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A Reconciled Estimate of Glacier Contributions to Sea Level Rise: 2003 to 2009

  • Alex S. Gardner*
  • , Geir Moholdt
  • , J. Graham Cogley
  • , Bert Wouters
  • , Anthony A. Arendt
  • , John Wahr
  • , Etienne Berthier
  • , Regine Hock
  • , W. Tad Pfeffer
  • , Georg Kaser
  • , Stefan R. M. Ligtenberg
  • , Tobias Bolch
  • , Martin J. Sharp
  • , Jon Ove Hagen
  • , Michiel R. van den Broeke
  • , Frank Paul
  • *Corresponding author for this work
  • University of Colorado Boulder
  • University of Bristol
  • University of Alaska Fairbanks
  • Utrecht University
  • University of Zurich
  • University of Oslo
  • Clark University
  • University of Michigan, Ann Arbor
  • Scripps Research Institute
  • Trent University
  • CNRS Centre National de la Recherche Scientifique
  • Uppsala University
  • University of Innsbruck
  • University of Massachusetts Medical School
  • University of Alberta

Research output: Contribution to journalArticleAcademicpeer-review

Abstract

Glaciers distinct from the Greenland and Antarctic Ice Sheets are losing large amounts of water to the world's oceans. However, estimates of their contribution to sea level rise disagree. We provide a consensus estimate by standardizing existing, and creating new, mass-budget estimates from satellite gravimetry and altimetry and from local glaciological records. In many regions, local measurements are more negative than satellite-based estimates. All regions lost mass during 2003-2009, with the largest losses from Arctic Canada, Alaska, coastal Greenland, the southern Andes, and high-mountain Asia, but there was little loss from glaciers in Antarctica. Over this period, the global mass budget was -259 +/- 28 gigatons per year, equivalent to the combined loss from both ice sheets and accounting for 29 +/- 13% of the observed sea level rise.

Original languageEnglish
Pages (from-to)852-857
Number of pages6
JournalScience
Volume340
Issue number6134
DOIs
Publication statusPublished - 17 May 2013

Funding

We thank K. Matsuo, M. Huss, T. Jacob, A. Kaab, S. Luthcke, A. Willsman, M. Willis, and I. Sasgen for updated or early access to regional estimates of glacier mass change; M. Flanner, T. Jacob, and S. Swenson for helping with analysis of the hydrologic models; A. Bliss, N. Molg, C. Nuth, P. Rastner, M. Willis, and G. Wolken for providing regional areas of ocean-terminating glacier basins; J. Lenaerts and J. van Angelen for providing RACMO2 output for Greenland and Antarctica; J. Box and C. Chen for making available Greenland Ice Sheet snowline estimates; G. A, R. Riva, and P. Stocchi for providing glacial isostatic adjustment models; and C. Starr and the NASA/Goddard Space Flight Center Scientific Visualization Studio for help with Fig. 1. This work was supported by funding to A. S. G. and M. J. S. from the Natural Sciences and Engineering Research Council of Canada, G. M. from NASA award NNX09AE52G, B. W. from a Marie Curie International Outgoing Fellowship within the 7th European Community Framework Programme (FP7-PEOPLE-2011-IOF-301260), E. B. from the TOSCA program of the French Space Agency (CNES), R. H. from NASA grants NNX11AF41G and NNX11A023G and NSF grant ANT-1043649, G. K. from Austrian Science Fund (FWF) grant P25362-N26, T. B. from the Deutsche Forschungsgemeinschaft (DFG, BO 3199/2-1), and F. P. from European Space Agency project Glaciers_cci (4000101778/10/I-AM).

Keywords

  • ICESAT LASER ALTIMETRY
  • MASS-BALANCE
  • CAPS
  • GREENLAND
  • AMERICA

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