Antarctic outlet glacier mass change resolved at basin scale from satellite gravity gradiometry

The orbit and instrumental measurement of the Gravity Field and Steady State Ocean Circulation Explorer (GOCE) satellite mission offer the highest ever resolution capabilities for mapping Earth's gravity field from space. However, past analysis predicted that GOCE would not detect changes in ic...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Bouman, J. (author), Fuchs, M. (author), Ivins, E. (author), Van der Wal, W. (author), Schrama, E.J.O. (author), Visser, P.N.A.M. (author), Horwath, M. (author)
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 2014
Subjects:
basin-scale ice mass change
Amundsen Sea Sector
Antarctica
satellite gravimetry
Amundsen Sea
Antarctic
Getz
Getz Ice Shelf
Pine Island Glacier
Thwaites Glacier
West Antarctica
Antarc*
Ice Sheet
Ice Shelf
Pine Island
Online Access:https://doi.org/10.1002/2014GL060637
http://resolver.tudelft.nl/uuid:b1ae5c0c-ac8c-4650-a53f-361887f8b31a

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