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The Influence of 5000 Year-old and Younger Glacial Mass Variability on Present-Day Crystal Rebound in the Antarctic Peninsula

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dc.contributor.author Ivins, E. en_US
dc.contributor.author Raymond, C. en_US
dc.contributor.author James, T. en_US
dc.date.accessioned 2004-09-23T20:56:48Z
dc.date.available 2004-09-23T20:56:48Z
dc.date.issued 2000 en_US
dc.identifier.citation Earth, Planets and Space en_US
dc.identifier.citation USA en_US
dc.identifier.clearanceno 00-1369 en_US
dc.identifier.uri http://hdl.handle.net/2014/15657
dc.description.abstract Assessment of Antarctic rebound is complicated by two issues: (1) The total ice volume at Last Glacial Maximum is contentious, with estimates ranging from just a few meters to several tens of meters equivalent eustatic sea level rise. en_US
dc.format.extent 3365669 bytes
dc.format.mimetype application/pdf
dc.language.iso en_US
dc.subject.other GPS glacier mass balance mantle viscosity antarctic ice sheet en_US
dc.title The Influence of 5000 Year-old and Younger Glacial Mass Variability on Present-Day Crystal Rebound in the Antarctic Peninsula en_US


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