Regional acceleration in ice mass loss from Greenland and Antarctica using GRACE time-variable gravity data
We use Gravity Recovery and Climate Experiment (GRACE) monthly gravity fields to determine the regional acceleration in ice mass loss in Greenland and Antarctica for 2003-2013. We find that the total mass loss is controlled by only a few regions. In Greenland, the southeast and northwest generate 70...
Main Authors: | , , |
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Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
eScholarship, University of California
2014
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Subjects: | |
Online Access: | https://escholarship.org/uc/item/3794v25j |