Division of Geodesy and Earth Observation, Department of Space Research and Space Technology (DTU Space), The Technical University of Denmark (DTU), Kgs. Lyngby, Denmark
Department of Civil and Environmental Engineering, Norwegian University of Science and Technology (NTNU), Trondheim, Norway
Department of Arctic Geophysics, The University Centre in Svalbard (UNIS), Longyearbyen, Norway
Henriette Skourup
Division of Geodesy and Earth Observation, Department of Space Research and Space Technology (DTU Space), The Technical University of Denmark (DTU), Kgs. Lyngby, Denmark
Eero Rinne
Department of Arctic Geophysics, The University Centre in Svalbard (UNIS), Longyearbyen, Norway
Division of Geodesy and Earth Observation, Department of Space Research and Space Technology (DTU Space), The Technical University of Denmark (DTU), Kgs. Lyngby, Denmark
Jeremy Wilkinson
British Antarctic Survey, Cambridge, Cambridgeshire, UK
Gaelle Veyssiere
British Antarctic Survey, Cambridge, Cambridgeshire, UK
Donghui Yi
GST Inc., Laboratory for Satellite Altimetry, Center for Satellite Applications and Research, NOAA, College Park, MD, USA
Division of Geodesy and Earth Observation, Department of Space Research and Space Technology (DTU Space), The Technical University of Denmark (DTU), Kgs. Lyngby, Denmark
Taniâ Gil Duarte Casal
ESA – ESTEC, European Space Agency, Noordwijk, the Netherlands
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An airborne campaign collected unprecedented coincident multi-frequency radar and lidar data over sea ice along a CryoSat-2 and ICESat-2 (CRYO2ICE) orbit in the Weddell Sea, useful for evaluating microwave snow penetration. Ka-band and Ku-band had limited penetration with significant contributions from the air–snow interface, contradicting traditional assumptions with discrepancies between commonly used C/S-band "snow-radar" methodologies, all challenging comparisons of airborne and spaceborne estimates.
An airborne campaign collected unprecedented coincident multi-frequency radar and lidar data...