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• W2089634315 abstract "Abstract The Greenland ice-sheet and Canadian Arctic ice-cap record of the last interglacial (undertood broadly as marine Isotopic Stage 5) is critically reviewed. Lack of age control on the deep ice-core records leaves open two largely different interpretations of the climate in marine Isotopic Stage 5: either most of Stage 5 (with the exception of Substage 5e) experienced a cold climate, and the main change from interglacial to glacial conditions took place at the boundary between Substages 5e and 5d; or, during much of Stage 5 the climate was integracial type, i.e. as warm as, or warmer than at present, with Substage 5d as the only period with a glacial type climate. It is concluded that most of the ‘hard’ evidence is in favour of the latter scenario. Ice-sheet dynamic model studies, using the ‘warm’ marine Isotopic Stage 5 scenario, indicate that the Greenland ice sheet in the warmest periods of Stage 5 had split up into a main ice sheet covering central and northern Greenland, and a much smaller ice cap over the southeastern highlands. The Greenland record of marine Isotopic Stage 5 is then discussed in relation to other paleoclimatic and paleoenvironmental records. The possibility of major inter-hemispheric differences of the climate in mid and late marine Isotopic Stage 5 is discussed. It is concluded that it is important to study the entire marine Isotopic Stage 5 (not only Substage 5e) in order to understand possible differences in the global climatic responses to nearly indentical peaks in orbitally driven summer insolation changes in the northern hemisphere." @default.
• W2089634315 created "2016-06-24" @default.
• W2089634315 creator A5091675030 @default.
• W2089634315 date "1991-01-01" @default.
• W2089634315 modified "2023-09-27" @default.
• W2089634315 title "The last interglacial as recorded in the greenland ice sheet and Canadian Arctic ice caps" @default.
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• W2089634315 doi "https://doi.org/10.1016/1040-6182(91)90045-p" @default.
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