C51D:
Snowmelt Driven Hydrological Processes Posters
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C51D:
Snowmelt Driven Hydrological Processes Posters
Snowmelt Driven Hydrological Processes Posters
You can still search the program to see your colleague�s abstract submissions as well as the sessions submitted for the 2016 Fall Meeting. The final program will be released in early October.
Session ID#: 13233
Session Description:
Snow is an important water resource around the world and is vital to a number of communities and ecosystems for survival. For these reasons the spring snowmelt season is important to water managers, ecosystems, and climate science. The hydrological response to snowmelt will certainly alter in a changing climate and gaining a stronger understating of the physical hydrological processes will better allow scientists and society to adapt to and mitigate negative consequences of the future. This session will focus on thes physical hydrological processes that occur during snowmelt and the connections between disciplines including streamflow connectivity, flooding, groundwater or soil moisture storage recharge, evapotranspiration, and land surface radiative feedback.
Primary Convener: Ryan Webb, University of Wyoming, Laramie, WY, United States
Convener: Steven R Fassnacht, Colorado State University, Watershed Science, Fort Collins, United States
Chairs: Ryan Webb, University of Wyoming, Laramie, WY, United States and Steven R Fassnacht, Colorado State University, Watershed Science, Fort Collins, United States
OSPA Liaison: Ryan Webb, University of Wyoming, Laramie, WY, United States
Cross-Listed:
- GC - Global Environmental Change
- H - Hydrology
- NH - Natural Hazards
- PA - Public Affairs
Index Terms:
0736 Snow [CRYOSPHERE]
0740 Snowmelt [CRYOSPHERE]
1836 Hydrological cycles and budgets [HYDROLOGY]
1863 Snow and ice [HYDROLOGY]
Abstracts Submitted to this Session:
An Integrated Canopy Gap Module with DHSVM for Improving Predictions of Canopy-Snow Dynamics (136573)
See more of: Cryosphere
