Author: Cold Regions Research and Engineering Laboratory (U.S.)
Publisher:
ISBN:
Category : Engineering
Languages : en
Pages : 32

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Author: Cold Regions Research and Engineering Laboratory (U.S.)
Publisher:
ISBN:
Category : Engineering
Languages : en
Pages : 62

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Author: Henri Bader
Publisher:
ISBN:
Category : Ice
Languages : en
Pages : 56

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Author: Malcolm Mellor
Publisher:
ISBN:
Category : Ice
Languages : en
Pages : 68

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Author:
Publisher:
ISBN:
Category : Cold regions
Languages : en
Pages : 56

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Author: R.R. Bowker Company. Department of Bibliography
Publisher:
ISBN:
Category : United States
Languages : en
Pages : 1454

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Author: Henri Bader
Publisher:
ISBN:
Category : Ice
Languages : en
Pages : 0

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The mean elevation of the bed of the ice sheet is 620 m (2060 ft), and almost 1/3 of its area lies below sea level. The mean thickness of the ice sheet (equal to the difference between the mean elevations of surface and bed) is 1515 m (4970 ft). The ice volume is 2,600,000 cu km = 620,000 cu mi. The water equivalent is 2,350,000 cu km (560,000 cu mi). If distributed over the world's oceans, it would raise the sea level by 6.5 m (21 ft). The maximum thickness of the ice sheet is about 3000 m (10,000 ft). (Author).

Author: R.R. Bowker Company
Publisher: R. R. Bowker
ISBN:
Category : Reference
Languages : en
Pages : 1446

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Author:
Publisher:
ISBN:
Category : Cold regions
Languages : en
Pages : 60

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Author: Johannes Oerlemans
Publisher: Springer Science & Business Media
ISBN: 9400963254
Category : Science
Languages : en
Pages : 220

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Climate modelling is a field in rapid development, and the fltudy of cryospheric processes has become an important part of it. On smaller time scales, the effect of snow cover and sea ice on the atmospheric circulation is of concern for long-range weather forecasting. Thinking in decades or centuries, the effect of a C02 climatic warming on the present-day ice sheets, and the resulting changes in global sea level, has drawn a lot of attention. In particular, the dynamics of marine ice sheets (ice sheets on a bed that would be below sea level after removal of ice and full isostatic rebound) is a subject of continuous research. This interest stems from the fact that the West Antarctic Ice Sheet is a marine ice sheet which, according to some workers, may be close to a complete collapse. The Pleistocene ice ages, or glacial cycles, are best characterized by total ice volume on earth, indicating that on 4 5 large time scales (10 to 10 yr) ice sheets are a dominant component of the climate system. The enormous amount of paleoclimatic information obtained from deep-sea sediments in the last few decades has led to a complete revival of iriterest in the physical aspects of the Pleistocene climatic evolution.