Water Resources Research Act Program

Details for Project ID 2008AK71B

Study of Streamflow Response to Seasonal Snowcover Change in the Yukon River

Institute: Alaska
Year Established: 2008 Start Date: 2008-03-01 End Date: 2010-02-28
Total Federal Funds: $49,428 Total Non-Federal Funds: $16,210

Principal Investigators: Daqing Yang

Abstract: The Yukon River is one of the largest rivers in the northern regions. It contributes 203 km3/year freshwater to the Bering Sea. Hydrologic conditions and its changes in the Yukon river significantly affect regional biologic and ecologic systems. Snowcover is one of the critical land memory processes that significantly impact atmosphere, hydrology and ecosystems in the high latitude regions. Snowcover melt and associated floods are the most important hydrologic event of the year in the northern river basins. Our current understanding of Yukon River hydrology and climate changes, particularly large-scale snowmelt processes and their interaction with climatic change and variation, is incomplete. This limits our capability of documenting past change and predict future change over this largest watershed in Alaska. This research will apply remote sensing and in-situ snowcover data and products for snowcover and snowmelt runoff analyses over the Yukon watershed. The focus is to examine the streamflow response to snowcover change during the spring melt season, and to determine the potential of using remotely sensed snowcover information to improve our capability of snowmelt runoff modeling and forecasting over large northern regions.