clark, R., Andreichuk, I., Sauchyn, D., McMartin, D. (2017). Incorporating climate change scenarios and water-balance approach to cumulative assessment models of solution potash mining in the Canadian Prairies. Climatic Change, 145(3), 321‒334. Retrieved June 2020, from https://doi.org/10.1007/s10584-017-2099-5
  49. Cobb, P., D’Souza, D., Switzer, J., and Douglas, A. (2015). Role of Policy in Oil and Gas Adaptation: An analysis of policy drivers and barriers in the Alberta Oil and Gas Sector. Submitted to Climate Change Impacts and Adaptation Division, Natural Resources Canada, Ottawa, Ontario. 73 p.
  50. Cohen, S., Bush, E., Zhang, X., Gillett, N., Bonsal, B., Derksen, C., Flato, G., Greenan, B., Watson, E. (2019). Synthesis of findings for Canada’s regions, Chapter 8 in Canada’s Changing Climate Report, (Eds.) E. Bush and D.S. Lemmen. Government of Canada, Ottawa, Ontario, 424‒443. Retrieved June 2020, from https://changingclimate.ca/CCCR2019/chapter/8-0/
  51. Conference Board of Canada. (2017). How Canada performs: Gender wage gap. Conference Board of Canada. Retrieved June 2020, from https://www.conferenceboard.ca/hcp/provincial/society/gender-gap.aspx?AspxAutoDetectCookieSupport=1
  52. Convery, F.J. and Wagner, G. (2015). Reflections-Managing Uncertain Climates: Some Guidance for Policy Makers and Researchers. Review of Environmental Economics and Policy, 9(2), 304‒320. Retrieved June 2020, from https://doi.org/10.1093/reep/rev003
  53. Corlett, R. and Westcott, D. (2013). Will plant movements keep up with climate change? Trends in Ecology & Evolution 28, 482‒488. Retrieved June 2020, from https://doi.org/10.1016/j.tree.2013.04.003
  54. COSEWIC [Committee on the Status of Endangered Wildlife in Canada] (2006). COSEWIC Assessment and Update Status Report on the Burrowing Owl, Athene cunicularia, in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa, Ontario. Retrieved December 2020, from https://www.canada.ca/en/environment-climate-change/services/species-risk-public-registry/cosewic-assessments-status-reports/burrowing-owl/chapter-1.html
  55. Craft, K., Mahmood, R., King, S., Goodrich, G., Yan, J. (2017). Droughts of the twentieth and early twenty-first centuries: Influences on the production of beef and forage in Kentucky, USA. Science of the Total Environment 577, 122‒135 Retrieved June 2020, from doi.org/10.1016/j.scitotenv.2016.10.128
  56. Crown-Indigenous Relations and Northern Affairs Canada (2019). First Nations Adapt Program. Retrieved June 2020, from https://www.aadnc-aandc.gc.ca/eng/1481305681144/1481305709311
  57. Cunsolo Willox, A., Harper, S.L., Ford, J.D., Landman, K., Houle, K., and Edge, V.L. (2012). “From this place and of this place:” Climate change, sense of place, and health in Nunatsiavut, Canada. Social Science & Medicine, 75(3), 538‒547. Retrieved June 2020, from https://doi.org/10.1016/j.socscimed.2012.03.043
  58. Dawe, K. and S. Boutin. (2016). Climate change is the primary driver of white-tailed deer (Odocoileus virginianus) range expansion at the northern extent of its range; land use is secondary. Ecology and Evolution 6(18), 6435-6451. Retrieved June 2020, from https://doi.org/10.1002/ece3.2316
  59. Desmarais, A.A., Qualman, D., Magnan, A., and Wiebe, N. (2015). Land grabbing and land concentration: Mapping changing patterns of farmland ownership in three rural municipalities in Saskatchewan, Canada. Canadian Food Studies / La Revue canadienne des études sur l’alimentation, 2(1), 16-47. Retrieved June 2020, from https://doi.org/10.15353/cfs-rcea.v2i1.52
  60. Diaz, H.P., Hurlbert, M., and Warren, J.W. (2016). Vulnerability and adaptation to drought: The Canadian prairies and South America. Energy, ecology, and the environment series; no. 9. University of Calgary Press, Calgary, Alberta. Retrieved June 2020, from http://hdl.handle.net/1880/51490
  61. Dominey-Howes, D., Gorman-Murray, A., and McKinnon, S. (2014). Queering disasters: On the need to account for LGBTI experiences in natural disaster contexts. Gender, Place & Culture, 21(7), 905‒918. Retrieved June 2020, from https://doi.org/10.1080/0966369X.2013.802673
  62. Downing, A. and Cuerrier, A. (2011). A synthesis of the impacts of climate change on the First Nations and Inuit of Canada. Indian journal of traditional knowledge 10(1), 57‒70. Retrieved June 2020, from https://www.semanticscholar.org/paper/A-synthesis-of-the-impacts-of-climate-change-on-the-Downing-Cuerrier/02302b6430553b2315f19fc57adc973f615afb90
  63. Dowsley, M., Gearheard, S., Johnson, N., and Inksetter, J. (2010). Should we turn the tent? Inuit women and climate change. Inuit Studies, 34(1), 151‒165. Retrieved June 2020, from https://doi.org/10.7202/045409ar
  64. Edmonton Social Planning Council (2017a). Keep Investing in Alberta’s Children: The Government’s Role in Ending Child and Family Poverty. Retrieved June 2020, from https://campaign2000.ca/wp-content/uploads/2017/11/AB-Child-Poverty-Report-2017-FINAL-for-releaseNov24.pdf
  65. Edmonton Social Planning Council (2017b). A Profile of Poverty in Edmonton Update. February. Retrieved June 2020, from ESPC Documents/PUBLICATIONS/A.06.C RESEARCH UPDATES/CityOfEdmontonPovertyProfileUpdate_2017.pdf
  66. Edwards, J., Pearce, C., Ogden, A.E., and Williamson, T.B. (2015). Climate Change and Sustainable Forest Management in Canada: A Guidebook for Assessing Vulnerability and Mainstreaming Adaptation into Decision Making. Canadian Council of Forest Ministers, Ottawa, Ontario, 172 p. Retrieved June 2020, from http://www.ccmf.org/english/coreproducts-cc.asp
  67. EPCOR (2017). Source Water Protection Plan, Edmonton’s Drinking Water System. 138 p. Retrieved June 2020, from https://www.epcor.com/products-services/water/Documents/source-water-protection-plan.pdf
  68. FireSmart Canada (2020) Retrieved June 2020, from https://firesmartcanada.ca/
  69. Fisher, R., Wellicome, T., Bayne, E., Poulin, R., and Todd, L. (2015). Extreme precipitation reduces reproductive output of an endangered raptor. Journal of Applied Ecology 52, 1500‒1508. Retrieved June 2020, from https://doi.org/10.1111/1365-2664.12510
  70. Fisher, R.F. and Bayne, E. (2014). Burrowing Owl Climate Change Adaptation Plan for Alberta. Alberta Biodiversity Monitoring Institute, Edmonton, Alberta. 63 p. Retrieved June 2020, from http://biodiversityandclimate.abmi.ca/wp-content/uploads/2015/01/FisherandBayne_2014_BurrowingOwlAdaptationPlan.pdf
  71. Flannigan, M.D., Krawchuk, M.A., de Groot, J., Wotton, B.M., and Gowman, L.M. (2009). Implications of changing climate for global wildland fire. International Journal of Wildland Fire 18, 483‒507. Retrieved June 2020, from https://doi.org/10.1071/WF08187
  72. Flannigan, M.D., Wotton, B.M., Marshall, G.A., de Groot, W.J., Johnston, J., Jurko, N., and A. S. Cantin (2016). Fuel moisture sensitivity to temperature and precipitation: climate change implications. Climatic Change 134, 59‒71. Retrieved June 2020, from https://doi.org/10.1007/s10584-015-1521-0
  73. Fletcher, A.J. (2017). “Maybe tomorrow will be better”: Gender and farm work in a changing climate. Chapter 12 in Climate Change and Gender in Rich Countries: Work, public policy and action, (Ed.) M. G. Cohen Routledge, Abingdon, Oxon, New York, New York, 185‒198 Retrieved June 2020, from https://doi.org/10.4324/9781315407906-12
  74. Fletcher, A.J. and Knuttila, E. (2016). Gendering change: Canadian farm women respond to drought. Chapter 7 in Vulnerability and adaptation to drought: The Canadian prairies and South America, (Eds.) H. Diaz, M. Hurlbert, and J. Warren. University of Calgary Press, Calgary, Alberta, 159‒177. Retrieved June 2020, from https://prism.ucalgary.ca/bitstream/handle/1880/51490/Vulnerability_and_adaptation_to_drought_2016_part%203.pdf?sequence=5&isAllowed=ywww.jstor.org/stable/j.ctv6gqwv1
  75. Ford, J.D. (2012). Indigenous Health and Climate Change. American Journal of Public Health, 102(7), 1260‒1266. Retrieved June 2020, from https://doi.org/10.2105/AJPH.2012.300752
  76. Ford, J.D., Berrang-Ford, L., King, M., and Furgal, C. (2010). Vulnerability of Aboriginal health systems in Canada to climate change. Global Environmental Change, 20(4), 668‒680. Retrieved June 2020, from https://doi.org/10.1016/j.gloenvcha.2010.05.003
  77. Gallagher, R., Makinson, R., Hogbin, P., and Hancock, N., (2015). Assisted colonization as a climate change adaptation tool. Austral Ecology 40, 12‒20. Retrieved June 2020, from https://doi.org/10.1111/aec.12163
  78. Garschagen, M. (2013). Resilience and organisational institutionalism from a cross-cultural perspective: an exploration based on urban climate change adaptation in Vietnam. Natural Hazards 67(1), 25‒46. Retrieved June 2020, from https://doi.org/10.1007/s11069-011-9753-4
