Figure ES8: Schematic diagram showing past and future projected changes in the seasonal distribution of streamflow in many snow-fed river basins across Canada. In association with warming temperatures, spring peak streamflow following snowmelt has, and will continue to, occur earlier with higher winter flows and reduced summer flows.
![](https://changingclimate.ca/site/assets/uploads/sites/2/2019/03/FigureNew-ES8-1024x800.png)