The rapid and steady mass loss of the patagonian icefields throughout the GRACE Era: 2002-2017
We use the complete gravity recovery and climate experiment (GRACE) Level-2 monthly time series to derive the ice mass changes of the Patagonian Icefields (Southern Andes). The glacial isostatic adjustment is accounted for by a regional model that is constrained by global navigation satellite system...
Published in: | Remote Sensing |
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Main Authors: | , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
MDPI
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Subjects: | |
Online Access: | http://hdl.handle.net/11336/119256 |