  79. Gauthier, S., Bernier, P., Burton, P.J., Edwards, J., Isaac, K., Isabel, N., Jayen, K., Le Goff, H., and Nelson, E.A. (2014). Climate change vulnerability and adaptation in the managed Canadian boreal forest. Environmental Reviews 22, 256‒285. Retrieved June 2020, from https://doi.org/10.1139/er-2013-0064
  80. Gillett, N.P., Weaver, A.J., Zwiers, F.W., and Flannigan, M.D. (2004). Detecting the effect of climate change on Canadian forest fires. Geophysical Research Letters 31(18) L18211, Retrieved June 2020, from https://doi.org/10.1029/2004GL020876
  81. Gizaw, M. S. and Gan, T. Y. (2015). Possible impact of climate change on future extreme precipitation of the Oldman, Bow and Red Deer River Basins of Alberta. International Journal of Climatology 36(1), 208‒224. Retrieved June 2020, from https://doi.org/10.1002/joc.4338
  82. Gorman-Murray, A., Morris, S., Keppel, J., McKinnon, S., and Dominey-Howes, D. (2017). Problems and possibilities on the margins: LGBT experiences in the 2011 Queensland floods. Gender, Place & Culture, 24(1), 37‒51. https://doi.org/10.1080/0966369X.2015.1136806
  83. Government of Alberta (2006). Approved Water Management Plan for the South Saskatchewan River Basin, 52 p. Retrieved June 2020, from https://open.alberta.ca/publications/0778546209
  84. Government of Alberta (2015) Alberta moves to protect Calgary, neighbouring communities from severe flooding. Retrieved June 2020, from https://www.alberta.ca/release.cfm?xID=3873971607DE6-AA9E-CE00-9521CF82FC5D4567
  85. Government of Alberta (2018). 2017 Alberta Labour Force Profiles. Immigrants in the Labour Force.. 15 p. Retrieved June 2020, from https://open.alberta.ca/dataset/cab80384-59c6-42a1-9d7c-4b1f8b676ad8/resource/8914b60c-0962-42ea-9480-54f1b29b0186/download/labour-profile-immigrants.pdf
  86. Government of Manitoba (2018). Manitoba Drought Management Strategy, 50 p. Retrieved June 2020, from https://www.gov.mb.ca/sd/pubs/research_data_maps/drought_management_strategy.pdf
  87. Government of Manitoba (2020) Manitoba’s Watershed Districts, 50 p. Retrieved June 2020 from https://www.gov.mb.ca/sd/water/watershed/cd/
  88. Government of Saskatchewan (2017). Prairie Resilience: A Made-in-Saskatchewan Climate Change Strategy. Government of Saskatchewan, Saskatchewan, 13 p. Retrieved December 2020, from https://pubsaskdev.blob.core.windows.net/pubsask-prod/104890/104890-2017_Climate_Change_Strategy.pdf
  89. Government of Saskatchewan (2018) Climate Resilience Measurement Framework, Government of Saskatchewan, Saskatchewan, 8 p. Retrieved December 2020, from https://pubsaskdev.blob.core.windows.net/pubsask-prod/109479/109479-Climate_Change_Resilience_Measurement_Framework.pdf
  90. Gray, L. and Hamann, A. (2013). Tracking suitable habitat for tree populations under climate change in western North America. Climatic Change 117, 289‒303. Retrieved June 2020, from https://doi.org/10.1007/s10584-012-0548-8
  91. Gronlund, C. J. (2014). Racial and Socioeconomic Disparities in Heat-Related Health Effects and Their Mechanisms: a Review. Current Epidemiology Reports, 1(3), 165‒173. Retrieved June 2020, from https://doi.org/10.1007/s40471-014-0014-4
  92. Guyadeen, D., Thistlethwaite, J., and Henstra, D. (2018). Evaluating the Quality of Municipal Climate Change Plans in Canada. Climatic Change, 152, 121‒143. Retrieved June 2020, from https://doi.org/10.1007/s10584-018-2312-1
  93. Hadarits, M., Pittman, J., Corkal, D., Hill, H., Bruce, K., and Howard, A. (2017). The interplay between incremental, transitional, and transformational adaptation: a case study of Canadian agriculture. Regional Environmental Change 17(5), 1515‒1525. Retrieved June 2020, from https://doi.org/10.1007/s10113-017-1111-y
  94. M. Hanesiak, R. E. Stewart, B. R. Bonsal, P. Harder, R. Lawford, R. Aider, B. D. Amiro, E. Atallah, A. G. Barr, T. A. Black, P. Bullock, J. C. Brimelow, R. Brown, H. Carmichael, C. Derksen, L. B. Flanagan, P. Gachon, H. Greene, J. Gyakum, W. Henson, E. H. Hogg, B. Kochtubajda, H. Leighton, C. Lin, Y. Luo, J. H. McCaughey, A. Meinert, A. Shabbar, K. Snelgrove, K. Szeto, A. Trishchenko, G. van der Kamp, S. Wang, L. Wen, E. Wheaton, C. Wielki, Y. Yang, S. Yirdaw and T. Zha(2011) Characterization and Summary of the 1999‒2005 Canadian Prairie Drought, Atmosphere-Ocean, 49(4), 421‒452. Retrieved June 2020, from https://doi.org/10.1080/07055900.2011.626757
  95. Hanna, E. G., Kjellstrom, T., and Bennett, C. (2011). Climate Change and Rising Heat: Population Health Implications for Working People in Australia. Asia-Pacific Journal of Public Health. Supplement to 23(2), 14S‒26S. Retrieved June 2020, from https://doi.org/:10.1177/1010539510391457
  96. Haque, H., Choudhury, M., and Sikder, S. (2018). “Events and failures are our only means for making policy changes”: learning in disaster and emergency management policies in Manitoba, Canada, Natural Hazards, 98, 137‒162. Retrieved June 2020, from https://doi.org/10.1007/s11069-018-3485-7
  97. Hargreaves, A., Samis, K., and Eckert, C. (2014). Are species’ range limits simply niche limits writ large? A review of transplant experiments beyond the range. The American Naturalist 183(2), 157‒173. Retrieved June 2020, from https://doi.org/10.1086/674525
  98. He, W., Yang, J., Qian, B., Drury, C., Hoogenboom, G., He, P., Lapen, D., and Zhou, W. (2018). Climatic change impacts on crop yield, soil water balance and nitrate leaching in the semiarid and humid regions of Canada. PLOS ONE 13(11), e0207370. Retrieved June 2020, from https://doi.org/10.1371/journal.pone.0207370
  99. Heal, G. and Millner, A. (2014). Reflections: Uncertainty and decision making in climate change economics. Review of Environmental Economics and Policy. 8(1), 120‒137. Retrieved June 2020, from https://doi.org/10.1093/reep/ret023
  100. Heinmiller, B.T. (2018). Canadian federalism and the governance of water scarcity in the South Saskatchewan River Basin. Regional Environmental Change 18, 1667‒1677. Retrieved June 2020, from https://doi.org/10.1007/s10113-018-1314-x
  101. Heller, N. and Zavaleta, E. (2009). Biodiversity management in the face of climate change: a review of 22 years of recommendations. Biological Conservation 142(1) 14‒32. Retrieved June 2020, from https://doi.org/10.1016/j.biocon.2008.10.006
  102. Henderson, N., Hogg, E., Barrow, E., and Dolter, B. (2002). Climate change impacts on the island forests of the Great Plains and the implications for nature conservation policy. Prairie Adaptation Research Collaborative, Regina, Saskatchewan. Retrieved June 2020, from https://www.parc.ca/project/climate-change-impacts-on-the-island-forests-of-the-great-plains-and-the-implications-for-nature-conservation-policy-the-outlook-for-sweet-grass-hills-montana-cypress-hills-alberta-saskatchewan/
  103. Hester, S. (2018). Air Transportation + Fuel Supply. City of Edmonton, Edmonton, Alberta. Retrieved June 2020, from https://www.edmonton.ca/city_government/documents/Images/AirFuelsmall.jpg
  104. HilleRisLambers, J., Harsch, M., Ettinger, A., Ford, K., and Theobald, E. (2013). How will biotic interactions influence climate change-induced range shifts? Annals of the New York Academy of Sciences 1297, 112‒125. Retrieved June 2020, from https://doi.org/10.1111/nyas.12182
  105. Hof, C., Levinsky, I., Araujo, M., and Rahbek, C. (2011). Rethinking species’ ability to cope with rapid climate change. Global Change Biology 17, 2987‒2990. Retrieved June 2020, from https://doi.org/10.1111/j.1365-2486.2011.02418.x
  106. Hogg, E. (1994). Climate and the southern limit of the western Canadian boreal forest. Canadian Journal of Forest Research 24(9), 1835‒1845. Retrieved June 2020, from https://doi.org/10.1139/x94-237
  107. Hogg, E. and Bernier, P. (2005). Climate change impacts on drought-prone forests in western Canada. The Forestry Chronicle, 81(5), 675‒682. Retrieved June 2020, from https://doi.org/10.5558/tfc81675-5
  108. Hogg, E. and Hurdle, P. (1995). The aspen parkland in western Canada: a dry-climate analogue for the future boreal forest? Water, Air, Soil Pollution, 82, 391‒400. Retrieved June 2020, from https://doi.org/10.1007/BF01182849
  109. Hogg, E., Brandt, J., and Michaelian, M. (2008). Impacts of a regional drought on the productivity, dieback, and biomass of western Canadian aspen forests. Canadian Journal of Forest Research 38, 1373‒1384. Retrieved June 2020, from https://doi.org/10.1139/X08-001
  110. Holling, C.S. (1978). Adaptive Environmental Assessment and Management. John Wiley and Sons. Chichester, United Kingdom, 402 p.
