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,...
Published in: | Geophysical Journal International |
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Main Authors: | , , , |
Format: | Text |
Language: | English |
Published: |
Oxford University Press
2011
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Subjects: | |
Online Access: | http://gji.oxfordjournals.org/cgi/content/short/187/2/797 https://doi.org/10.1111/j.1365-246X.2011.05206.x |