SMOS supports investigations of Antarctica’s ice-sheet internal temperature
Lack of in-situ measurements of ice temperature (boreholes) limit our capabilities to understand ice sheet dynamics. Researchers combined L-band (1.4 GHz) passive microwave observations from SMOS over Antarctica with glaciological and emission models to infer information on glaciological properties of the ice sheet at various depths, including temperature. Comparison with existing models showed that differences …