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Interhemispheric Differences in Dentifrication and Related Processes Affecting Polar OzoneThe 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.
Document ID
20060042287
Acquisition Source
Jet Propulsion Laboratory
Document Type
Preprint (Draft being sent to journal)
External Source(s)
Authors
Santee, M. L.
Read, W. G.
Waters, J. W.
Froidevaux, L.
Manney, G. L.
Flower, D. A.
Jarnot, R. F.
Harwood, R. S.
Peckham, G. E.
Date Acquired
August 23, 2013
Publication Date
January 1, 1994
Distribution Limits
Public
Copyright
Other
Keywords
ozone depletion

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