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On the role of precession in Quaternary glacial cycles

dc.contributor.authorGunning, Daniel Francis James
dc.contributor.authorNisancioglu, Kerim Hestnes
dc.contributor.authorVan de Wal, Rodecrick S.
dc.contributor.authorCapron, Emilie
dc.date.accessioned2024-11-04T09:43:27Z
dc.date.available2024-11-04T09:43:27Z
dc.date.created2024-08-29T00:17:43Z
dc.date.issued2023
dc.identifier.issn2411-605X
dc.identifier.urihttps://hdl.handle.net/11250/3163137
dc.description.abstractAn outstanding question of the Quaternary glacial cycles is the gradual emergence of a precession signal. Its absence in the Early Pleistocene may be explained by Northern Hemisphere ice sheets varying out-of-phase with a dynamic Antarctic ice sheet.en_US
dc.language.isoengen_US
dc.publisherPagesen_US
dc.relation.urihttps://doi.org/10.22498/pages.31.2.58
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleOn the role of precession in Quaternary glacial cyclesen_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
cristin.ispublishedtrue
cristin.fulltextoriginal
dc.identifier.doi10.22498/pages.31.2.58
dc.identifier.cristin2290283
dc.source.journalPast Global Changes Magazineen_US
dc.source.pagenumber58-59en_US
dc.relation.projectSigma2: NN4659Ken_US
dc.relation.projectEU – Horisont Europa (EC/HEU): 955750en_US
dc.relation.projectNorges forskningsråd: 324520en_US
dc.identifier.citationPast Global Changes Magazine. 2023, 31 (2), 58-59.en_US
dc.source.volume31en_US
dc.source.issue2en_US


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Except where otherwise noted, this item's license is described as Navngivelse 4.0 Internasjonal