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AGU: Geophysical Research Letters

 

Index Terms

  • Global Change: Impact phenomena
  • Global Change: Remote sensing
  • Hydrology: Glaciology
  • Hydrology: Snow and ice

Abstract

GEOPHYSICAL RESEARCH LETTERS, VOL. 31, L21402, 4 PP., 2004
doi:10.1029/2004GL020816

Rapid disintegration of Alpine glaciers observed with satellite data

Frank Paul

Department of Geography, University of Zurich-Irchel, Zurich, Switzerland

Andreas Kääb

Department of Geography, University of Zurich-Irchel, Zurich, Switzerland

Max Maisch

Department of Geography, University of Zurich-Irchel, Zurich, Switzerland

Tobias Kellenberger

Department of Geography, University of Zurich-Irchel, Zurich, Switzerland

Wilfried Haeberli

Department of Geography, University of Zurich-Irchel, Zurich, Switzerland

Analyses of multispectral satellite data indicate accelerated glacier decline around the globe since the 1980s. By using digitized glacier outlines inferred from the 1973 inventory and Landsat Thematic Mapper (TM) satellite data from 1985 to 1999, we obtained area changes of about 930 Alpine glaciers. The 18% area reduction as observed for the period 1985 to 1999 (−1.3% a−1) corresponds to a seven times higher loss rate compared to the 1850–1973 decadal mean. Extrapolation of area change rates and cumulative mass balances to all Alpine glaciers yields a corresponding volume loss of about 25 km3 since 1973. Highly individual and non-uniform changes in glacier geometry (disintegration) indicate a massive down-wasting rather than a dynamic response to a changed climate. Our results imply stronger ongoing glacier retreat than assumed so far and a probable further enhancement of glacier disintegration by positive feedbacks.

Received 23 June 2004; accepted 6 October 2004; published 12 November 2004.

Citation: Paul, F., A. Kääb, M. Maisch, T. Kellenberger, and W. Haeberli (2004), Rapid disintegration of Alpine glaciers observed with satellite data, Geophys. Res. Lett., 31, L21402, doi:10.1029/2004GL020816.

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