On the modelled thermal response of the Antarctic stratosphere to a depletion of ozone

Details On the modelled thermal response of the Antarctic stratosphere to a depletion of ozone On the modelled thermal response of the Antarctic stratosphere to a depletion of ozone

Nov 1986

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1986georl..13.1331s&link_type=abstract

Geophysical Research Letters (Supplement) (ISSN 0094-8276), vol. 13, Nov. 1986, p. 1331-1334. NERC-supported research.

Physics

45

Antarctic Regions, Atmospheric Effects, Atmospheric Temperature, Ozone, Ozone Depletion, Stratosphere, Atmospheric Models, Cooling, Ice Clouds, Spring (Season)

Scientific paper

Simple models are used to investigate the effect of a spring-time depletion of ozone in the Antarctic on stratospheric temperatures. It is shown that coolings in excess of 5 K are possible in the lower stratosphere. No evidence for such changes exist. One possible mechanism that could offset this cooling involves the loss of water vapor from the lower stratosphere due to desiccation processes associated with polar stratospheric clouds.

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