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Contribution of Alaskan glaciers to sea level rise derived from satellite imagery
Berthier E., Schiefer E., Clarke G. K. C., Menounos B., Rémy F.
Nature geoscience 3, 2 (2010) 92-95 - http://hal.archives-ouvertes.fr/hal-00537722
Articles dans des revues avec comité de lecture
Planète et Univers/Sciences de la Terre/Océanographie
Contribution of Alaskan glaciers to sea level rise derived from satellite imagery
Etienne Berthier 1, Eric Schiefer 2, Garry K. C. Clarke 3, Brian Menounos 4, Frédérique Rémy 1
1 :  Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS)
http://www.legos.obs-mip.fr/
CNRS : UMR5566 – Institut de recherche pour le développement [IRD] – CNES – Observatoire Midi-Pyrénées – INSU – Université Paul Sabatier [UPS] - Toulouse III
14 avenue Edouard Belin 31400 Toulouse
France
2 :  Department of Geography, Planning and Recreation (NAU)
Northern Arizona University
Box 15016 Flagstaff, Arizona 86011-5016
États-Unis
3 :  Earth and Ocean Sciences (EOS)
University of British Columbia
University of British Columbia, 6339 Stores Road, Vancouver, BC V6T 1Z4, Canada
Canada
4 :  Geography Program and Natural Resources Environmental Studies Institute (UNBC)
University of Northern British Columbia
Prince George, BC, Canada V2N 4Z9
Canada
Over the last 50 years, retreating glaciers and ice caps (GIC) contributed 0.5 mm/yr to sea level rises (SLR), and one third is believed to originate from ice masses bordering the Gulf of Alaska. However, these estimates of ice wastage in Alaska are based on methods that measure a limited number of glaciers and extrapolate the results to estimate ice loss for the many thousands of others. How these methods capture the complex pattern of decadal elevation changes at the scale of individual glacier and mountain range is unclear. Here, combining a comprehensive glacier inventory with elevation changes derived from sequential digital elevation models (DEMs), we found that, between 1962 and 2006, Alaskan glaciers lost 41.9 ± 8.6 km**3/yr water equivalent (w.e.) and contributed 0.12±0.02 mm/yr to SLR. Our ice loss is 34% lower than previous estimates. Reasons for our lower values include the higher spatial resolution of our glacier inventory and the reduction of ice thinning under debris and at the glacier margins which were not resolved in earlier work. Estimates of mass loss from GIC in other mountain regions could be subject to similar revisions.
Anglais

Nature geoscience
internationale
2010
3
2
92-95

Glacier – Alaska – Sea level rise – satellite – ASTER – SPOT5

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