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...

Full description

Bibliographic Details
Published in:Remote Sensing
Main Authors: Richter, Andreas Jorg, Groh, Andreas, Horwath, Martin, Ivins, Erik, Marderwald, Eric Rodolfo, Hormaechea, José Luis, Perdomo, Raúl, Dietrich, Reinhard
Format: Article in Journal/Newspaper
Language:English
Published: MDPI
Subjects:
Online Access:http://hdl.handle.net/11336/119256