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dc.contributor.authorHuybers, Peter John
dc.date.accessioned2017-10-27T19:24:49Z
dc.date.issued2009
dc.identifier.citationHuybers, P. 2009. “Antarctica’s Orbital Beat.” Science 325 (5944) (August 27): 1085–1086. doi:10.1126/science.1176186.en_US
dc.identifier.issn0036-8075en_US
dc.identifier.urihttp://nrs.harvard.edu/urn-3:HUL.InstRepos:34305980
dc.description.abstractAlternating glacial and interglacial conditions have dominated Earth's climate for at least the past 800,000 years (1, 2). Such a global rhythm of glaciation is surprising—at least if summer solar radiation controls glaciation (3)—because variations in Earth's orbit cause opposite changes in the intensity of northern and southern summer radiation. Deciphering the origins of the orbital period variations found in Antarctic proxies of climate may tell us why glaciations are global.en_US
dc.description.sponsorshipEarth and Planetary Sciencesen_US
dc.language.isoen_USen_US
dc.publisherAmerican Association for the Advancement of Science (AAAS)en_US
dc.relation.isversionofdoi:10.1126/science.1176186en_US
dash.licenseMETA_ONLY
dc.titleAntarctica's Orbital Beaten_US
dc.typeJournal Articleen_US
dc.description.versionVersion of Recorden_US
dc.relation.journalScienceen_US
dash.depositing.authorHuybers, Peter John
dash.embargo.until10000-01-01
dc.identifier.doi10.1126/science.1176186*
dash.contributor.affiliatedHuybers, Peter


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