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AGU: Geophysical Research Letters

 

Keywords

  • glaciology
  • mass balance
  • sea level

Index Terms

  • Cryosphere: Glaciers
  • Cryosphere: Ice sheets
  • Cryosphere: Mass balance
  • Global Change: Cryospheric change
  • Global Change: Climate dynamics

Abstract

GEOPHYSICAL RESEARCH LETTERS, VOL. 35, L20502, 5 PP., 2008
doi:10.1029/2008GL035417

Mass balance of the Greenland ice sheet from 1958 to 2007

E. Rignot

Department of Earth System Science, University of California, Irvine, California, USA

Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA

J. E. Box

Byrd Polar Research Center, Ohio State University, Columbus, Ohio, USA

E. Burgess

Department of Geography, University of Utah, Salt Lake City, Utah, USA

E. Hanna

Department of Geography, University of Sheffield, Sheffield, UK

We combine estimates of the surface mass balance, SMB, of the Greenland ice sheet for years 1958 to 2007 with measurements of the temporal variability in ice discharge, D, to deduce the total ice sheet mass balance. During that time period, we find a robust correlation (R2 = 0.83) between anomalies in SMB and in D, which we use to reconstruct a continuous series of total ice sheet mass balance. We find that the ice sheet was losing 110 ± 70 Gt/yr in the 1960s, 30 ± 50 Gt/yr or near balance in the 1970s–1980s, and 97 ± 47 Gt/yr in 1996 increasing rapidly to 267 ± 38 Gt/yr in 2007. Multi-year variations in ice discharge, themselves related to variations in SMB, cause 60 ± 20% more variation in total mass balance than SMB, and therefore dominate the ice sheet mass budget.

Received 21 July 2008; accepted 22 September 2008; published 22 October 2008.

Citation: Rignot, E., J. E. Box, E. Burgess, and E. Hanna (2008), Mass balance of the Greenland ice sheet from 1958 to 2007, Geophys. Res. Lett., 35, L20502, doi:10.1029/2008GL035417.

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