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Melt rates at calving termini: a study at Glaciar León, Chilean Patagonia

By
Eleanor Haresign
Eleanor Haresign
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Charles R. Warren
Charles R. Warren
School of Geography and Geosciences, University of St Andrews, St Andrews, Fife KY16 9AL, Scotland, UK(e-mail: ech@st-andrews.ac.uk)
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Published:
January 01, 2005

Abstract

Glaeiar León, a temperate, grounded outlet of the North Patagonian Icefield, terminates at an active but stable calving margin in Lago Leones. Glaciological and limno-logical data gathered during 2001 and 2002 are used to examine the relative contributions of calving and melting to mass loss at the terminus, and the interplay between glacier and lake processes. The calving rate of 880 m/a in a mean water depth of 65 m is high for lake-calving glaciers. Subaerial melt rates at the terminus are small compared with calving rates, but melting at the waterline facilitates calving by undercutting the subaerial calving cliff. Ice-proximal surface water temperatures of 6–7°C allow waterline melt notches to grow at rates of c. 0.8 m/day, suggesting that melt-driven calving accounts for c. 23% of ice loss at the terminus. The significance of melting at calving termini decreases with increasing calving speeds, but is greater than simple calculations of melt losses suggest because of the process-linkage with calving.

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Contents

Geological Society, London, Special Publications

Cryospheric Systems: Glaciers and Permafrost

C. Harris
C. Harris
Cardiff University, UK
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J. B. Murton
J. B. Murton
University of Sussex, UK
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Geological Society of London
Volume
242
ISBN electronic:
9781862394902
Publication date:
January 01, 2005

GeoRef

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