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Titel Relative effect of slope and equilibrium line altitude on the retreat of Himalayan glaciers
VerfasserIn T. N. Venkatesh, A. V. Kulkarni, J. Srinivasan
Medientyp Artikel
Sprache Englisch
ISSN 1994-0416
Digitales Dokument URL
Erschienen In: The Cryosphere ; 6, no. 2 ; Nr. 6, no. 2 (2012-03-15), S.301-311
Datensatznummer 250003479
Publikation (Nr.) Volltext-Dokument vorhandencopernicus.org/tc-6-301-2012.pdf
 
Zusammenfassung
It has been observed that a majority of glaciers in the Himalayas have been retreating. In this paper, we show that there are two major factors which control the advance/retreat of the Himalayan glaciers. They are the slope of the glacier and changes in the equilibrium line altitude. While it is well known, that these factors are important, we propose a new way of combining them and use it to predict retreat. The functional form of this model has been derived from numerical simulations using an ice-flow code. The model has been successfully applied to the movement of eight Himalayan glaciers during the past 25 years. It explains why the Gangotri glacier is retreating while Zemu of nearly the same length is stationary, even if they are subject to similar environmental changes. The model has also been applied to a larger set of glaciers in the Parbati basin, for which retreat based on satellite data is available, though over a shorter time period.
 
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