Titlebook: Ice in the Climate System; W. Richard Peltier Conference proceedings 1993 Springer-Verlag Berlin Heidelberg 1993 Eis.Orbit.Scale.Snow.Tide

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書目名稱Ice in the Climate System影響因子(影響力)




書目名稱Ice in the Climate System影響因子(影響力)學(xué)科排名




書目名稱Ice in the Climate System網(wǎng)絡(luò)公開度




書目名稱Ice in the Climate System網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Ice in the Climate System被引頻次




書目名稱Ice in the Climate System被引頻次學(xué)科排名




書目名稱Ice in the Climate System年度引用




書目名稱Ice in the Climate System年度引用學(xué)科排名




書目名稱Ice in the Climate System讀者反饋




書目名稱Ice in the Climate System讀者反饋學(xué)科排名

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Modelling of the Fennoscandian Ice Sheetion is based on a degree day method that was used for the Greenland ice sheet (Reeh, 1991). The complete model is forced by uniform changes in atmospheric temperature. The model results show that the initiation of the Fennoscandian ice sheet is not easy, and requires more severe climatic conditions than had been expected.

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Endearing

Conference proceedings 1993an ice sheet, which consisted of three interconnected ice domes --the Scandinavian, Kara, and East Siberian. The Kara Sea glacier was largely a marine ice dome grounded on the sea‘s continental shelf. The ice dome discharged its ice in all directions, northward into the deep Arctic Basin, southward

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hegemony

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Modelling Ice Sheet and Climate Changes through the Ice Agesdrock depression. The recognition of these phase shifts, caused primarily by the slow ice sheet response and feedback, may assist the interpretation of phase differences observed in proxy paleorecords.

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Qualitative Dynamics of Marine Ice Sheets streams, these ice streams may not be very important in determining the overall stability of marine ice sheets and indeed may stabilise them. The conclusions regarding ice streams rest upon a new vertically integrated mechanical model of the sheet-stream-shelf transition.