  111. Hunter, F.G., Donald, D.B., Johnson, B.N., Hyde, W.H., Hopkinson, R.F., Hanesiak, J.M., Markus O.B. Kellerhals, M.O.B., and Oegema, B.W. (2002) The Vanguard Torrential Storm (Meteorology and Hydrology), Canadian Water Resources Journal / Revue canadienne des ressources hydriques,27(2), 213‒227. Retrieved June 2020, from https://doi.org/10.4296/cwrj2702213
  112. Hunter, G. and Sanchez, M. (2017). Child and Family Poverty in Saskatchewan: November 2017. Social Policy Research Centre, University of Regina, Regina, Saskatchewan. Retrieved June 2020, from https://campaign2000.ca/wp-content/uploads/2017/11/2017_Sask_ChildPovertyReport_Nov21.pdf
  113. Hunter, G. (2011). Poverty in Canada and Saskatchewan in 2011: No Closer to the Truth (Poverty Papers No. 4). Social Research Unit, University of Regina, Regina, Saskatchewan, 26 p.
  114. Hurlbert, M. (2018). Adaptive governance of disaster: Drought and flood in rural areas. Cham, Springer International Publishing. 247 p.
  115. Hurlbert, M. and Gupta, J. (2017). The adaptive capacity of institutions in Canada, Argentina, and Chile to droughts and floods. Regional Environmental Change, 17(3), 865‒877. Retrieved June 2020, from https://doi.org/10.1007/s10113-016-1078-0
  116. Hurlbert, M., Diaz, H., Corkal, D.R., and Warren, J. (2009). Climate change and water governance in Saskatchewan, Canada. International Journal of Climate Change Strategies and Management, 1(2), 118‒132. Retrieved June 2020, from https://doi.org/10.1108/17568690910955595
  117. Ignatowski, J.A., and Rosales, J. (2013). Identifying the exposure of two subsistence villages in Alaska to climate change using traditional ecological knowledge. Climatic Change, 121(2), 285‒299. Retrieved June 2020, from https://doi.org/10.1007/s10584-013-0883-4
  118. International Institute for Sustainable Development (2019). Local Climate Change Adaptation Planning in Manitoba, International Institute for Sustainable Development, Winnipeg, Manitoba, 60 p. Retrieved June 2020, https://www.google.com/url?client=internal-element-cse&cx=013574609802403716772:n5ygqmw9zvs&q=https://www.iisd.org/sites/default/files/publications/climate-change-adaptation-planning-manitoba.pdf&sa=U&ved=2ahUKEwi3_Pz714bqAhUgTTABHTSuC44QFjAAegQIARAB&usg=AOvVaw3EsVMB6zMOeoC_VPC5I8GJ
  119. Ingty, T. (2017). High mountain communities and climate change: adaptation, traditional ecological knowledge, and institutions. Climatic Change, 145(1-2), 41‒55. Retrieved June 2020, from https://doi.org/10.1007/s10584-017-2080-3
  120. Iniesta-Arandia, I., Ravera, F., Buechler, S., Díaz-Reviriego, I., Fernández-Giménez, M.E., Reed, M. G.,Thompson-Hall, M., Wilmer, H., Aregu, L., Cohen, P., Djoudi, H., Lawless, S., Martín-Lopez, B., Smucker, T., Villamor, G.B., and Wangui, E.E. (2016). A synthesis of convergent reflections, tensions and silences in linking gender and global environmental change research. Ambio, 45(S3), 383‒393. Retrieved June 2020, from https://doi.org/10.1007/s13280-016-0843-0
  121. Insurance Bureau of Canada (2019). Facts of the Property and Casualty Insurance Industry in Canada, 41st edition. Retrieved June 2020, from http://assets.ibc.ca/Documents/Facts%20Book/Facts_Book/2019/IBC-2019-Facts.pdf
  122. IPCC [Intergovernmental Panel on Climate Change] (2014). Climate Change 2014: Synthesis Report. Contribution of Working Groups I, II and III to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change (Eds.) R.K. Pachauri and L.A. Meyer and the Core Writing Team, IPCC, Geneva, Switzerland, 151 p. Retrieved June 2020, from https://www.ipcc.ch/site/assets/uploads/2018/05/SYR_AR5_FINAL_full_wcover.pdf
  123. Ireson, A., Barr, A., Johnstone, J., Mamet, S., Van der Kamp, G., Whitfield, C.J., Michel, N.L., North, R.L., Westbrook, C.J., DeBeer, C.M., Chun, K.P., Nazemi, A., and Sagin, J. (2015). The changing water cycle: the Boreal Plains ecozone of Western Canada. Wiley Interdisciplinary Reviews: Water 2, 505‒521. Retrieved June 2020, from https://doi.org/10.1002/wat2.1098
  124. Jencso, K., B. Parker, M. Downey, T. Hadwen, A. Howell, J. Rattling Leaf, L. Edwards, and A. Akyuz, D. Kluck, D. Peck, M. Rath, M. Syner, N. Umphlett, H. Wilmer, V. Barnes, D. Clabo, B. Fuchs, M. He, S. Johnson, J. Kimball, D. Longknife, D. Martin, N. Nickerson, J. Sage and T. Fransen. (2019). Flash Drought: Lessons Learned from the 2017 Drought Across the U.S. Northern Plains and Canadian Prairies. NOAA National Integrated Drought Information System, 76 p. Retrieved June 2020, from https://www.drought.gov/drought/documents/flash-drought-lessons-learned-2017-drought-across-us-northern-plains-and-canadian-0
  125. Jerneck, A. (2018). What about Gender in Climate Change? Twelve Feminist Lessons from Development. Sustainability, 10(3), 627. Retrieved June 2020, from https://doi.org/10.3390/su10030627
  126. Jia, G., Epstein, H., and Walker, D. (2009). Vegetation greening in the Canadian Arctic related to decadal warming. Journal of Environmental Monitoring 11, 2231‒2238. Retrieved June 2020, from https://doi.org/10.1657/AAAR0016-075
  127. Jing, Q., Bélanger, G., Qian, B., and Baron, V. (2013). Timothy Yield and Nutritive Value under Climate Change in Canada. Agronomy Journal, 105(6). Retrieved June 2020, from https://doi.org/10.2134/agronj2013.0195
  128. Jing, Q., Huffman, T., Shang, J., Liu, J., Pattey, E., Morrison, M., Jego, G., and Qian, B. (2017). Modelling soybean yield responses to seeding date under projected climate change scenarios. Canadian Journal of Plant Science 97, 1152‒1164. Retrieved June 2020, from https://doi.org/10.1139/cjps-2017-0065
  129. Johnson, W., Werner, B., Guntenspergen, G., Voldseth, R., Millett, B., Naugle, D.E., Tulbere, M.,Carroll, R.W.H., Tracy, J., and Olawsky, C. (2010). Prairie wetland complexes as landscape functional units in a changing climate. BioScience 60,128‒140. Retrieved June 2020, from https://doi.org/10.1525/bio.2010.60.2.7
  130. Joyce, L., Briske, D., Brown, J., Polley, H., McCarl, B., and Bailey, D. (2013). Climate Change and North American Rangelands: Assessment of Mitigation and Adaptation Strategies. Rangeland Ecology & Management, 66(5), 512‒528. Retrieved June 2020, from https://doi.org/10.2111/REM-D-12-00142.1
  131. Kaijser, A. and Kronsell, A. (2014). Climate change through the lens of intersectionality. Environmental Politics, 23(3), 417‒433. Retrieved June 2020, from https://doi.org/10.1080/09644016.2013.835203
  132. Kelly, A. and Goulden, M. (2008). Rapid shifts in plant distribution with recent climate change. Proceedings of the National Academy of Sciences 105, 11823‒11826. Retrieved June 2020, from https://doi.org/10.1073/pnas.0802891105
  133. Kettridge, N. and Waddington, J. (2014). Towards quantifying the negative feedback regulation of peatland evaporation to drought. Hydrological Processes 28, 3728‒3740. Retrieved June 2020, from https://doi.org/10.1002/hyp.9898
  134. Kirchmeier-Young, M.C., Zwiers, F.W., Gillett, N.P., and Cannon, A.J. (2017). Attributing extreme fire risk in Western Canada to human emissions. Climatic Change 144, 365‒379. Retrieved June 2020, from https://doi.org/10.1007/s10584-017-2030-0
  135. Kissling, W., Field, R., Korntheuer, H., Heyder, U., and Bohning-Gaese, K. (2010). Woody plants and the prediction of climate-change impacts on bird diversity. Philosophical Transactions of the Royal Society of London B: Biological Sciences 365, 2035‒2045. Retrieved June 2020, from https://doi.org/10.1098/rstb.2010.0008
  136. Klenk, N.L., Reed, M.G., Lidestav, G., and Carlsson, J. (2013). Models of representation and participation in Model Forests: Dilemmas and implications for networked forms of environmental governance involving Indigenous people. Environmental Policy and Governance, 23(3), 161‒176. Retrieved June 2020, from https://doi.org/10.1002/eet.1611
  137. Kochtubajda, B., Brimelow, J., Flannigan, M., Morrow, B., and Greenhough, M.D. (2017). The Extreme 2016 Wildfire in Fort McMurray, Alberta, Canada. Sidebar 7.1 in State of the Climate in 2016 Special Supplement to the Bulletin of the American Meteorological Society,98(8),176‒177. Retrieved June 2020, from https://doi.org/10.1175/2017BAMSStateoftheClimate.1
  138. Kulshreshtha, S., Wheaton, E. (2013). Climate change and agriculture: some knowledge gaps. International Journal of Climate Change: Impacts and Responses 4(2), 127‒148. Retrieved June 2020, from https://doi.org/10.18848/1835-7156/CGP/v04i02/37165
  139. Kulshreshtha, S., Wheaton, E., and Wittrock, V. (2011). Natural Hazards and First Nations Community Setting: Challenges for Adaptation, in Section 5: Socio-economic issues in Management of Natural Resources, Sustainable Development and Ecological Hazards, (Eds.). C. A. Brebbia, and S.S. Zubir WIT Press, Ashhurst, Southampton, United Kingdom, 277‒288. Retrieved June 2020, from https://doi.org/10.2495/RAV110261
  140. Lal, P., Alavalapati, J.R.R., and Mercer, E.D. (2011). Socio-economic impacts of climate change on rural United States. Mitigation and Adaptation Strategies for Global Change, 16(7), 819‒844. Retrieved June 2020, from https://doi.org/10.1007/s11027-011-9295-9
  141. Landhäusser, S., Deshaies, D., and Lieffers, V. (2010). Disturbance facilitates rapid range expansion of aspen into higher elevations of the Rocky Mountains under a warming climate. Journal of Biogeography 37, 68‒76. Retrieved June 2020, from https://doi.org/10.1111/j.1365-2699.2009.02182.x
  142. Larson, D. (1995). Effects of climate on numbers of northern prairie wetlands. Climate Change 30, 169‒180. Retrieved June 2020, from https://doi.org/10.1007/BF01091840
  143. Leonard, S., Parsons, M., Olawsky, K., and Kofod, F. (2013). The role of culture and traditional knowledge in climate change adaptation: Insights from East Kimberley, Australia. Global Environmental Change, 23(3), 623‒632.Retrieved June 2020, from https://doi.org/10.1016/j.gloenvcha.2013.02.012
  144. Lilliston, B and, Athanasiou, L. (2018). From the ground up: The state of the States on Climate Adaptation for Agriculture. Institute for Agriculture and Trade Policy, Minneapolis, Minnesota, 43 p. Retrieved June 2020, from https://www.cakex.org/documents/ground-state-states-climate-adaptation-agriculture
  145. Liu J., Stewart R.E., and Szeto K.K. (2004). Moisture transport and other hydrometeorological features associated with the severe 2000/01 drought over the western and central Canadian Prairies. Journal of Climate, 17, 305‒319. Retrieved December 2020, from https://www.researchgate.net/publication/249611550_Moisture_Transport_and_Other_Hydrometeorological_Features_Associated_with_the_Severe_200001_Drought_over_the_Western_and_Central_Canadian_Prairies
  146. Lura Consulting (2018). City of Saskatoon Climate Change Mitigation Business Plan Executive Summary of Feedback from Engagement Activities. Report Prepared for the City of Saskatoon. Retrieved June 2020, from https://www.saskatoon.ca/sites/default/files/documents/corporate-performance/environmental-corporate-initiatives/climate-change/executive_summary_engagement_-_climate_change.pdf
  147. Lynes, L. and Boyd, R. (2018). Adaptation Planning and Local Early Action Plan: A Guide for Indigenous Communities, The Rockies Institute and All One Sky Foundation, Alberta, 40 p. Retrieved June 2020, from https://www.prairiesrac.com/wp-content/uploads/2019/01/Guide_facilitating_co-created_adaptation_planning_Indigenous_communities_2018.pdf
  148. MacGregor, S. (2010). A stranger silence still: The need for feminist social research on climate change. The Sociological Review, 57, 124‒140. Retrieved June 2020, from https://doi.org/10.1111/j.1467-954X.2010.01889.x
  149. Magzul, L. (2009). The Blood Tribe: Adapting to Climate Change, in Part III: Case Studies of Vulnerability, in A Dry Oasis. Regina, (Ed.). G. P. Marchildon. Canadian Plains Research Center, University of Regina, Regina, Saskatchewan, 289‒309.
