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Snow on sea ice is a sensitive indicator of climate change because it plays an important role regulating surface and near surface air temperatures. Given its high albedo and low thermal conductivity, snow cover is considered a key reason for amplified warming in polar regions. This study focuses on retrieving snow depth on sea ice from brightness temperatures recorded by the Microwave Radiation Imager...
Given the high albedo and low thermal conductivity, snow on sea ice is regarded as one of the key reasons for the amplification of the warming in polar regions. This study focused on the retrieval of snow depth on sea ice from brightness temperatures of the Microwave Radiation Imager (MWRI) on board the FengYun (FY)-3B satellite. After cross calibrated to the Advanced Microwave Scanning Radiometer-EOS...
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