Abstract
We have used Radar Altimeter 2 (RA‐2) onboard ESA’s EnviSAT and Geosciences Laser Altimeter System (GLAS) onboard NASA’s ICESat to map the elevation change of the Flade Isblink Ice Cap (FIIC) in northern Greenland. Based on RA‐2 data we show that the mean surface elevation change of the FIIC has
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