Cited by 3,277

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The Last Glacial Maximum

Clark, Peter U., Dyke, Arthur S., Shakun, Jeremy D., Carlson, Anders E., Clark, Jorie, Wohlfarth, Barbara, Mitrovica, Jerry X., Hostetler, Steven W., McCabe, A. Marshall·2009·Science

Abstract

The Melting Is in the Details: Global sea level rises and falls as ice sheets and glaciers melt and grow, providing an integrated picture of the changes in ice volume but little information about how much individual ice fields are contributing to those variations. Knowing the regional structure of ice variability during glaciations and deglaciations will clarify the mechanisms of the glacial cycle. Clark et al. (p. 710 ) compiled and analyzed more than 5000 radiocarbon and cosmogenic surface exposure ages in order to develop a record of maximum regional ice extent around the time of the Last Glacial Maximum. The responses of the Northern and Southern Hemispheres differed significantly, which reveals how the evolution of specific ice sheets affected sea level and provides insight into how insolation controlled the deglaciation.

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Crossref · 10.1126/science.1172873

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  • The southern margin of the Cordilleran Ice Sheet reached its maximum several thousand years after the peak in global ice volume at around 20-19 ka.

    “The southern margin of the ice sheet reached its maximum several thousand years after the peak in global ice volume at around 20-19 ka (Carlson & Clark, 2012;Clark et al., 2009;Lambeck et al., 2014;Lisiecki & Raymo, 2005).”

    From Retreat of the Western Cordilleran Ice Sheet Margin During the Last Deglaciation (2018) · cites this paper as Clark et al., 2009

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Metadata

Authors
Clark, P. U., Dyke, A. S., Shakun, J. D., Carlson, A. E., Clark, J., Wohlfarth, B., Mitrovica, J. X., Hostetler, S. W., & McCabe, A. M.
Affiliations
  • Department of Geosciences, Oregon State University, Corvallis, OR 97331, USA.
  • Geological Survey of Canada, 601 Booth Street, Ottawa, Ontario K1A 0E8, Canada.
  • Department of Geology and Geophysics, University of Wisconsin, Madison, WI 53706, USA.
  • Department of Geology and Geochemistry, Stockholm University, SE-10691, Stockholm, Sweden.
  • Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138, USA.
  • U.S. Geological Survey, Department of Geosciences, Oregon State University, Corvallis, OR 97331, USA.
  • School of Environmental Science, University of Ulster, Coleraine, County Londonderry, BT52 1SA, UK.
Venue
Science
Published
2009-08-07
Volume
325
Issue
5941
Pages
710-714
ISSN
  • 0036-8075
  • 1095-9203
Cited by
3,277
References
0
Language
en

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