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Titlebook: Dynamics of the West Antarctic Ice Sheet; Proceedings of a Wor C. J. Veen,J. Oerlemans Conference proceedings 1987 D. Reidel Publishing Com

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書目名稱Dynamics of the West Antarctic Ice Sheet
副標(biāo)題Proceedings of a Wor
編輯C. J. Veen,J. Oerlemans
視頻videohttp://file.papertrans.cn/285/284217/284217.mp4
叢書名稱Glaciology and Quaternary Geology
圖書封面Titlebook: Dynamics of the West Antarctic Ice Sheet; Proceedings of a Wor C. J. Veen,J. Oerlemans Conference proceedings 1987 D. Reidel Publishing Com
描述Few scientists doubt the prediction that the antropogenic release of carbon dioxide in the atmosphere will lead to some warming of the earth‘s climate. So there is good reason to investigate the possible effects of such a warming, in dependence of geographical and social- economic setting. Many bodies, governmental or not, have organized meetings and issued reports in which the carbon dioxide problem is defined, reviewed, and possible threats assessed. The rate at which such reports are produced still increases. However, while more and more people are getting involved in the ‘carbon dioxide business‘, the number of investigators working on the basic problems grows, in our view, too slowly. Many fundamental questions are still not answered in a satisfactory way, and the carbon dioxide building rests on a few thin pillars. One such fundamental question concerns the change in sea level associated with a climatic warming of a few degrees. A number of processes can be listed that could all lead to changes of the order of tens of centimeters (e. g. thermal expansion, change in mass balance of glaciers and ice sheets). But the picture of the carbon dioxide problem has frequently be made m
出版日期Conference proceedings 1987
關(guān)鍵詞Ice shelf; Scale; atmosphere; climate; subglacial; temperature; water; hydrogeology
版次1
doihttps://doi.org/10.1007/978-94-009-3745-1
isbn_softcover978-94-010-8171-9
isbn_ebook978-94-009-3745-1Series ISSN 0924-5006
issn_series 0924-5006
copyrightD. Reidel Publishing Company, Dordrecht, Holland 1987
The information of publication is updating

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Quantitative Estimates of the Mass Flux and Ice Movement Along the Ice Edges in the Eastern and Sour than previous estimates..Most of the major ice shelves in the Weddell Sea region show steadily advancing ice fronts during the period of observation. This has the consequence that the source region for icebergs during this time should be limited mainly to ice fronts in the eastern Weddell Sea. The
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Ice Stream-Ice Shelf Interaction in West Antarctica,d ridges instead of the smoother surface of Ice Stream C. Regions of Ice Stream B with a lower surface elevation move faster than higher elevation regions, presumably because the lower-elevation ice is thinner and experiences less basal friction. Surface strain rates at Ice Stream B vary on a scale
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Longitudinal Stresses and Basal Sliding: A Comparative Study,975). In the latter model, longitudinal deviatoric stresses play a minor role and have very little effect on the model results. The two other models yield virtually the same results. This means that indeed the gradient of the deviatoric stress along a flowline may be neglected. In fact, the results
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A Subglacial Aquifer Bed Model and Water Pressure Dependent Basal Sliding Relationship for a West Aund to be the cause of the 1982–1983 surge of Variegated Glacier in Alaska, may be typical of the flow regime of this ice stream. The bed model and inferred subglacial water pressures are consistent with (1) the calculated subglacial water flux, (2) the thickness of a porous water-saturated subglaci
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Numerical Modelling of the Large-Scale Basal Water Flux under the West Antarctic Ice Sheet, pattern of steady-state mean water-film thickness is then interpreted in terms of its possible relationships to the basal sliding rates and the basal shear stress particularly under the major ice streams.
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Modelling the Response of the West Antarctic Ice Sheet to a Climatic Warming, the Antarctic ice shelves and the resulting increased strain rates which could then occur near the grounding lines..A hierarchy of ice-sheet modelling studies has been carried out covering the fast-flowing ice streams, the ice sheet thermal regime and the whole Antarctic at a coarser resolution. Th
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Women Entrepreneurs and Successr than previous estimates..Most of the major ice shelves in the Weddell Sea region show steadily advancing ice fronts during the period of observation. This has the consequence that the source region for icebergs during this time should be limited mainly to ice fronts in the eastern Weddell Sea. The
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