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Yan, Fenglin

Snowmelt runoff in high latitudes has significant impacts on global climatic and hydrologic systems. Snowmelt timing and snow water equivalent (SWE) from the Advanced Microwave Scanning Radiometer for EOS (AMSR-E) are inputs to the new flux-based SWEHydro model to simulate the spring streamflow without meteorological data for high-latitude, snow-dominated drainages. The model was developed for the Ross River (7250 km2) and tested on the Pelly River (49,000 km2), nested tributaries to the Yukon River. The model uses four parameters: snowmelt rate during and after the melt transition (as defined by passive microwave observations), and flow timing during and after the melt transition. A normalized mismatch function...
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Snowmelt runoff in high latitudes has significant impacts on global climatic and hydrologic systems. Snowmelt timing and snow water equivalent (SWE) from the Advanced Microwave Scanning Radiometer for EOS (AMSR-E) are inputs to the new flux-based SWEHydro model to simulate the spring streamflow without meteorological data for high-latitude, snow-dominated drainages. The model was developed for the Ross River (7250 km2) and tested on the Pelly River (49,000 km2), nested tributaries to the Yukon River. The model uses four parameters: snowmelt rate during and after the melt transition (as defined by passive microwave observations), and flow timing during and after the melt transition. A normalized mismatch function...
Snowmelt runoff in high latitudes has significant impacts on global climatic and hydrologic systems. Snowmelt timing and snow water equivalent (SWE) from the Advanced Microwave Scanning Radiometer for EOS (AMSR-E) are inputs to the new flux-based SWEHydro model to simulate the spring streamflow without meteorological data for high-latitude, snow-dominated drainages. The model was developed for the Ross River (7250 km2) and tested on the Pelly River (49,000 km2), nested tributaries to the Yukon River. The model uses four parameters: snowmelt rate during and after the melt transition (as defined by passive microwave observations), and flow timing during and after the melt transition. A normalized mismatch function...
Snowmelt runoff in high latitudes has significant impacts on global climatic and hydrologic systems. Snowmelt timing and snow water equivalent (SWE) from the Advanced Microwave Scanning Radiometer for EOS (AMSR-E) are inputs to the new flux-based SWEHydro model to simulate the spring streamflow without meteorological data for high-latitude, snow-dominated drainages. The model was developed for the Ross River (7250 km2) and tested on the Pelly River (49,000 km2), nested tributaries to the Yukon River. The model uses four parameters: snowmelt rate during and after the melt transition (as defined by passive microwave observations), and flow timing during and after the melt transition. A normalized mismatch function...
Snowmelt runoff in high latitudes has significant impacts on global climatic and hydrologic systems. Snowmelt timing and snow water equivalent (SWE) from the Advanced Microwave Scanning Radiometer for EOS (AMSR-E) are inputs to the new flux-based SWEHydro model to simulate the spring streamflow without meteorological data for high-latitude, snow-dominated drainages. The model was developed for the Ross River (7250 km2) and tested on the Pelly River (49,000 km2), nested tributaries to the Yukon River. The model uses four parameters: snowmelt rate during and after the melt transition (as defined by passive microwave observations), and flow timing during and after the melt transition. A normalized mismatch function...
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