Paleotopography of Glacial-Age Ice Sheets

The model of the paleotopography of glacial-age ice sheets suggesting a lower elevation for the northern hemisphere sheet than previously believed should be corrected for tectonic uplift in Papua New Guinea and Barbados.

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Bibliographic Details
Published inScience (American Association for the Advancement of Science) Vol. 267; no. 5197; pp. 536 - 538
Main Authors Edwards, R. Lawrence, Peltier, W. R.
Format Journal Article
LanguageEnglish
Published United States American Society for the Advancement of Science 27.01.1995
American Association for the Advancement of Science
The American Association for the Advancement of Science
Subjects
Atmospheric general circulation models
Climate models
Glacial epoch
Glacial landforms
Ice
Ice ages
Ice sheets
Modeling
Oceans
Sea level
Sea level rise
Technical Comments
Tectonic uplift
Online AccessGet full text
ISSN0036-8075
1095-9203
DOI10.1126/science.267.5197.536

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Summary:The model of the paleotopography of glacial-age ice sheets suggesting a lower elevation for the northern hemisphere sheet than previously believed should be corrected for tectonic uplift in Papua New Guinea and Barbados.
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ISSN:0036-8075
1095-9203
DOI:10.1126/science.267.5197.536