Regional ice-mass changes and glacial-isostatic adjustment in Antarctica from GRACE

We infer regional mass changes in Antarctica using ca. 4 years of Gravity Recovery and Climate Experiment (GRACE) level 2 data. We decompose the time series of the Stokes coefficients into their linear as well as annual and semi-annual components by a least-squares adjustment and apply a statistical...

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Bibliographic Details
Published in:Earth and Planetary Science Letters
Main Authors: Sasgen, I., Martinec, Z., Fleming, K.
Other Authors: 1.3 Earth System Modelling, 1.0 Geodesy and Remote Sensing, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum
Format: Article in Journal/Newspaper
Language:unknown
Published: 2007
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_236033
https://gfzpublic.gfz-potsdam.de/pubman/item/item_236033_1/component/file_236032/10449.pdf