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• W1969259132 abstract "Finite element model simulations of ice sheet dynamics are conducted to investigate the role of natural atmospheric CO2 variations (obtained from ice core bubbles) in creating climatic conditions necessary to glaciate the Eurasian Arctic. Effects of CO2 variations are sufficient to support extensive marine ice sheet and ice shelf development at the last glacial maximum and to deglaciate the region during the Holocene (from approximately 14 ka to 9 ka). The ice sheet coverage simulated for the last glacial maximum agrees with evidence for extensive ice sheet grounding over the shallow continental shelves of the Barents, Kara, Laptev, and East Siberian seas. An ice shelf also forms over the Arctic Ocean and Greenland and Norwegian seas." @default.
• W1969259132 created "2016-06-24" @default.
• W1969259132 creator A5078892564 @default.
• W1969259132 date "1990-04-01" @default.
• W1969259132 modified "2023-09-26" @default.
• W1969259132 title "The Eurasian Ice Sheet Formation and collapse resulting from natural atmospheric CO2concentration variations" @default.
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• W1969259132 doi "https://doi.org/10.1029/pa005i002p00207" @default.
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