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000052348 0247_ $$2DOI$$a10.1029/2006GL028901
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000052348 084__ $$2WoS$$aGeosciences, Multidisciplinary
000052348 1001_ $$0P:(DE-Juel1)129122$$aGrooß, J.-U.$$b0$$uFZJ
000052348 245__ $$aSimulation of ozone loss in the Arctic winter 2004/05
000052348 260__ $$aWashington, DC$$bAmerican Geophysical Union$$c2007
000052348 29510 $$aGeophysical Research Letters
000052348 300__ $$aL05804
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000052348 440_0 $$02249$$aGeophysical Research Letters$$v34$$x0094-8276
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000052348 520__ $$aWe present simulations of stratospheric ozone depletion in the Arctic winter 2004/2005 by the Chemical Lagrangian Model of the Stratosphere (CLaMS). This winter is among the coldest on record with large observed ozone losses. It is also different from previously analyzed winters, as ozone mixing ratios within the polar vortex were not homogeneously distributed. The reason for the untypical ozone distribution is a second transport barrier that existed at the time of vortex formation. The simulations agree well with ozone measurements by the Fourier Transform Spectrometer (ACE-FTS). The simulated vortex average column ozone loss between 380 and 550 K potential temperature (+/- 1 sigma) was 69 +/- 21 Dobson Units on 23 March. The simulated ozone loss is in approximate agreement with some published estimates, but is significantly lower than others. A possible reason for this difference is the inhomogeneous ozone distribution within the vortex which makes it more complicated to estimate of ozone loss.
000052348 536__ $$0G:(DE-Juel1)FUEK406$$2G:(DE-HGF)$$aAtmosphäre und Klima$$cP22$$x0
000052348 542__ $$lAccepted for publication in Geophysical Reserch Letters. Copyright (2007) American
Geophysical Union. Further reproduction or electronic distribution is not permitted.
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000052348 7001_ $$0P:(DE-Juel1)129138$$aMüller, R.$$b1$$uFZJ
000052348 773__ $$0PERI:(DE-600)2021599-X$$a10.1029/2006GL028901$$gVol. 34, p. L05804$$pL05804$$q34<L05804$$tGeophysical research letters$$v34$$x0094-8276$$y2007
000052348 8567_ $$uhttp://dx.doi.org/10.1029/2006GL028901
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