Physical Characteristics and Modeling of the Greenland Ice Sheet. Progress Report to the National Science Foundation, Division of Polar Programs PDF Download
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Author: R. G. BARRY
Publisher:
ISBN:
Category :
Languages : en
Pages : 65
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Author: R. G. BARRY
Publisher:
ISBN:
Category :
Languages : en
Pages : 65
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Book Description
Author: Chester C. Langway
Publisher: American Geophysical Union
ISBN: 0875900577
Category : Greenland Ice Sheet Program
Languages : en
Pages : 127
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Author: PICO. Polar Ice Coring Office (PICO)
Publisher:
ISBN:
Category :
Languages : en
Pages : 33
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Author: Nicholas M. Short
Publisher:
ISBN:
Category : Science
Languages : en
Pages : 750
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Author: Robert A. Bindschadler
Publisher:
ISBN:
Category : Climatic changes
Languages : en
Pages : 64
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Proceedings of a workshop on the possibility of a rapid rise in sea level following the response of the West Antarctic ice sheet to global warming, and outline of a project to study the phenomenon, called SEARISE : Sea Level Response to Ice Sheet Evolution.
Author: National Science Foundation (U.S.)
Publisher:
ISBN:
Category : Research
Languages : en
Pages : 164
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Author: Robert A. Bindschadler
Publisher:
ISBN:
Category : Ice sheets
Languages : en
Pages : 68
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Author: University of Colorado Boulder. Cooperative Institute for Research in Environmental Sciences
Publisher:
ISBN:
Category : Glaciology
Languages : en
Pages : 193
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Aims at producing computerized ice sheet model. A third volume, part 4, containing annotated computer programmes also available from publisher.
Author: Johannes Oerlemans
Publisher: Springer Science & Business Media
ISBN: 9400963254
Category : Science
Languages : en
Pages : 220
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Book Description
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.
Author:
Publisher:
ISBN:
Category : Core drilling
Languages : en
Pages : 120
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