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...

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Bibliographic Details
Main Authors: Andreas Richter, Andreas Groh, Martin Horwath, Erik Ivins, Eric Marderwald, José Luis Hormaechea, Raúl Perdomo, Reinhard Dietrich
Format: Article
Language:English
Published: MDPI AG 2019-04-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/11/8/909