Stratospheric influence on circulation changes in the Southern Hemisphere troposphere in coupled climate models

Karpechko, A. Yu, Gillett, N. P., Marshall, G. J. and Scaife, A. A. (2008) Stratospheric influence on circulation changes in the Southern Hemisphere troposphere in coupled climate models. Geophysical Research Letters, 35 (20). ISSN 1944-8007

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Abstract

The recent intensification of the circumpolar circulation in the SH troposphere in summer and autumn has been attributed to external forcing such as stratospheric ozone depletion and greenhouse gas (GHG) increases. Several studies have shown that climate models are able to simulate observed changes when forced by observed ozone trends or combined ozone and GHG trends. However, as some of these studies suffered from erroneously specified forcing, the reason for the circulation intensification remains debatable. Here, we re-approach this issue using data from 21 CMIP3 models. We demonstrate that only models that include ozone depletion simulate downward propagation of the circulation changes from the stratosphere to the troposphere similar to that observed, with GHG increases causing significant Antarctic geopotential height trends only in the lower troposphere. These changes are simulated by the majority of the ozone-forced models except those with the lowest vertical resolution between 300 hPa and 10 hPa.

Item Type:	Article
Uncontrolled Keywords:	sdg 12 - responsible consumption and production,sdg 13 - climate action ,/dk/atira/pure/sustainabledevelopmentgoals/responsible_consumption_and_production
Faculty \ School:	Faculty of Science > School of Environmental Sciences
UEA Research Groups:	Faculty of Science > Research Groups > Climatic Research Unit
Depositing User:	Rosie Cullington
Date Deposited:	01 Mar 2011 15:34
Last Modified:	15 Jun 2023 17:31
URI:	https://ueaeprints.uea.ac.uk/id/eprint/25444
DOI:	10.1029/2008GL035354

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