  150. Manitoba Hydro (2014). Climate Change Report, 48 p. Retrieved June 2020, from https://www.hydro.mb.ca/environment/pdf/climate_change_report_2014_15.pdf
  151. Manitoba’s Auditor General (2017) Managing Climate Change, 37 p. Retrieved June 2020, from https://digitalcollection.gov.mb.ca/awweb/pdfopener?smd=1&did=25775&md=1
  152. Manitoba Sustainable Development (2017). A Made-in-Manitoba Climate and Green Plan, 64 p. Retrieved June 2020, from https://www.gov.mb.ca/asset_library/en/climatechange/climategreenplandiscussionpaper.pdf
  153. Marchildon, G., Wheaton, D., Fletcher, A., and Vanstone, J. (2016). Extreme drought and excessive moisture conditions in two Canadian watersheds: comparing the perception of farmers and ranchers with the scientific record. Natural Hazards 82, 245‒266 Retrieved June 2020, from https://doi.org/10.1007/s11069-016-2190-7
  154. Marchildon, G.P. (2009). The Prairie Farm Rehabilitation Administration: Climate crisis and federal–provincial relations during the Great Depression. Canadian Historical Review, 90(2), 275‒301. Retrieved June 2020, from https://doi.org/10.3138/chr.90.2.275
  155. Martens, T. (2016). Land and the Food That Grows on It. Briarpatch Magazine, 45(5). Retrieved June 2020, from https://briarpatchmagazine.com/articles/view/land-and-the-food-that-grows-on-it
  156. Martin, D.E., Thompson, S., Ballard, M., and Linton, J. (2017). Two-Eyed Seeing in Research and its Absence in Policy: Little Saskatchewan First Nation Elders’ Experiences of the 2011 Flood and Forced Displacement. International Indigenous Policy Journal, 8(4), 1‒25. Retrieved June 2020, from https://doi.org/10.18584/iipj.2017.8.4.6
  157. Martinez-Meyer, E., Townsend P., and Hargrove, W. (2004). Ecological niches as stable distributional constraints on mammal species, with implications for Pleistocene extinctions and climate change projections for biodiversity. Global Ecology and Biogeography 13, 305‒314. Retrieved June 2020, from https://doi.org/10.1111/j.1466-822X.2004.00107.x
  158. McLeman, R. (2010). Impacts of population change on vulnerability and the capacity to adapt to climate change and variability: a typology based on lessons from “a hard country”. Population and Environment, 31(5), 286‒316. Retrieved June 2020, from https://doi.org/10.1007/s11111-009-0087-z
  159. McLeman, R.A., Dupre, J., Berrang-Ford, L., Ford, J., Gajewski, K., and Marchildon, G. (2014). What we learned from the Dust Bowl: lessons in science, policy, and adaptation. Population and Environment, 35(4), 417‒440. Retrieved June 2020, from https://doi.org/10.1007/s11111-013-0190-z
  160. McMartin, D.W. and Hernani Merino, B.H. (2014). Analysing the links between agriculture and climate change: Can ‘best management practices’ be responsive to climate extremes? International Journal of Agricultural Resources, Governance and Ecology, 10(1): 50‒62. Retrieved June 2020, from https://doi.org/10.1504/IJARGE.2014.061042
  161. McNeeley, S.M., Dewes, C.F., Stiles, C.J., Beeton, T.A., Rangwala, I., Hobbins, M.T., and Knutson, C. L. (2018). Anatomy of an interrupted irrigation season: Micro-drought at the Wind River Indian Reservation. Climate Risk Management, 19, 61‒82. Retrieved June 2020, from https://doi.org/10.1016/j.crm.2017.09.004
  162. Melles, S., Fortin, M., Lindsay, and Badzinski, D. (2011). Expanding northward: influence of climate change, forest connectivity, and population processes on a threatened species’ range shift. Global Change Biology 17, 17‒31. Retrieved June 2020, from https://doi.org/10.1111/j.1365-2486.2010.02214.x
  163. Meng, T., Carew, R., Florkowski, W, and Klepacka, A. (2017). Analyzing temperature and precipitation influences on yield distributions of canola and spring wheat in Saskatchewan. Journal of Applied Meteorology and Climatology 56, 897‒913. Retrieved June 2020, from https://doi.org/10.1175/JAMC-D-16-0258.1
  164. Moosa, C.S. and Tuana, N. (2014). Mapping a Research Agenda Concerning Gender and Climate Change: A Review of the Literature. Hypatia, 29(3), 677‒694. Retrieved June 2020, from https://doi.org/10.1111/hypa.12085
  165. Mottershead, K.D. (2017). The 2012 wildfire evacuation experiences of Dene Tha’ First Nation. University of Alberta, Edmonton, Alberta. Retrieved from https://era.library.ualberta.ca/items/ed07c2b5-c18b-4674-b953-7eb10796d6fd/view/cfe9fcd0-b91e-4446-8aeb-eb4427ad9a83/Mottershead_Kyla_D_201704_MA.pdf
  166. Moyser, M. and Burlock, A. (2018). Time use: Total work burden, unpaid work, and leisure. Catalogue No. 89-503-X. Statistics Canada, Ottawa, Ontario, 22 p. Retrieved June 2020, from https://www150.statcan.gc.ca/n1/pub/89-503-x/2015001/article/54931-eng.pdf
  167. Müller, B., Johnson, L., and Kreuer, D. (2017). Maladaptive Outcomes of Climate Insurance in Agriculture. Global Environmental Change 46, 23‒33. Retrieved June 2020, from https://doi.org/10.1016/j.gloenvcha.2017.06.010
  168. Myers, S.S., Smith, M.R., Guth, S., Golden, C.D., Vaitla, B., Mueller, N.D., Dangour, A.D., and Huybers, P. (2017). Climate change and global food systems: Potential impacts on food security and undernutrition. Annual Review of Public Health, 38, 259‒277. Retrieved June 2020, from https://doi.org/10.1146/annurev-publhealth-031816-044356
  169. Nantel, P., Pellatt, M.G., Keenleyside, K., and Gray, P.A. (2014): Biodiversity and protected areas; Chapter 6 in Canada in a Changing Climate: Sector Perspectives on Impacts and Adaptation, (Eds.) F.J. Warren and D.S. Lemmen. Government of Canada, Ottawa, Ontario159‒190. Retrieved June 2020, from https://changingclimate.ca/CCCR2019/chapter/6-0/
  170. Natcher, D.C., Shirley, S., Rodon, T., and Southcott, C. (2016). Constraints to wildlife harvesting among Aboriginal communities in Alaska and northern Canada. Food Security, 8(6), 1153‒1167. Retrieved June 2020, from https://doi.org/10.1007/s12571-016-0619-1
  171. Nixon, A., Fisher, R.J., Stralberg, D., Bayne, E., and Farr, D. (2016). Projected responses of North American grassland songbirds to climate change and habitat availability at their northern range limits in Alberta, Canada. Avian Conservation and Ecology 11(2). Retrieved June 2020, from https://doi.org/10.5751/ACE-00866-110202.
