Present Day Regional Mass Loss of Greenland Observed with Satellite Gravimetry

19Citations
Citations of this article
43Readers
Mendeley users who have this article in their library.

This article is free to access.

Abstract

This paper summarizes results obtained for Greenland's mass balance observed with NASA's GRACE mission. We estimate a Greenland ice sheet mass loss at -201 ± 19 Gt/year including a discernible acceleration of -8 ± 7 Gt/year2 between March 2003 and February 2010. The mass loss of glacier systems on the South East of Greenland has slowed down while the mass loss increases toward the North along the West side of Greenland. The mass balance can be compared with results obtained by a regional climate model of the Greenland system and ice sheet altimeter data obtained from NASA's ICEsat mission. Our GRACE-only results differ to within 15% from these independently calculated values; we will comment on the possible causes and the quality of the glacial isostatic adjustment model which is used to correct geodetic datasets. © 2011 The Author(s).

Cite

CITATION STYLE

APA

Schrama, E., Wouters, B., & Vermeersen, B. (2011). Present Day Regional Mass Loss of Greenland Observed with Satellite Gravimetry. Surveys in Geophysics, 32(4–5), 377–385. https://doi.org/10.1007/s10712-011-9113-7

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free