Modelling of the Fennoscandian Ice Sheet
作者： Anne Letréguilly , Catherine Ritz
DOI: 10.1007/978-3-642-85016-5_2
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摘要: The Fennoscandian ice sheet is simulated by means of a numerical model. model includes three main parts: Ice flow mechanics (with the isothermal approximation), mass balance, and bedrock isostasy. balance based on atmospheric humidity, takes into account effect orographically induced precipitation, which causes zones high precipitation to shift with edge (Sanberg Oerlemans, 1981). ablation degree day method that was used for Greenland (Reeh, 1991). complete forced uniform changes in temperature. results show initiation not easy, requires more severe climatic conditions than had been expected.
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sci-hub.st 参考文章(15)
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