  172. Nunez, T., Lawler, J., McRae, B., Pierce, and Krosby, M. (2013). Connectivity planning to address climate change. Conservation Biology 27,407‒416. Retrieved June 2020, from https://doi.org/10.1111/cobi.12014
  173. O’Brien, K.L. and Leichenko, R.M. (2000). Double exposure: assessing the impacts of climate change within the context of economic globalization. Global Environmental Change, 10(3), 221‒232. Retrieved June 2020, from https://doi.org/10.1016/S0959-3780(00)00021-2
  174. Olszynski, M. (2017). Failed experiments: an empirical assessment of adaptive management in Alberta’s energy resources sector. UBC Law Review (Forthcoming). Retrieved June 2020, from https://papers.ssrn.com/sol3/papers.cfm?abstract_id=2909040
  175. O’Shaughnessy, S. and Krogman, N.T. (2011). Gender as contradiction: From dichotomies to diversity in natural resource extraction. Journal of Rural Studies, 27(2), 134‒143. Retrieved June 2020, from https://doi.org/10.1016/j.jrurstud.2011.01.001
  176. Ogden, A.E. and Innes, J. (2007). Incorporating climate change adaptation considerations into forest management planning in the boreal forest. International Forestry Review 9, 713‒733. Retrieved June 2020, from https://doi.org/10.1505/ifor.9.3.713
  177. Ogden, A.E. and Innes, J. (2009). Application of structured decision making to an assessment of climate change vulnerabilities and adaptation options for sustainable forest management. Ecology and Society 14, 11. Retrieved June 2020, from https://www.ecologyandsociety.org/vol14/iss1/art11/
  178. Okorosobo, T. (2018). Anthropogenic Climate Change: A Slow Moving Emergency. PRAC Regional Workshop. Edmonton, Alberta: Prairies Regional Adaptation Collaborative. Retrieved from https://www.prairiesrac.com/wp-content/uploads/2018/10/Tosan-Okorosobo-Interlake-Reserve-Tribal-Council-2018.pdf
  179. Oliver, T., Brereton, T., and Roy, D. (2013). Population resilience to an extreme drought is influenced by habitat area and fragmentation in the local landscape. Ecography 36, 579‒586. Retrieved June 2020, from https://doi.org/10.1111/j.1600-0587.2012.07665.x
  180. Oxman-Martinez, J., Rummens, A.J., Moreau, J., Choi, Y.R., Beiser, M., Ogilvie, L., and Armstrong, R. (2012). Perceived Ethnic Discrimination and Social Exclusion: Newcomer Immigrant Children in Canada. American Journal of Orthopsychiatry, 82(3), 376‒388. Retrieved June 2020, from https://doi.org/10.1111/j.1939-0025.2012.01161.x
  181. Park, D., Sullivan, M., Bayne, E., and Scrimgeour, G. (2008). Landscape-level stream fragmentation caused by hanging culverts along roads in Alberta’s boreal forest. Canadian Journal of Forest Research 38, 566‒575. Retrieved June 2020, from https://doi.org/10.1139/X07-179
  182. Parlee, B. and Furgal, C. (2012). Well-being and environmental change in the arctic: a synthesis of selected research from Canada’s International Polar Year program. Climatic Change, 115(1), 13‒34. Retrieved June 2020, from https://doi.org/10.1007/s10584-012-0588-0
  183. Patiño, L. and Gauthier, D.A. (2009). Integrating local perspectives into climate change decision making in rural areas of the Canadian prairies. International Journal of Climate Change Strategies and Management, 1(2), 179‒196. Retrieved June 2020, from https://doi.org/10.1108/17568690910955630
  184. Patrick, R. (2018a). Social and cultural impacts of the 2013 Bow River flood at Siksika Nation, Alberta, Canada. Indigenous Policy Journal, 28(3). Retrieved June 2020, from http://www.indigenouspolicy.org/index.php/ipj/article/view/521
  185. Patrick, R. J. (2018b). Adapting to Climate Change Through Source Water Protection: Case Studies from Alberta and Saskatchewan, Canada. The International Indigenous Policy Journal, 9(3). Retrieved June 2020, from https://doi.org/10.18584/iipj.2018.9.3.1
  186. Pearse, R. (2017). Gender and climate change. Wiley Interdisciplinary Reviews: Climate Change, 8(2), e451. Retrieved June 2020, from https://doi.org/10.1002/wcc.451
  187. Pearson, R., Stanton, J., Shoemaker, K., Aiello-Lammens, M., and Ersts, P. (2014). Life history and spatial traits predict extinction risk due to climate change. Nature Climate Change 4, 217‒221. Retrieved June 2020, from https://doi.org/10.1038/nclimate2113
  188. Pennesi, K., Arokium, J., and McBean, G. (2012). Integrating local and scientific weather knowledge as a strategy for adaptation to climate change in the Arctic. Mitigation and Adaptation Strategies for Global Change, 17(8), 897‒922. Retrieved June 2020, from https://doi.org/10.1007/s11027-011-9351-5
  189. Perkins, P.E. (2017). Canadian Indigenous female leadership and political agency on climate change. Chapter 18 in Climate Change and Gender in Rich Countries: Work, Public Policy and Action, (Ed.) M. G. Cohen, 282-296. Routledge, New York, New York
  190. Pittman, J., Wittrock, V., Kulshreshtha, S., and Wheaton, E. (2011). Vulnerability to climate change in rural Saskatchewan: Case study of the Rural Municipality of Rudy No. 284. Journal of Rural Studies, 27(1), 83‒94. https://doi.org/10.1016/j.jrurstud.2010.07.004
  191. Pittman, J., Corkal, D.R., Hadarits, M., Harrison, T., Hurlbert, M., and Unvoas, A. (2016). Bridging knowledge systems for drought preparedness: A case study of the Swift Current Creek watershed. Chapter 12 in .Vulnerability and Adaptation to Drought: The Canadian Prairies and South America.(Eds.) H. P. Diaz, M. Hurlbert, and J. Warren, 279‒299,University of Calgary Press, Calgary, Alberta. Retrieved June 2020, from https://doi.org/10.2307/j.ctv6gqwv1.15
  192. Poudel, S., Kulshreshtha, S., Wheaton, E. (2017). The economic impacts of climate change and climatic extremes on the mixed farms of the Canadian Prairie. International Journal of Climate Change: Impacts and Responses 9(4), 35‒52. Retrieved June 2020, from https://doi.org/10.18848/1835-7156/CGP/v09i04/35-52
  193. Poudel, S. and Kulshreshtha, S. (2016). Choice of Beef Herd Adaptation Strategy on Canadian Prairie Mixed Farms under Extreme Climate Events. Sociological Study 6(3), 147‒163. Retrieved June 2020, from https://doi.org/10.17265/2159-5526/2016.03.001
  194. Prairie Province Water Board (2014). Annual Report 2014‒2015. Regina, Saskatchewan. Retrieved June 2020, from https://www.ppwb.ca/uploads/media/5c8175a94bf18/ppwb-annual-report-final-resizeden2014.pdf?v1
  195. Prairie Provinces Water Board (2015). The 1969 Master Agreement on Apportionment. Prairie Provinces Water Board, Regina, Saskatchewan, 110 p. Retrieved June 2020, from https://www.ppwb.ca/uploads/media/5cad077eeae53/master-agreement.pdf?v1
  196. Pomeroy, J., Stewart, R., and Whitfield, P. (2015). The 2013 flood event in the South Saskatchewan and Elk River basins: Causes, assessment and damages, Canadian Water Resources Journal / Revue canadienne des ressources hydriques, 41(1-2), 105‒117, Retrieved June 2020, from http://dx.doi.org/10.1080/07011784.2015.1089190
  197. Public Safety Canada (2019). Canadian Disaster Database. Government of Canada, Ottawa, Ontario Retrieved June 2020, from https://www.publicsafety.gc.ca/cnt/rsrcs/cndn-dsstr-dtbs/index-en.aspx
  198. Qian, B., Jing, Q., Belanger, G., Shang, J., Huffman, T., Liu, J. and Hoogenboom, G. (2018). Simulated canola yield responses to climate change and adaptation in Canada. Agronomy Journal 2018, 110 (1), 133‒146. Retrieved June 2020, from https://doi.org/10.2134/agronj2017.02.0076
  199. Qian, B. (2018) Personal communication with Budong Qian, November 2018. Agroclimatologist at Agriculture and Agri-Food Canada, Ottawa, Ontario.
  200. Qian, B., De Jong, R., Huffman, T., Wang, H., and Yang, J. (2015). Projecting yield changes of spring wheat under future climate scenarios on the Canadian Prairies. Theoretical and Applied Climatology 123, 651‒669. Retrieved June 2020, from https://doi.org/10.1007/s00704-015-1378-1
  201. Qian B., De Jong R., Gameda S. (2009) Multivariate analysis of water-related agroclimatic factors limiting spring wheat yields on the Canadian prairies. European Journal of Agronomy 30, 140‒150. Retrieved June 2020, from https://doi.org/10.1016/j.eja.2008.09.003
  202.  QUEST [Quality Urban Energy Systems of Tomorrow] (2015). Resilient Pipes and Wires: Assessing policies as driver and barriers to integration of adaptation in the planning and operation of the energy distribution sub-sector, Report to Natural Resources Canada through the Adaptation Platform, 52 p.
  203. Rannie, W.F. (2006). A comparison of 1858-59 and 2000-2001 drought patterns on the Canadian Prairies. Canadian Water Resources Journal / Revue canadienne des ressources hydriques, 31(4), 263‒274. Retrieved June 2020, from https://doi.org/10.4296/cwrj3104263
  204. Rapaport, E., Manuel, P., Krawchenko, T., and Keefe, J. (2015). How can aging communities adapt to coastal climate change? Planning for both social and place vulnerability. Canadian Public Policy / Analyse de politiques, 41(2), 166‒177. Retrieved June 2020, from https://doi.org/10.3138/cpp.2014-055
  205. Ready, E. (2018). Sharing-based social capital associated with harvest production and wealth in the Canadian Arctic. PLOS ONE, 13(3), e0193759.Retrieved June 2020, from https://doi.org/10.1371/journal.pone.0193759
  206. Reed, M. G. and Davidson, D. (2011). Terms of engagement: The intersections among gender, class and race in Canadian sustainable forest management. Chapter 11 in Reshaping gender and class in rural spaces, (Eds.) B. Pini & B. Leach 199‒220. Ashgate Publishing, Aldershot.
