Low potential for stratospheric dynamical change to be implicated in the large winter warming in the central Antarctic Peninsula

Stratospheric change associated with the Antarctic ozone hole is clearly implicated in changing surface climate near 65°S in late summer, in both measurements and models, via downward propagation of height anomalies following the final warming. But one of the largest changes in surface temperature i...

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Bibliographic Details
Published in:Quarterly Journal of the Royal Meteorological Society
Main Authors: Roscoe, H.K., Marshall, G.J., King, J.C.
Format: Article in Journal/Newspaper
Language:unknown
Published: Royal Meteorological Society 2006
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/113/
https://doi.org/10.1256/qj.05.81