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000058071 084__ $$2WoS$$aGeosciences, Multidisciplinary
000058071 1001_ $$0P:(DE-Juel1)VDB14612$$aFeck, T.$$b0$$uFZJ
000058071 245__ $$aSensitivity of Arctic ozone loss to stratospheric H2O
000058071 260__ $$aWashington, DC$$bAmerican Geophysical Union$$c2008
000058071 300__ $$a
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000058071 440_0 $$02249$$aGeophysical Research Letters$$v35$$x0094-8276$$yL01803
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000058071 520__ $$aLikely causes of a future increase in stratospheric H2O are a rise in tropospheric CH4 and H-2 leakages from an increased integration of hydrogen into the energy supply system. Here we evaluate the impact of potential future stratospheric H2O increases on Arctic ozone loss by comparing ozone loss proxies based on two different mechanisms of chlorine activation. In particular, the H2O dependence of the volume of air is analyzed where temperatures are low enough to form nitric acid trihydrate, denoted as V-PSC, and for C1 activation on liquid sulfate aerosols, denoted as V-AC1. We show that V-AC1 increases faster than VPSC with increasing H2O mixing ratios in the altitude range of 400 K to 550 K potential temperature. As a consequence, the additional ozone column loss is expected to be most pronounced for cold winters and large H2O increases and to be significantly higher when V-AC1 is used as a proxy.
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000058071 7001_ $$0P:(DE-Juel1)129122$$aGrooß, J.-U.$$b1$$uFZJ
000058071 7001_ $$0P:(DE-Juel1)129145$$aRiese, M.$$b2$$uFZJ
000058071 773__ $$0PERI:(DE-600)2021599-X$$a10.1029/2007GL031334$$gVol. 35$$q35$$tGeophysical research letters$$v35$$x0094-8276$$y2008
000058071 8567_ $$uhttp://dx.doi.org/10.1029/2007GL031334
000058071 8564_ $$uhttps://juser.fz-juelich.de/record/58071/files/2007GL031334.pdf$$yOpenAccess
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