Hostname: page-component-cd9895bd7-p9bg8 Total loading time: 0 Render date: 2024-12-26T07:08:45.952Z Has data issue: false hasContentIssue false

Lakes on George VI Ice Shelf, Antarctica

Published online by Cambridge University Press:  27 October 2009

Extract

George VI Ice Shelf is about 450 km long, 20–70 km wide, and averages 250 m in thickness. It is bordered by Alexander Island to the west and by the Antarctic Peninsula to the east (Fig 1). The ice shelf is fed by glaciers flowing westwards from the Palmer Land plateau. In summer (November to late February) the ice shelf undergoes considerable surface melting and meltwater lakes form over an area of 4 500 km2 between 70°15′S and 72°00′S. The lakes and pools vary in size from a few centimetres deep and several square metres in area to a few metres deep covering areas of several square kilometres (Fig 2). Most of the lakes are characteristically elongate and ribbon-like and hence are termed ‘ribbon lakes’. From mid November to late February the lakes are a major obstacle to sledge parties travelling over the ice shelf.

Type
Articles
Copyright
Copyright © Cambridge University Press 1981

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Bishop, J. F. and Walton, J. L. W. (in press). Bottom melting under George VI Ice Shelf, Antarctica. Journal of Glaciology.Google Scholar
Gerdel, R. W. 1948. Penetration of radiation into the snow pack. Transactions. American Geophysical Union, Vol 29, No 3, p 366–74.Google Scholar
Grenfell, T. C. and Maykut, G. A. 1977.The optical properties of ice and snow in the Arctic Basin. Journal of Glaciology, Vol 18, No 80, p 445–63.CrossRefGoogle Scholar
Gurling, P. 1980. Some notes on a sledge journey from Stonington Island 1940–41. Polar Record, Vol 19, No 123, p 613–16.CrossRefGoogle Scholar
Megahan, W. F.and others. 1970. The effect of albedo-reducing materials on net radiation at a snow surface. Bulletin of the International Association for Scientific Hydrology, Vol 15, No 1, p 6980.CrossRefGoogle Scholar
Mellor, M. and McKinnon, G. 1960. The Amery Ice Shelf and its hinterland. Polar Record, Vol 10, No 64, p 3034.Google Scholar
Østrem, G. 1959. Ice melting under a thin layer of moraine and the existence of ice-cores in moraine ridges. Geografiska Annaler, Vol 41, No 4, p 228–30.Google Scholar
Paterson, W. S. B. 1969. The physics of glaciers. Oxford, Pergamon Press.Google Scholar
Pearson, M. R. and Rose, I. H. (in press). The dynamics of George VI Ice Shelf. British Antarctic Survey Bulletin, No 52.Google Scholar
Reynolds, J. M. (in press). The distribution of mean annual temperatures in the Antarctic Peninsula. British Antarctic Survey Bulletin, No 54.Google Scholar
Reynolds, J. M. and Paren, J. G. 1980. Recrystallization and the electrical behaviour of glacier ice. Nature, Vol 283, No 5742, p 6364.CrossRefGoogle Scholar
Rose, I. H. and Pearson, M. R. 1971. Fossil Bluff Glaciology, 1971. Cambridge, British Antarctic Survey. (Unpublished Report No G/1971/KG).Google Scholar
Sanderson, T. J. O. 1978. Thermal stresses near the surface of a glacier. Journal of Glaciology, Vol 20, No 83, p 257–83.Google Scholar
Stephenson, A. and Fleming, W. L. S. 1940. King George the Sixth Sound. The Geographical Journal, Vol 96, No 3, p 153–66.Google Scholar
Wager, A. C. 1972. Flooding of the ice shelf in George VI Sound. British Antarctic Survey Bulletin, No 28, p 7174.Google Scholar