  207. Reed, M., Scott, A., Natcher, D., and Johnston, M. (2014). Linking gender, climate change, adaptive capacity and forest-based communities in Canada. Canadian Journal of Forest Research, 44(9): 995‒1004.Retrieved June 2020, from https://doi.org/10.1139/cjfr-2014-0174
  208. Reid, M.G., Hamilton, C., Reid, S.K., Trousdale, W., Hill, C., Turner, N., Picard, C.R., Lamontangue, C., and Matthews, H.D. (2014). Indigenous Climate Change Adaptation Planning Using a Values-Focused Approach: A Case Study with the Gitga’at Nation. Journal of Ethnobiology, 34(3), 401‒424. Retrieved June 2020, from https://doi.org/10.2993/0278-0771-34.3.401
  209. Rempel, J. C., Kulshreshtha, S. N., Amichev B. Y., and Van Rees, K. C.J. (2017) Costs and benefits of shelterbelts: A review of producers’ perceptions and mind map analyses for Saskatchewan, Canada Canadian Journal of Soil Science 97(3), 341‒352. Retrieved June 2020, from https://doi.org/10.1139/cjss-2016-0100
  210. Rickards, L. & Howden, S. M. 2012. Transformational adaptation: Agriculture and climate change. Crop and Pasture Science 63(3) 240‒250. Retrieved June 2020, from https://doi.org/10.1071/CP11172
  211. Romps, D.M., Seeley, J.T., Vollaro, D., and Molinari, J. (2014). Projected increase in lightning strikes in the United States due to global warming. Science 346, 851‒854. Retrieved June 2020, from https://doi.org/10.1126/science.1259100
  212. Rosales, J. and Chapman, J. (2015). Perceptions of Obvious and Disruptive Climate Change: Community-Based Risk Assessment for Two Native Villages in Alaska. Climate, 3(4), 812‒832. Retrieved June 2020, from https://doi.org/10.3390/cli3040812
  213. City of Saskatoon (2018). Engage. Retrieved June 2020, from https://www.saskatoon.ca/engage/climate-change
  214. Sauchyn, D. and Kulshreshtha, S. (2008). Prairies, in From impacts to adaptation: Canada in a changing climate 2007, (Eds.) D.S. Lemmen, F.J. Warren, J. Lacroix and E. Bush. Government of Canada, Ottawa, Ontario, 276‒328. Retrieved June 2020, from https://www.nrcan.gc.ca/impacts-adaptation-canada-changing-climate/10253https://www.nrcan.gc.ca/environment/impacts-adaptation/assessments/10031
  215. Sauchyn, D., Bonsal, B., Kienzle, S., St. Jacques, J-M, Vanstone, J., and Wheaton, E. (2014). Adaptation according to mode of climate variability: A case study from Canada’s western interior. 1-24 in Handbook of Climate Change Adaptation, (Ed.) W. Leal Filho, Springer, Berlin Heidelberg, Germany. https://doi.org/10.1007/978-3-642-40455-9_93-1
  216. Sauchyn, D., Vanstone, J., St.-Jacques, J., and Sauchyn, R. (2015). Dendrohydrology in Canada’s western interior and applications to water resource management. Journal of Hydrology, 529, 548‒558. Retrieved June 2020, from https://doi.org/10.1016/j.jhydrol.2014.11.049
  217. Sauchyn, D., St-Jacques, J., Barrow, E., Nemeth, M., MacDonald, R., Sheer, M., and Sheer, D. (2016). Adaptive Water Resource Planning in the South Saskatchewan River Basin: Use of Scenarios of Hydroclimatic Variability and Extremes. Journal of the American Water Resources Association, 52(1), 222‒240. Retrieved June 2020, from https://doi.org/10.1111/1752-1688.12378
  218. Savage, J. and Vellend, M. (2015). Elevational shifts, biotic homogenization and time lags in vegetation change during 40 years of climate warming. Ecography 38, 546‒555. Retrieved June 2020, from https://doi.org/10.1111/ecog.01131
  219. Schauberger, B., Archontoulis, S., Arneth, A., Balkovic, J., Ciais, P., Deryng, D., Elliot, J.,  Folberth, C., Khabarov, N., Muller, C., Pugh, T., Rolinski, S., Schaphoff, S., Schmid, E.,Wang, X., Shlenker, W., and Frieler, K. (2017). Consistent negative response of US crops to high temperatures in observations and crop models. Nature Communications 8, 13931. Retrieved June 2020, from https://doi.org/10.1038/ncomms13931
  220. Schneider, R. (2013). Alberta’s natural subregions under a changing climate: past, present, and future. Alberta Biodiversity Monitoring Institute, Edmonton, Alberta. Retrieved June 2020, from https://doi.org/10.7939/R3WS8HM1N
  221. Schneider, R., Hamann, A., Farr, D., Wang, X., and Boutin, S. (2009). Potential effects of climate change on ecosystem distribution in Alberta. Canadian Journal of Forest Research 39, 1001‒1010. Retrieved June 2020, from https://doi.org/10.1139/X09-033
  222. Schneider, R., Devito, K., Kettridge, N., and Bayne, E. (2015). Moving beyond bioclimatic envelope models: integrating upland forest and peatland processes to predict ecosystem transitions under climate change in the western Canadian boreal plain. Ecohydrology 9, 899-908. Retrieved June 2020, from https://doi.org/10.1002/eco.1707
  223. Schneider, R and Bayne, E.M. (2015). Reserve Design under Climate Change: From Land Facets Back to Ecosystem Representation. PLoS ONE 10(5). Retrieved June 2020, from https://doi.org/10.1371/journal.pone.0126918
  224. Schneider, R.R. (2014). Conserving Alberta’s Biodiversity Under a Changing Climate: A Review and Analysis of Adaptation Measures. Alberta Biodiversity Monitoring Institute, Edmonton, Alberta. Retrieved June 2020, from https://era.library.ualberta.ca/items/fdb2f52f-89ff-4341-8c1a-42996364c4d1/view/4acadc1f-7809-49d0-b627-2f2dcd2138e4/Schneider-202014-20–20Adapting-20to-20climate-20change.pdf .
  225. SeaFirst Insurance Brokers (2018). The Top 5 Most Expensive Natural Disasters in Canada. Retrieved June 2020, from https://www.seafirstinsurance.com/top-5-most-expensive-natural-disasters-canada
  226. Seager, J. (2014). Disasters are gendered: What’s new? in Reducing disaster: Early warning systems For climate change, (Eds.) A. Singh and Z. Zommers, 265‒281. Springer, Dordrecht, Germany Retrieved June 2020, from https://doi.org/10.1007/978-94-017-8598-3_14
  227. Shuba, C., Ozog, C., Diaz, H.P., Hurlbert, M., and Fletcher, A. J. (2016). Community and governance vulnerability: The Canada case study (Vulnerability and Adaptation to Climate Extremes in the Americas (VACEA)). University of Regina, Regina, Saskatchewan.
