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Analysis of Alpine glacier length change records with a macroscopic glacier model

Bibliographic Data

ID18976146
AuthorsM P Lüthi (0000-0003-4419-8496, Ecole polytechnique fédérale de Lausanne, corresponding author), Andreas Bauder (0000-0001-7197-7706, Ecole polytechnique fédérale de Lausanne)
Year2010
Volume65
Issue2
Pages92-102
Publication date2010-06-30
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueGeographica Helvetica (JOURNAL)
Journal identifiersISSN: 0016-7312 • E-ISSN: 2194-8798
PublisherCopernicus GmbH (PUBLISHER • DE)
DOI10.5194/gh-65-92-2010
OpenAlexW2329416894
LanguageEN
References cited6

The length change record of 91 glaciers in the Swiss Alps was analyzed with a novel macroscopic glacier model (LV-model). Based on a history of equilibrium line variations, synthetic length change data were calculated. From the LV-models matching best the measured length changes, characteristic parameters were obtained. The volume time scale thus determined ranges from 5 to 170 years for glaciers of different slope and length. The analysis shows that the observed glacier length changes cannot be reproduced with an equilibrium line variation based on temperature and precipitation alone. The equilibrium line has to be lowered by 100 to 200 meters during several phases of the Little Ice Age (in the time span 1650 to 1850) to obtain observed glacier responses. Such an effect might be attributable to either higher winter precipitation in the Alps, or to radiation forcing

Climate change · Climatology · Geography · Geomorphology · Glacier · Glacier mass balance · Length scale · Mechanics · Meteorology · Physical geography · Physics · Precipitation · Climate change and permafrost · Cryospheric studies and observations · Geology · Geology and Paleoclimatology Research · Oceanography

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Citation velocityhistorical
Highly citedNo
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