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• W2069185979 abstract "CR Climate Research Contact the journal Facebook Twitter RSS Mailing List Subscribe to our mailing list via Mailchimp HomeLatest VolumeAbout the JournalEditorsSpecials CR 20:1-7 (2002) - doi:10.3354/cr020001 A relief-specific model of the ice age on the basis of uplift-controlled glacier areas in Tibet and the corresponding albedo increase as well as their positive climatological feedback by means of the global radiation geometry Matthias Kuhle* Geographisches Institut der Universität Göttingen, Goldschmidtstraße 5, 37077 Göttingen, Germany *E-mail: mkuhle@gwdg.de ABSTRACT: The onset of the ice age era at ~2.75 Ma BP and its increasing intensity from ~1 Ma BP onwards cannot be explained by variations of the Earth¹s orbit. Evidence supporting a 2.4 million km2 ice sheet on the Tibetan plateau during the Last Glacial Maximum has led to the hypothesis that the resulting albedo-induced heat loss in the Earth¹s atmosphere may have triggered global ice ages. Recent data obtained from marine and terrestrial sediment records now confirm the climatic-ecological impact of a Tibetan glaciation; they also show that the development of Tibet¹s ice sheet was synchronous with the onset and intensification of global ice ages. KEY WORDS: Ice ages · Tibetan ice sheet · Quaternary climate Full text in pdf format NextExport citation RSS - Facebook - Tweet - linkedIn Cited by Published in CR Vol. 20, No. 1. Online publication date: February 12, 2002 Print ISSN: 0936-577X; Online ISSN: 1616-1572 Copyright © 2002 Inter-Research." @default.
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• W2069185979 date "2002-01-01" @default.
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• W2069185979 title "A relief-specific model of the ice age on the basis of uplift-controlled glacier areas in Tibet and the corresponding albedo increase as well as their positive climatological feedback by means of the global radiation geometry" @default.
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• W2069185979 doi "https://doi.org/10.3354/cr020001" @default.
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