我没有辱骂
发表于 2025-3-21 18:59:11
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assent
发表于 2025-3-21 23:48:26
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.
不愿
发表于 2025-3-22 02:42:58
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Endearing
发表于 2025-3-22 06:08:54
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
使高兴
发表于 2025-3-22 09:56:45
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使满足
发表于 2025-3-22 13:46:08
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流浪者
发表于 2025-3-22 19:27:13
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hegemony
发表于 2025-3-22 21:35:52
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金盘是高原
发表于 2025-3-23 03:45:49
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.
挖掘
发表于 2025-3-23 07:00:40
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.