Radial and tangential gravity rates from GRACE in areas of glacial isostatic adjustment

In areas dominated by Glacial Isostatic Adjustment (GIA), the free-air gravity anomaly rate can be converted to uplift rate to good approximation by using a simple spectral relation. We provide quantitative comparisons between gravity rates derived from monthly gravity field solutions (GFZ Potsdam,...

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Bibliographic Details
Published in:Geophysical Journal International
Main Authors: van der Wal, Wouter, Kurtenbach, Enrico, Kusche, Jürgen, Vermeersen, Bert
Format: Text
Language:English
Published: Oxford University Press 2011
Subjects:
Online Access:http://gji.oxfordjournals.org/cgi/content/short/187/2/797
https://doi.org/10.1111/j.1365-246X.2011.05206.x