Possible long-term changes in stratospheric circulation: evidence from total ozone measurements at the edge of the Antarctic vortex in early winter

Measurements of total ozone in Antarctica during early winter show an increase, consistent with the observed descent of stratospheric air and the convergence that accompanies descent. Measurements in the vortex edge region at Faraday (65°S) show that the rate of increase has on average doubled betwe...

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Bibliographic Details
Published in:Quarterly Journal of the Royal Meteorological Society
Main Authors: Roscoe, H.K., Fowler, C.L., Shanklin, J.D., Hill, J.G.T.
Format: Article in Journal/Newspaper
Language:unknown
Published: Royal Meteorological Society 2004
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/12396/
http://onlinelibrary.wiley.com/doi/10.1256/qj.03.70/pdf