Oceanic environment of George VI Ice Shelf, Antarctic Peninsula
Talbot, M.H.. 1988 Oceanic environment of George VI Ice Shelf, Antarctic Peninsula. Annals of Glaciology, 11. 161-164. 10.3189/S0260305500006480
Full text not available from this repository. (Request a copy)Abstract/Summary
A collation of available data shows that sea-water with a temperature 3°C above the in-situ freezing point lies beneath George VI Ice Shelf in the Antarctic Peninsula, and is widespread on the Amundsen-Bellingshausen continental shelf. The presence of warm water is a factor in the recent and continuing disintegration of ice shelves in the region, yet the meteorology and oceanography of the sector are little known. We discuss a plausible link between the present climatic conditions, sea-water characteristics and the warm-water intrusion on to the continental shelf, thereby illustrating an indirect climatic influence on the mass balance of ice shelves.
Item Type: | Publication - Article |
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Digital Object Identifier (DOI): | 10.3189/S0260305500006480 |
ISSN: | 0260-3055 |
Date made live: | 13 Dec 2018 11:39 +0 (UTC) |
URI: | https://nora.nerc.ac.uk/id/eprint/521870 |
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