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Publication:
Atmospheric CO2 concentrations over the last glacial termination

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dc.contributor.authorMonnin, Eric
dc.contributor.authorIndermühle, Andreas
dc.contributor.authorDällenbach, Andre ́
dc.contributor.authorFlückiger, Jacqueline
dc.contributor.authorStauffer, Bernhard
dc.contributor.authorStocker, Thomas
dc.contributor.authorRaynaud, Dominique
dc.contributor.authorBarnola, Jean-Marc
dc.date.accessioned2024-09-02T17:43:47Z
dc.date.available2024-09-02T17:43:47Z
dc.date.issued2001
dc.description.abstractA record of atmospheric carbon dioxide (CO2) concentration during the transition from the Last Glacial Maximum to the Holocene, obtained from the Dome Concordia, Antarctica, ice core, reveals that an increase of 76 parts per million by volume occurred over a period of 6000 years in four clearly distinguishable intervals. The close correlation between CO2 concentration and Antarctic temperature indicates that the Southern Ocean played an important role in causing the CO2 increase. However, the similarity of changes in CO2 concentration and variations of atmospheric methane concentration suggests that processes in the tropics and in the Northern Hemisphere, where the main sources for methane are located, also had substantial effects on atmospheric CO2 concentrations.
dc.description.numberOfPages3
dc.description.sponsorshipPhysikalisches Institut
dc.description.sponsorshipPhysikalisches Institut, Klima- und Umweltphysik (KUP)
dc.identifier.doi10.48350/158269
dc.identifier.publisherDOI10.1126/science.291.5501.112
dc.identifier.urihttps://boris-portal.unibe.ch/handle/20.500.12422/43025
dc.language.isoen
dc.publisherAmerican Association for the Advancement of Science
dc.relation.ispartofScience
dc.relation.issn0036-8075
dc.relation.organizationDCD5A442BF29E17DE0405C82790C4DE2
dc.relation.organizationDCD5A442C44AE17DE0405C82790C4DE2
dc.subject.ddc500 - Science::530 - Physics
dc.titleAtmospheric CO2 concentrations over the last glacial termination
dc.typearticle
dspace.entity.typePublication
oaire.citation.endPage114
oaire.citation.issue5501
oaire.citation.startPage112
oaire.citation.volume291
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oairecerif.author.affiliationPhysikalisches Institut
oairecerif.author.affiliationPhysikalisches Institut, Klima- und Umweltphysik (KUP)
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unibe.date.licenseChanged2021-08-19 07:57:46
unibe.description.ispublishedpub
unibe.eprints.legacyId158269
unibe.journal.abbrevTitleSCIENCE
unibe.refereedTRUE
unibe.subtype.articlejournal

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