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dc.contributor.authorMueller, Richard
dc.date.accessioned2010-10-12T19:29:54Z
dc.date.available2010-10-12T19:29:54Z
dc.date.issued2001
dc.identifier.urihttp://hdl.handle.net/11858/00-1735-0000-0001-322B-7
dc.description.abstractBesides measurements of atmospheric trace gases and laboratory studies of chemical reactions, modelling has been recognised to be of increasing importance to improve our knowledge of the atmosphere and the capabilities of photochemical models. Main scope of this work was the development of a photochemical atmospheric model, which was especielly designed for the interpretation of Differential Optical Absorption measurments (DOAS). This model has been used to improve our knowledge of atmospheric chemistry. For example, for the first time it was possible to demonstrate that a significant amount of IO in a range of 0.65 to 0.8 pptv is present in the stratosphere in the polar region (Ny-Alesund,Spitzbergen). Moreover it has been shown that such amounts of stratospheric IO lead to an additional Ozone loss in the range of 10 % in cold arctic winters.
dc.format.mimetypeapplication/pdf
dc.language.isodeu
dc.publisherUniv. Bremen
dc.rights.urihttp://e-docs.geo-leo.de/rights
dc.subject.ddc551.5
dc.subject.ddc550
dc.subject.gokTUA 700
dc.subject.gokTVA 210
dc.titleEntwicklung und Anwendung eines photochemischen schräge Säulen Modell-Paketes zur Interpretation von DOAS-Daten atmosphärischer Spurengase
dc.typemonograph
dc.subject.gokverbalVerfahren zur Untersuchung der freien Atmosphäre {Meteorologie}
dc.subject.gokverbalChemische Zusammensetzung der Atmosphäre {Meteorologie}
dc.identifier.doi10.23689/fidgeo-411
dc.identifier.ppn354452371
dc.type.versionpublishedVersion
dc.relation.collectionGeophysik
dc.description.typethesis


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