RATIONALE: THE ANTARCTIC ICE SHEET LOSES METEORIC ICE BY BASAL MELTING AND PRODUCTION OF LARGE TABULAR AND SMALLER SLIVER ICEBERGS FROM ITS ICE SHELVES. AVERAGED OVER SEVERAL DECADES THE CALVING FLUX IS ABOUT 50% OF TOTAL ICE SHEET LOSS BUT IS HIGH
$503,408FY2021National Aeronautics and Space AdministrationNASA
Earth And Space Research, Seattle WA