Microwave remote sensing of snow water equivalent and melt
Snow extent, depth, and melt status have implications for energy balance, hydrology, wildlife, hazards, and human systems. Passive microwave sensors have a long, multi-decadal record of global daily observations. These observations work in darkness and cloud cover so they have importance for high latitude and stormy regions. We are using Calibrated Enhanced-resolution brightness temperatures (CETB) from the suite of SSMI, SSMIS, and AMSR sensors to measure snow water equivalent for the entire period of record, and improving tools for measuring snow melt timing over that time period and in near real time.