Global Water Futures project mobilizes interdisciplinary teams to investigate winter soil processes
Warmer winters are leading to a greater frequency of freeze-thaw events and colder soils due to the loss of the insulating snowpack. These factors are subsequently changing the movement of water, carbon and nutrients in soils during the winter. Many assume that frozen soils are dormant. However, a new research project at the University of Waterloo is discovering that soils remain biogeochemically active during winter months, just differently from other seasons.