Understanding and Assessing Impacts
This plan presents historical and projected climate data. The Kaslo Adjusted and Homogenized Canadian Climate Data (AHCCD) record formed the basis of the data used in understanding historical climate; however, missing data has become more frequent and data acquisition at the station appears to have ended in September 2018. Missing temperature and precipitation data in the Kaslo record were estimated from the Duncan Lake Dam (ECCC) and Queens Bay (BCH) records using the ‘buddy system’ for temperature and the Normal Ratio Method for precipitation. The century-scale climate history for the Southeast Fire Centre region was reconstructed with data from eight Environment and Climate Change Canada (ECCC) AHCCD climate stations (Kaslo, Creston, Fauquier, Warfield, Grand Forks, Cranbrook, Golden and Revelstoke) and two standard ECCC stations with long and consistently recorded data (Fernie and Castlegar). The Kaslo AHCCD temperature and precipitation records were compared with the climate records in the Southeast Fire Centre region to ensure regional consistency. Consequently, the climate history for the immediate Kaslo area was based on the Kaslo AHCCD record. This plan compiles climate model projections for the Kaslo region that are associated with two RCPs: a ‘High Carbon’ pathway (RCP8.5) and a ‘Low Carbon’ pathway (RCP4.5). Climate model projections are based on output from an ensemble of 12 statistically downscaled Global Climate Model (GCM) projections from the Pacific Climate Institute Consortium. Trends in the regional records and the Kaslo temperature and precipitation time series were computed for the last ca. 100 years and for the last ca. 50 years. The significance of the trends was determined using the Mann-Kendall test. The magnitude of the trends was determined with the Theil-Sens approach. Climate impacts include increasing temperature, wetter, warmer winters, drier, warmer summers, more extreme precipitation events, and more extreme weather and lightning events. In addition to the direct human security risk associated with wildfire, wildfire also impacts soils, runoff, terrain stability, and water quality.