May Science Seminar: Rain-on-Snow Responses to Warming and Their Implications for Streamflow and Stream Temperature in the Great Lakes Basin

 

Snow processes play a key role in the hydrology and ecology of cold regions. Climate change is likely to change the magnitude, timing, and spatial patterns of snowpacks. This is especially true in the Great Lakes Basin, where decreases in snowpack, intensified snowmelt, and more frequent rain-on-snow events are causing changes in streamflow and stream temperature in ecologically important rivers.