Publication:
Temporal 10Be variations in ice

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dc.contributor.authorBeer, Juerg
dc.contributor.authorAndrée, Michael
dc.contributor.authorOeschger, Hans
dc.contributor.authorStauffer, Bernhard
dc.contributor.authorBalzer, Richard
dc.contributor.authorBonani, Georges
dc.contributor.authorStoller, Christian
dc.contributor.authorSuter, Martin
dc.contributor.authorWölfli, Willy
dc.contributor.authorFinkel, Robert C.
dc.date.accessioned2024-09-02T17:48:57Z
dc.date.available2024-09-02T17:48:57Z
dc.date.issued1983
dc.description.abstract10Be (T1/2 = 1.5·106y) is mainly produced in the atmosphere by cosmic ray spallation reactions on nitrogen and oxygen. About 70 % of the production takes place in the stratosphere. 10Be becomes attached to aerosols within a very short time. If 10Be is produced in the stratosphere some latitudinal mixing occurs. Most of the 10Be is transferred to the troposphere during spring and early summer when, mainly at median latitudes, large stratospheric air masses enter the troposphere. Tropospheric 10Be is deposited rapidly on the earth's surface by precipitation. The mean residence time of 10Be in the atmosphere is ca 1 to 2 years. 10Be removed from the atmosphere by precipitation is either preserved in snow and ice layers, in the topsoil and the biosphere, or it enters the hydrosphere (oceans and lakes), where it is transported to the sediments.
dc.description.numberOfPages10
dc.description.sponsorshipPhysikalisches Institut
dc.identifier.doi10.48350/158695
dc.identifier.publisherDOI10.1017/S0033822200005579
dc.identifier.urihttps://boris-portal.unibe.ch/handle/20.500.12422/43311
dc.language.isoen
dc.publisherArizona Board of Regents, University of Arizona
dc.relation.ispartofRadiocarbon
dc.relation.issn0033-8222
dc.relation.organizationDCD5A442C44AE17DE0405C82790C4DE2
dc.relation.organizationDCD5A442BF29E17DE0405C82790C4DE2
dc.subject.ddc500 - Science::530 - Physics
dc.titleTemporal 10Be variations in ice
dc.typearticle
dspace.entity.typePublication
oaire.citation.endPage278
oaire.citation.issue2
oaire.citation.startPage269
oaire.citation.volume25
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oairecerif.author.affiliationPhysikalisches Institut
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unibe.date.licenseChanged2021-08-30 06:56:42
unibe.description.ispublishedpub
unibe.eprints.legacyId158695
unibe.journal.abbrevTitleRADIOCARBON
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