  228. Smit, B. and M. Skinner. 2002. Adaptation options in agriculture to climate change: a typology. Mitigation and Adaptation Strategies for Global Change, Vol 7(1), 85‒114. Retrieved June 2020, from https://doi.org/10.1023/A:1015862228270
  229. Smith, W.N., Grant, B.B., Desjardins, R.L., Kroebel, R., Li, C., Qian, B., Worth, D.E., McConkey, B.G., and Drury, C.F. (2013). Assessing the effects of climate change on crop production and GHG emissions in Canada. Agriculture, Ecosystems & Environment, 179, 139‒150. Retrieved June 2020, from https://doi.org/10.1016/j.agee.2013.08.015
  230. Statistics Canada (2007). A statistical portrait of agriculture, Canada and provinces: Census years 1921 to 2006 (No. 95-632- XWE). Statistics Canada, Ottawa, Ontario. Retrieved June 2020, from https://www150.statcan.gc.ca/n1/pub/95-632-x/2007000/t/4185570-eng.htm
  231. Statistics Canada. (2011a). 2011 Census of Agriculture. Statistics Canada, Ottawa, Ontario. Retrieved June 2020, from http://www.statcan.gc.ca/daily-quotidien/120510/dq120510a-eng.htm
  232. Statistics Canada. (2011b). Canada’s rural population since 1851. Statistics Canada, Ottawa, Ontario: retrieved June 2020, from https://www12.statcan.gc.ca/census-recensement/2011/as-sa/98-310-x/98-310-x2011003_2-eng.pdf
  233. Statistics Canada (2015). Lone-parent families: The new face of an old phenomenon. Ottawa, ON: Government of Canada. Retrieved June 2020, from https://www150.statcan.gc.ca/n1/pub/11-630-x/11-630-x2015002-eng.htm
  234. Statistics Canada (2016) After-tax low income status of tax filers and dependants based on Census Family Low Income Measure (CFLIM-AT), by family type and family type composition. Table: 11-10-0018-01 (formerly CANSIM111-0046). Statistics Canada, Ottawa, Ontario. Retrieved June 2020, from https://www150.statcan.gc.ca/t1/tbl1/en/tv.action?pid=1110001801
  235. Statistics Canada (2017a). The Daily — 2016 Census of Agriculture. Statistics Canada, Ottawa, Ontario Retrieved June 2020, from https://www150.statcan.gc.ca/n1/daily-quotidien/170510/dq170510a-eng.htm
  236. Statistics Canada (2017b). Farm Debt Outstanding, classified by lender (x 1,000) (Table 32-10-0051-01). Statistics Canada, Ottawa, Ontario. Retrieved June 2020, from https://www150.statcan.gc.ca/t1/tbl1/en/tv.action?pid=3210005101
  237. Statistics Canada (2018a) The Canadian Immigrant Labour Market: Recent Trends from 2006 to 2017, Retrieved June 2020, from https://www150.statcan.gc.ca/n1/pub/71-606-x/71-606-x2018001-eng.htm
  238. Statistics Canada (2018b). Women in Canada: A gender – based statistical report, 7th edition (No. 89-503- X). Statistics Canada, Ottawa, Ontario Retrieved June 2020, from https://www150.statcan.gc.ca/n1/en/catalogue/89-503-X
  239. Statistics Canada (2019a). Aboriginal Peoples Highlight Tables, 2016 Census. Statistics Canada, Ottawa, Ontario. Retrieved June 2020, from https://www12.statcan.gc.ca/census-recensement/2016/dp-pd/hlt-fst/abo-aut/Table.cfm?Lang=Eng&T=101&S=99&O=A
  240. Statistics Canada (2019b). Aboriginal Peoples Highlight Tables, 2016 Census. Statistics Canada, Ottawa, Ontario. Retrieved June 2020, from https://www12.statcan.gc.ca/census-recensement/2016/dp-pd/hlt-fst/abo-aut/Table.cfm?Lang=Eng&T=102&D1=1&D2=1&D3=1&RPP=25&PR=0&SR=1&S=54&O=A
  241. Ste-Marie, C., Nelson, E.A., Dabros, A., and Bonneau, M.E. (2011). Assisted migration: introduction to a multifaceted concept. Forestry Chronicle 87(6), 724‒730. Retrieved June 2020, from https://doi.org/10.5558/tfc2011-089
  242. Stralberg, D., Wang, X., Parisien, M., Robinne, F., and Solymos, P. (2018). Wildfire-mediated vegetation change in boreal forests of Alberta, Canada. Ecosphere 9, e02156. Retrieved June 2020, from https://doi.org/10.1002/ecs2.2156
  243. Sudmeyer, R A, Edward, A, Fazakerley, V, Simpkin, L, and Foster, I. (2016), Climate change: impacts and adaptation for agriculture in Western Australia. Bulletin 4870. Department of Agriculture and Food, Perth, Western Australia, Retrieved June 2020, from https://researchlibrary.agric.wa.gov.au/cgi/viewcontent.cgi?article=1043&context=bulletins
  244. Suncor Energy Inc. (2018). 2018 Climate Risk and Resilience Report. Calgary, Alberta. 28 p. Retrieved June 20202, from https://sustainability.suncor.com/en/downloads
  245. Suttle, K., Thomsen, M., and Power, M. (2007). Species interactions reverse grassland responses to changing climate. Science 315, 640‒642. Retrieved June 2020, from http://angelo.berkeley.edu/wp-content/uploads/Suttle_2007_Science.pdf
  246. Szeto, K. et al. (2016).The 2015 Extreme drought in Western Canada. Chapter 9 in Explaining Extreme Events of 2015 from a Climate Perspective. Special Supplement to the Bulletin of the American Meteorological Society, 97(12). Retrieved June 2020, from https://journals.ametsoc.org/doi/pdf/10.1175/BAMS-D-16-0147.1
  247. Szeto, K., Henson, W., Stewart, R., and Gascon, G. (2011). The catastrophic June 2002 prairie rainstorm. Atmosphere-Ocean 49, 380‒395. Retrieved June 2020, from https://doi.org/10.1080/07055900.2011.623079
  248. Szeto, K., Gysbers, P., Brimelow, J., and Stewart, R. (2014). The 2014 Extreme Flood on the Southeastern Canadian Prairies in Explaining Extreme Events of 2014 from a Climate Perspective. Special Supplement to the Bulletin of the American Meteorological Society 96(12), S20-4. Retrieved June 2020, from https://doi.org/10.1175/BAMS-D-15-00110.1
  249. Tam, B.Y., Gough, W.A., Edwards, V., and Tsuji, L.J.S. (2013). The impact of climate change on the well-being and lifestyle of a First Nation community in the western James Bay region: Impacts of climate change on a First Nation community. The Canadian Geographer / Le Géographe canadien, 57(4), 441‒456.Retrieved June 2020, from https://doi.org/10.1111/j.1541-0064.2013.12033.x
  250. Tan, X., Chen, S., Gan, T.Y., Liu, B., and Chen, X. (2019). Dynamic and thermodynamic changes conducive to the increased occurrence of extreme fire weather over western Canada under possible anthropogenic climate change. Agricultural And Forest Meteorology 265, 269‒279 Retrieved June 2020, from https://doi.org/10.1016/j.agrformet.2018.11.026
  251. Tang, E. (2003).Agriculture: The Relationship between Aboriginal Farmers and Non-Aboriginal Farmers. Saskatchewan Indian Cultural Centre. 22 p.
  252. Taylor, S. and Parry, J.-E. (2014). Enhancing the resilience of Manitoba’s winter roads system. International Institute for Sustainable Development, Winnipeg, Manitoba. Retrieved June 2020, from https://www.iisd.org/sites/default/files/publications/winter_roads.pdf
  253. Teriman, S. and Yigitcanlar, T. (2011). Social infrastructure planning and sustainable communities: Example from South East Queensland, Australia. World Journal of Social Sciences, 1(4), 23‒32. Retrieved June 2020, from https://eprints.qut.edu.au/40205/
  254. Teufel, B., Diro, G.T., Whan, K., Milrad, S.M., Jeong,D.I., Ganji, A., Huziy, O., Winger,K., Gyakum,J.R., de Elia,R., Zwiers, F.W., and Sushama, L. (2017). Investigation of the 2013 Alberta flood from weather and climate Perspectives, Climate Dynamics 48, 2881‒2899 https://doi.org/10.1007/s00382-016-3239-8
  255. The Women’s Centre of Calgary (2017). A Gender Analysis for Poverty Reduction in Alberta: Recommendations. Calgary, Alberta. 15 p. Retrieved June 2020, from https://www.womenscentrecalgary.org/wp-content/uploads/2011/07/A-Gendered-Analysis-for-Alberta-2015.pdf
  256. Thompson, S. (2015). Flooding of First Nations and Environmental Justice in Manitoba: Case Studies of the Impacts of the 2011 Flood and Hydro Development in Manitoba. Manitoba Law Journal, 38(2), 220. Retrieved June 2020, from http://ecohealthcircle.com/wp-content/uploads/2017/02/Flooding-of-First-Nations-and-Environmental-Justice-in-Manitoba.pdf
  257. Thorpe, J. (2011). Vulnerability of Prairie Grassland to Climate Change. Saskatchewan Research Council Saskatoon, Saskatchewan. Report prepared for the Prairie Adaptation Research Collaborative. Retrieved June 2020, from https://www.parc.ca/rac/fileManagement/upload/12855-2E11%20Vulnerability%20of%20Grasslands%20to%20climate%20change.pdf
  258. TransAlta Corporation (2018). Management’s Discussion and Analysis. 2017 Annual Integrated Report. Calgary, Alberta. 98 p. Retrieved June 2020, from https://www.transalta.com/wp-content/uploads/2018/03/TAC2017_MDA.pdf
  259. Trans PULSE. (2011). We’ve got work to do: Workplace discrimination and employment challenges for trans people in Ontario. Trans PULSE E-Bulletin, 2(1), 1‒3. Retrieved June 2020, from https://transpulseproject.ca/wp-content/uploads/2011/05/E3English.pdf
  260. Urban, M., Tewksbury, J., and Sheldon, K. (2012). On a collision course: competition and dispersal differences create no-analogue communities and cause extinctions during climate change. Proceedings of the Royal Society of London B: Biological Sciences 279, 2072‒2080. Retrieved June 2020, from https://doi.org/10.1098/rspb.2011.2367
  261. Vasseur, L., Thornbush, M., and Plante, S. (2015). Gender-based experiences and perceptions after the 2010 winter storms in Atlantic Canada. International Journal of Environmental Research and Public Health, 12(10), 12518‒12529. Retrieved June 2020, from https://doi.org/10.3390/ijerph121012518
  262. Veitch, A. (2001). An unusual record of a White-tailed Deer, Odocoileus virginianus, in the Northwest Territories. Canadian Field Naturalist 115, 172‒175. Retrieved June 2020, from https://www.researchgate.net/publication/285013752_An_unusual_record_of_a_White-tailed_Deer_Odocoileus_virginianus_in_the_Northwest_Territories
  263. Veland, S., Howitt, R., Dominey-Howes, D., Thomalla, F., and Houston, D. (2013). Procedural vulnerability: Understanding environmental change in a remote indigenous community. Global Environmental Change, 23(1), 314‒326. Retrieved June 2020, from https://doi.org/10.1016/j.gloenvcha.2012.10.009
  264. Venema, H. D., Oborne, B., & Neudoerffer, C. (2010). The Manitoba challenge: linking water and land management for climate adaptation. International Institute for Sustainable Development, Winnipeg, Manitoba.79 p. Retrieved December 2020, from https://www.iisd.org/publications/manitoba-challenge-linking-water-and-land-management-climate-adaptation#:~:text=The%20Manitoba%20Challenge%3A%20Linking%20Water%20and%20Land%20Management,also%20help%20improve%20the%20state%20of%20Lake%20Winnipeg.
