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000052930 017__ $$aAn edited version of this paper was published by AGU. Copyright 2001 American Geophysical Union. To view the published open abstract, go to http://dx.doi.org/10.1029/2006GL026925
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000052930 084__ $$2WoS$$aGeosciences, Multidisciplinary
000052930 1001_ $$0P:(DE-Juel1)VDB1652$$aTilmes, S.$$b0$$uFZJ
000052930 245__ $$aChemical ozone loss in the Arctic and Antarctic stratosphere between 1992 and 2005
000052930 260__ $$aWashington, DC$$bAmerican Geophysical Union$$c2006
000052930 300__ $$aL20812
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000052930 440_0 $$02249$$aGeophysical Research Letters$$v33$$x0094-8276
000052930 500__ $$aRecord converted from VDB: 12.11.2012
000052930 520__ $$a[1] The magnitude of chemical loss of polar ozone induced by anthropogenic halogens depends on the extent of chlorine activation, which is controlled by polar stratospheric clouds (PSCs) and thus by temperature. We propose a new quantity, the PSC formation potential (PFP) of the polar vortex, suitable for comparing the amount of ozone depletion in the Arctic and Antarctic regions. PFP represents the fraction of the vortex, over an ozone loss season, exposed to PSC temperatures. Chemical ozone loss in the Arctic correlates well with PFP, for winters between 1991 and 2005. For Antarctic and cold Arctic winters, PFP has been increasing over the past 30 years. In winter 2005, PFP and ozone loss in the Arctic reached record highs, approaching Antarctic levels. Nevertheless, column ozone in spring in the Arctic is much larger than the Antarctic, because of larger dynamical resupply of ozone to the Arctic.
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000052930 7001_ $$0P:(DE-Juel1)129138$$aMüller, R.$$b1$$uFZJ
000052930 7001_ $$0P:(DE-Juel1)VDB352$$aEngel, A.$$b2$$uFZJ
000052930 7001_ $$0P:(DE-Juel1)VDB8772$$aRex, M.$$b3$$uFZJ
000052930 7001_ $$0P:(DE-HGF)0$$aRussell, J. M.$$b4
000052930 773__ $$0PERI:(DE-600)2021599-X$$a10.1029/2006GL026925$$gVol. 33, p. L20812$$pL20812$$q33<L20812$$tGeophysical research letters$$v33$$x0094-8276$$y2006
000052930 8567_ $$uhttp://hdl.handle.net/2128/580$$uhttp://dx.doi.org/10.1029/2006GL026925
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