Hostname: page-component-77c89778f8-gq7q9 Total loading time: 0 Render date: 2024-07-19T20:49:52.829Z Has data issue: false hasContentIssue false

Climatology and implications for perennial lake ice occurrence at Bunger Hills Oasis, East Antarctica

Published online by Cambridge University Press:  12 May 2004

Peter T. Doran
Affiliation:
Biological Sciences Center, Desert Research Institute, Box 60220, Reno, NV 89506, USA
C.P. McKay
Affiliation:
MS 245-3, NASA-Ames Research Center, Moffett Field, CA 94035, USA
M.A. Meyer
Affiliation:
Biological Sciences Center, Desert Research Institute, Box 60220, Reno, NV 89506, USA
D.T. Andersen
Affiliation:
MS 245-3, NASA-Ames Research Center, Moffett Field, CA 94035, USA
R.A. Wharton
Affiliation:
Biological Sciences Center, Desert Research Institute, Box 60220, Reno, NV 89506, USA
J.T. Hastings
Affiliation:
Biological Sciences Center, Desert Research Institute, Box 60220, Reno, NV 89506, USA

Abstract

The Bunger Hills Oasis (66°15'S; 100°45'E), a large ice-free expanse on the coast of East Antarctica, contains many lakes, only a few of which maintain an ice cover all year. To understand the environmental conditions that allow for persistent ice cover we established an automatic meteorological station on White Smoke Lake, a perennially ice-covered lake in contact with the Apfel Glacier. The data were collected from January 1992–July 1993. The mean annual solar flux during this period was 115 W m−2, the mean wind speed 4.6 m S−1, and the mean air temperature −11.2°C. Summer degree-days above freezing (71 °C-days) are similar to regions of the Antarctic (the McMurdo Dry Valleys - 78°45'S; 163°00'E) with thick perennial lake ice but the winter freezing degree days (3987 °C-Days) are much smaller and are closer to regions with seasonal ice covers (e.g. the high Arctic). The Bunger Hills Oasis seems to be in a marginal climatic region for the persistence of thick lake ice. Therefore, the extent of glacier ice contact becomes the controlling factor in maintaining an ice cover all year. We propose that this is either through the heat sink the glacier offers, and/or the positive feedback for ice growth provided by the high albedo of the adjacent glacier.

Type
Papers—Atmospheric Sciences
Copyright
© Antarctic Science Ltd 1996

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.)