Sticky spots and a catastrophe possibility in West Antarctica
It is known that reloading of the central regions of Antarctica from the ice mass accumulated there occurs mainly by means of the outlet glaciers and ice flows that are sometimes called ice streams. A supposition is put forward about another cause that slows down the B stream: the existence of the s...
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Veröffentlicht in: | Doklady earth sciences 2011-04, Vol.437 (2), p.486-489 |
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Format: | Artikel |
Sprache: | eng |
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Online-Zugang: | Volltext |
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Zusammenfassung: | It is known that reloading of the central regions of Antarctica from the ice mass accumulated there occurs mainly by means of the outlet glaciers and ice flows that are sometimes called ice streams. A supposition is put forward about another cause that slows down the B stream: the existence of the so-called clinging patches at the bed of the glacier. |
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ISSN: | 1028-334X 1531-8354 |
DOI: | 10.1134/S1028334X11040027 |