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001     52348
005     20240712100855.0
024 7 _ |a 10.1029/2006GL028901
|2 DOI
024 7 _ |a WOS:000244707200008
|2 WOS
024 7 _ |a 0094-8276
|2 ISSN
024 7 _ |a 2128/649
|2 Handle
037 _ _ |a PreJuSER-52348
041 _ _ |a eng
082 _ _ |a 550
082 _ _ |a 550
084 _ _ |2 WoS
|a Geosciences, Multidisciplinary
100 1 _ |a Grooß, J.-U.
|0 P:(DE-Juel1)129122
|b 0
|u FZJ
245 _ _ |a Simulation of ozone loss in the Arctic winter 2004/05
260 _ _ |a Washington, DC
|b American Geophysical Union
|c 2007
295 1 0 |a Geophysical Research Letters
300 _ _ |a L05804
336 7 _ |a Journal Article
|0 PUB:(DE-HGF)16
|2 PUB:(DE-HGF)
336 7 _ |a Output Types/Journal article
|2 DataCite
336 7 _ |a Journal Article
|0 0
|2 EndNote
336 7 _ |a ARTICLE
|2 BibTeX
336 7 _ |a JOURNAL_ARTICLE
|2 ORCID
336 7 _ |a article
|2 DRIVER
440 _ 0 |a Geophysical Research Letters
|x 0094-8276
|0 2249
|v 34
500 _ _ |a Record converted from VDB: 12.11.2012
500 _ _ |a Record converted from JUWEL: 18.07.2013
520 _ _ |a We present simulations of stratospheric ozone depletion in the Arctic winter 2004/2005 by the Chemical Lagrangian Model of the Stratosphere (CLaMS). This winter is among the coldest on record with large observed ozone losses. It is also different from previously analyzed winters, as ozone mixing ratios within the polar vortex were not homogeneously distributed. The reason for the untypical ozone distribution is a second transport barrier that existed at the time of vortex formation. The simulations agree well with ozone measurements by the Fourier Transform Spectrometer (ACE-FTS). The simulated vortex average column ozone loss between 380 and 550 K potential temperature (+/- 1 sigma) was 69 +/- 21 Dobson Units on 23 March. The simulated ozone loss is in approximate agreement with some published estimates, but is significantly lower than others. A possible reason for this difference is the inhomogeneous ozone distribution within the vortex which makes it more complicated to estimate of ozone loss.
536 _ _ |a Atmosphäre und Klima
|c P22
|2 G:(DE-HGF)
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542 _ _ |l Accepted for publication in Geophysical Reserch Letters. Copyright (2007) American Geophysical Union. Further reproduction or electronic distribution is not permitted.
588 _ _ |a Dataset connected to Web of Science
650 _ 7 |a J
|2 WoSType
700 1 _ |a Müller, R.
|0 P:(DE-Juel1)129138
|b 1
|u FZJ
773 _ _ |a 10.1029/2006GL028901
|g Vol. 34, p. L05804
|p L05804
|q 34|0 PERI:(DE-600)2021599-X
|t Geophysical research letters
|v 34
|y 2007
|x 0094-8276
856 7 _ |u http://dx.doi.org/10.1029/2006GL028901
856 4 _ |u https://juser.fz-juelich.de/record/52348/files/2006gl028901_final.pdf
|y OpenAccess
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909 C O |o oai:juser.fz-juelich.de:52348
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913 1 _ |k P22
|v Atmosphäre und Klima
|l Atmosphäre und Klima
|b Umwelt
|z fortgesetzt als P23
|0 G:(DE-Juel1)FUEK406
|x 0
914 1 _ |y 2007
915 _ _ |0 StatID:(DE-HGF)0010
|a JCR/ISI refereed
915 _ _ |0 StatID:(DE-HGF)0510
|2 StatID
|a OpenAccess
915 _ _ |0 LIC:(DE-HGF)APS-112012
|2 HGFVOC
|a American Physical Society Transfer of Copyright Agreement
920 1 _ |k ICG-1
|l Stratosphäre
|d 30.09.2010
|g ICG
|0 I:(DE-Juel1)VDB790
|x 1
970 _ _ |a VDB:(DE-Juel1)82271
980 1 _ |a FullTexts
980 _ _ |a VDB
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980 _ _ |a journal
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980 _ _ |a UNRESTRICTED
980 _ _ |a JUWEL
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981 _ _ |a I:(DE-Juel1)IEK-7-20101013

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