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Interhemispheric Differences in Dentifrication and Related Processes Affecting Polar Ozone

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dc.contributor.author Santee, M. L. en_US
dc.contributor.author Read, W. G. en_US
dc.contributor.author Waters, J. W. en_US
dc.contributor.author Froidevaux, L. en_US
dc.contributor.author Manney, G. L. en_US
dc.contributor.author Flower, D. A. en_US
dc.contributor.author Jarnot, R. F. en_US
dc.contributor.author Harwood, R. S. en_US
dc.contributor.author Peckham, G. E. en_US
dc.date.accessioned 2004-10-05T21:47:32Z
dc.date.available 2004-10-05T21:47:32Z
dc.date.issued 1994 en_US
dc.identifier.clearanceno 94-0551
dc.identifier.uri http://hdl.handle.net/2014/33820
dc.description.abstract The severe depletion of stratospheric ozone over Antarctica in late winter and early spring is caused by enhanced CLO abundances arising from heterogeneous reactions on polar stratospheric clouds (PSCs). CLO abundances comparable to those over Antarctica have also been observed throughout the Arctic Vortex, but the accompanying loss of Arctic ozone has been much less severe. en_US
dc.format.extent 1019349 bytes
dc.format.mimetype application/pdf
dc.language.iso en_US
dc.subject.other ozone depletion en_US
dc.title Interhemispheric Differences in Dentifrication and Related Processes Affecting Polar Ozone en_US


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