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Nature 419, 465-467 (3 October 2002) | doi:10.1038/nature01081;
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Chemical Reaction Engineering & Reactor Design
- Praj Matrix - Praj Industries Ltd
- Pune, Maharashtra Pune-411021 India
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- South Dakota State University
- Brookings, SD
Switch of flow direction in an Antarctic ice stream
Fast-flowing ice streams transport ice from the interior of West Antarctica to the ocean, and fluctuations in their activity control the mass balance of the ice sheet. The mass balance of the Ross Sea sector of the West Antarctic ice sheet is now positive—that is, it is growing—mainly because one of the ice streams (ice stream C) slowed down about 150 years ago.
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