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AGU: Geophysical Research Letters

 

Keywords

  • GRACE
  • gravity change
  • Patagonia Icefield
  • ice melting

Index Terms

  • Geodesy and Gravity: Time variable gravity
  • Geodesy and Gravity: Mass balance
  • Geodesy and Gravity: Global change from geodesy
  • Cryosphere: Glaciers
  • Global Change: Sea level change

Abstract

Patagonia Icefield melting observed by Gravity Recovery and Climate Experiment (GRACE)

J. L. Chen

Center for Space Research, University of Texas at Austin, Austin, Texas, USA

C. R. Wilson

Center for Space Research, University of Texas at Austin, Austin, Texas, USA

Department of Geological Sciences, University of Texas at Austin, Austin, Texas, USA

B. D. Tapley

Center for Space Research, University of Texas at Austin, Austin, Texas, USA

D. D. Blankenship

Institute for Geophysics, University of Texas at Austin, Austin, Texas, USA

E. R. Ivins

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

Using recently released reprocessed gravity solutions from the Gravity Recovery and Climate Experiment (GRACE), we estimate the ice loss rate for the Patagonia Icefield (PIF) of South America, for the period April 2002 through December 2006. After postglacial rebound and hydrological effects are corrected, the estimated rate is −27.9 ± 11 km3/year, equivalent to an average loss of ∼−1.6 m/year ice thickness change if evenly distributed over the entire PIF area. The estimated contribution to global sea level rise is 0.078 ± 0.031 mm/year. This is an independent confirmation of relatively large melting rate estimates from earlier studies employing topographic and cartographic data.

Received 30 August 2007; accepted 22 October 2007; published 17 November 2007.

Citation: Chen, J. L., C. R. Wilson, B. D. Tapley, D. D. Blankenship, and E. R. Ivins (2007), Patagonia Icefield melting observed by Gravity Recovery and Climate Experiment (GRACE), Geophys. Res. Lett., 34, L22501, doi:10.1029/2007GL031871.

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