Show simple item record

dc.contributor.authorRoedel, Walter
dc.date.accessioned2021-02-11T19:31:29Z
dc.date.available2021-02-11T19:31:29Z
dc.date.issued1980-01-01
dc.identifier.citationRoedel, W. (1980). On the climate-radiocarbon relationship: Nitric oxide and ozone as connecting links between radiation and the earth's surface temperatures. Radiocarbon, 22(2), 250-259.
dc.identifier.issn0033-8222
dc.identifier.doi10.1017/S0033822200009528
dc.identifier.urihttp://hdl.handle.net/10150/652429
dc.description.abstractThe correlations between atmospheric radiocarbon cencentrations, on the one hand, and solar activity and the earth's magnetic field, on the other, as well as possible relations between surface temperatures and solar activity and the earth's magnetic field are considered. To draw a consistent picture of these relations, the following mechanisms for climatic changes are proposed: The earth's magnetic field and solar activity both influence the fluxes of charged solar particles into the upper stratosphere; higher surface temperatures are positively correlated with higher particles fluxes. Charged particles produce nitric oxide, which controls, to some extent, the ozone destruction and, thus, the ozone inventory in the upper layers of the stratosphere (above the 10 mbar level) in latitudes greater than about 60 degrees. The varying ozone contents in the upper stratosphere affect the radiation balance and the temperatures on the earth's surface. It has been estimated that a reduction, or increase, respectively, of ozone in the layers above 10 mbar warms, or cools, respectively, the earth's surface. A change of ozone in the lower layers of the stratosphere has the opposite effect. The maximum net effect is in the order of Delta-T is approximately equal to 0.3 1 K, in both directions. This hypothesis might be in accordance with an orbital origin of long-term climatic changes.
dc.language.isoen
dc.publisherAmerican Journal of Science
dc.relation.urlhttp://radiocarbon.webhost.uits.arizona.edu/
dc.rightsCopyright © The American Journal of Science
dc.rights.urihttp://rightsstatements.org/vocab/InC/1.0/
dc.titleOn the Climate-Radiocarbon Relationship: Nitric Oxide and Ozone as Connecting Links Between Radiation and the Earth's Surface Temperatures
dc.typeArticle
dc.typetext
dc.identifier.journalRadiocarbon
dc.description.noteThis material was digitized as part of a cooperative project between Radiocarbon and the University of Arizona Libraries.
dc.description.collectioninformationThe Radiocarbon archives are made available by Radiocarbon and the University of Arizona Libraries. Contact lbry-journals@email.arizona.edu for further information.
dc.eprint.versionFinal published version
dc.description.admin-noteMigrated from OJS platform February 2021
dc.source.volume22
dc.source.issue2
dc.source.beginpage250
dc.source.endpage259
refterms.dateFOA2021-02-11T19:31:29Z


Files in this item

Thumbnail
Name:
612-863-1-PB.pdf
Size:
988.2Kb
Format:
PDF

This item appears in the following Collection(s)

Show simple item record