  265. Venema, H., Parry, J., McCullough, S., Temmer, J., Terton, A., and Smith, R. (2017) Building a Climate-Resilient City: Nine Reports on Climate Change Adaptation in Edmonton and Calgary, The Prairie Climate Centre. Retrieved June 2020, from http://prairieclimatecentre.ca/publications/
  266. VandenBygaart, A.J. (2016). The myth that no-till can mitigate global climate change. Agriculture, Ecosystems & Environment, 216, 98‒99.  Retrieved June 2020, from https://doi.org/10.1016/j.agee.2015.09.013
  267. Vincent, C. (2013). Why do women earn less than men?: A synthesis of findings from Canadian microdata (CRDCN Synthesis Series) p. 24. Canadian Research Data Centre Network. Retrieved June 2020, from https://crdcn.org/sites/default/files/carole_vincent_synthesis_final_2.pdf
  268. Volney, W.J.A. and Hirsch, K.G. (2005). Disturbing forest disturbances. The Forestry Chronicle 81, 662‒668. Retrieved June 2020, from http://pubs.cif-ifc.org/doi/pdf/10.5558/tfc81662-5
  269. Walther, G., Roques, A., Hulme, P., Sykes, M., and Pyvsek, P. (2009). Alien species in a warmer world: risks and opportunities. Trends in Ecology & Evolution 24, 686‒693. Retrieved June 2020, from https://doi.org/10.1016/j.tree.2009.06.008
  270. Warren, F.J. and Lemmen, D.S. (Eds.) (2014). Canada in a Changing Climate: Sector Perspectives on Impacts and Adaptation; Government of Canada, Ottawa, Ontario, 286 p. Retrieved June 2020, from https://www.nrcan.gc.ca/climate-change/impacts-adaptations/what-adaptation/canada-changing-climate-sector-perspectives-impacts-and-adaptation/16309
  271. Wang, H., He, Y., Qian, B., McConkey, B., Cutforth, H., McCaig, T., McLeod, G., Zentner, R., DePauw, R.,Lemke, R., Brandt, K., Liu, T., Xiaobo Qin, White, J., Hunt, T.and Hoogenboom, G. (2012). Short Communication: Climate change and biofuel wheat: A case study of southern Saskatchewan. Canadian Journal of Plant Science, 92(3), 421-425. Retrieved June 2020, from https://doi.org/10.4141/cjps2011-192
  272. Warren, J.W. (2016a). The “min till” revolution and the culture of innovation. Chapter 5 in Vulnerability and adaptation to drought: The Canadian prairies and South America, (Eds.) H. P. Diaz, M. Hurlbert, & J. W. Warren. University of Calgary Press, Calgary, Alberta, 107‒132. Retrieved June 2020 from https://prism.ucalgary.ca/bitstream/1880/51490/5/Vulnerability_and_adaptation_to_drought_2016_part%203.pdf
  273. Warren, J.W. (2016b). The troubled state of irrigation in southwestern Saskatchewan: the effects of climate variability and government offloading on a vulnerable community. Chapter 6 in (Eds.) H. P. Diaz, M. Hurlbert, and  J. W. Warren ,Vulnerability and adaptation to drought: The Canadian prairies and South America 133‒157. University of Calgary Press, Calgary, Alberta. Retrieved June 2020, from http://hdl.handle.net/1880/51490
  274. Water Security Agency of Saskatchewan (2012) 25 Year Saskatchewan Water Security Plan, 53 p.
  275. Water Security Agency (2016) Quill Lakes Flood Mitigation Study, Prepared for the Water Security Agency by KGS Group Consulting Engineers, Winnipeg, Manitoba. Retrieved June 2020, from https://www.wsask.ca/Global/About%20WSA/Quill%20Lakes/Intro%20-%20Pages%20i%20to%20ix.pdf
  276. WaterSMART Solutions Ltd. (2018). A Roadmap for Sustainable Water Management in the Athabasca River Basin. Produced by WaterSMART Solutions Ltd. for Alberta Innovates, Calgary, Alberta, Canada. 247 p. Retrieved June 2020, from https://watersmartsolutions.ca/wp-content/uploads/2018/08/ARB-Initiative-final_report_Roadmap_for-sustainable_water_management_in_the_ARB_Sept-2018.pdf
  277. Western Economic Diversification Canada (2018). Economic Overview. Retrieved June 2020, from: https://www.wd-deo.gc.ca/eng/243.asp
  278. Wheaton, E. and Kulshreshtha, S. (2017). Environmental Sustainability of Agriculture Stressed by Changing Extremes of Drought and Excess Moisture: A Conceptual Review. Sustainability 9(6)970. Retrieved June 2020, from https://doi.org/10.3390/su9060970
  279. Wheaton, E., Kulshreshtha, S., Wittrock, V., and Koshida, G. (2008). Dry times: hard lessons from the Canadian drought of 2001 and 2002. The Canadian Geographer 52(2), 242‒262. Retrieved June 2020, from https://doi.org/10.1111/j.1541-0064.2008.00211.x
  280. Whyte, K.P. (2014). Indigenous women, climate change impacts, and collective action. Hypatia, 29(3), 599‒616. Retrieved June 2020, from https://doi.org/10.1111/hypa.12089
  281. Wiens, J., Ackerly, D., Allen, A. Anacker, B., and Buckley, L. (2010). Niche conservatism as an emerging principle in ecology and conservation biology. Ecology Letters 13, 1310‒1324. Retrieved June 2020, from https://doi.org/10.1111/j.1461-0248.2010.01515.x
  282. Wiensczyk, A.S. (2014). Climate Change Impacts to the Oil and Gas Sector in Western Canada – How are we preparing? Report submitted to Climate Change Impacts and Adaptation, Natural Resources Canada. Trout Creek Collaborative Solutions. Retrieved June 2020, from https://www.prairiesrac.com/wp-content/uploads/2018/06/Oil-and-Gas-Industry-Climate-Change-Impact-A-Wiensczyk.pdf
  283. Williams, L. (2018). Climate change, colonialism, and women’s well-being in Canada: what is to be done? Canadian Journal of Public Health, 109(2), 268‒271. Retrieved June 2020, from https://doi.org/10.17269/s41997-018-0031-z
  284. Willig, M., Kaufman, D., and Stevens, R. (2003). Latitudinal gradients of biodiversity: pattern, process, scale, and synthesis. Annual Review of Ecology, Evolution, and Systematics 34, 273‒309. Retrieved June 2020, from https://doi.org/10.1146/annurev.ecolsys.34.012103.144032
  285. Wittrock, V., Halliday, R., Corkal, D., Johnston, M., Wheaton, E., Lettvenuk, J., Stewart, I., Bonsal, B., and Geremia, M. (2018). Saskatchewan Flood and Natural Hazard Risk Assessment. Prepared for the Saskatchewan Ministry of Government Relations, Saskatchewan Research Council, Saskatoon, Saskatchewan. SRC Publication No. 14113-2E18, 256 p. Retrieved June 2020, from https://www.saskatchewan.ca/-/media/news-release-backgrounders/2018/dec/saskatchewanfloodandnaturalhazardriskassessment-2.pdf
  286. Wittrock, V., Wheaton, E., Bonsal, B., and Vanstone, J. (2014). Connecting Climate and Crop Yields: Case Studies of the Swift Current Creek and Oldman River Watersheds. Prepared for the Vulnerability and Adaptation to Climate Extremes in the Americas Project of the Prairie Adaptation Research Collaborative Saskatchewan Research Council. Saskatoon, Saskatchewan, 41 p.
  287. Wittrock, V., E. Wheaton, E., and Siemens, E. (2010) March. More than a close call: a preliminary assessment of the characteristics, impacts of, and adaptations to the drought of 2008-2010 in the Canadian Prairies. Prepared for Environment Canada. Saskatchewan Research Council, Saskatoon, Saskatchewan, Publication 12803-1E10, 157 p.
  288. Wittrock, V., Kulshreshtha S., and Wheaton, E. (2012) Bio-Physical and Socio-Economic Vulnerabilities of Selected Prairie Communities in South Saskatchewan River Basin Facing Droughts. Chapter in Droughts: New Research. (Eds.) D. F. Neves and J. D. Sanz. Nova Science Publishers, Inc., New York, New York, USA. 267‒288.
  289. Wittrock, V., Kulshreshtha, S. N., and Wheaton, E. (2011). Canadian prairie rural communities: their vulnerabilities and adaptive capacities to drought. Mitigation and Adaptation Strategies for Global Change, 16(3), 267‒290. Retrieved June 2020, from https://doi.org/10.1007/s11027-010-9262-x
  290. Wolf, J., Allice, I., and Bell, T. (2013). Values, climate change, and implications for adaptation: Evidence from two communities in Labrador, Canada. Global Environmental Change, 23(2), 548‒562. Retrieved June 2020, from https://doi.org/10.1016/j.gloenvcha.2012.11.007
  291. Wood, S., Karp, D., DeClerck, F., Kremen, C., Naeem, S., Palm, C. (2016). Functional traits in agriculture: agrobiodiversity and ecosystem services. Trends in Ecology and Evolution, 30(9), 531‒539. Retrieved June 2020, from https://doi.org/10.1016/j.tree.2015.06.013
  292. Wotton, B., Flannigan, M., and Marshall, G. (2017). Potential climate change impacts on fire intensity and key wildfire suppression thresholds in Canada. Environmental Research Letters 12(9). Retrieved June 2020, from https://doi.org/10.1088/1748-9326/aa7e6e
  293. Yusa, A., Berry, P., Cheng, J., Ogden, N., Bonsal, B., Stewart, R., and Waldick, R. (2015). Climate Change, Drought and Human Health in Canada. International Journal of Environmental Research and Public Health 12(7), 8359‒8412. Retrieved June 2020, from https://doi.org/10.3390/ijerph120708359
  294. Zeitoun, M., Lankford, B., Krueger, T., Forsyth, T., Carter, R., Hoekstra, A.Y.,Taylor, R., Varis, O., Cleaver, F., Boelens, R., Swatuk, L., Tickner, D., Scott, C.A., Miramachi, N., and Matthews, N. (2016). Reductionist and integrative research approaches to complex water security policy challenges. Global Environmental Change, 39, 143‒154. Retrieved June 2020, from https://doi.org/10.1016/j.gloenvcha.2016.04.010
  295. Zhang, X., Flato, G., Kirchmeier-Young, M., Vincent, L., Wan, H., Wang, X., Rong, R., Fyfe, J., Li, G., and Kharin, V.V. (2019). Changes in temperature and precipitation across Canada, Chapter 4 in Canada’s Changing Climate Report, (Eds.) E. Bush, and D.S. Lemmen.  Government of Canada, Ottawa, Ontario, 112‒193. Retrieved June 2020, from https://changingclimate.ca/CCCR2019/chapter/4-0/
  296. Zizzo, L.A. (2014). Understanding Canadian Electricity Generation and Transmission Sectors’ Actions and Awareness on Climate Change and the Need to Adapt. Zizzo Allan Professional Corporation, Toronto, Ontario, 30 p. Retrieved June 2020, from https://mantle314.com/canada-electricity-generation-and-transmission-sectors-action-and-awareness/
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