Glacial Isostatic Adjustment (GIA) in Greenland: A Review

Leanne Wake; Benoit Lecavalier; Mike Bevis

doi:10.1007/s40641-016-0040-z

Glacial Isostatic Adjustment (GIA) in Greenland: A Review

Leanne Wake, Benoit Lecavalier, Mike Bevis

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Abstract

Using the most recently published regional and global deglaciation histories we provide updated estimates of the Glacial Isostatic Adjustment (GIA) component of present day uplift at a suite of GPS sites in Greenland. The GIA of the solid Earth beneath Greenland contributes -6 to +10 Gt/yr to the present day mass trends observed by the Gravity Recovery and Climate Experiment (GRACE), representing

Original language	English
Pages (from-to)	101-111
Journal	Current Climate Change Reports
Volume	2
Issue number	3
Early online date	5 Jul 2016
DOIs	https://doi.org/10.1007/s40641-016-0040-z
Publication status	Published - Sept 2016

Keywords

Geodesy
Greenland Ice Sheet
Glacial Isostatic Adjustment

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10.1007/s40641-016-0040-zLicence: CC BY

Art 3A10Final published version, 1.36 MBLicence: CC BY

Cite this

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KW - Geodesy

KW - Greenland Ice Sheet

KW - Glacial Isostatic Adjustment

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Glacial Isostatic Adjustment (GIA) in Greenland: A Review

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Keywords

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