Antarctic winter tropospheric warming - the potential role of polar stratospheric clouds, a sensitivity study
Lachlan-Cope, Thomas A. ORCID: https://orcid.org/0000-0002-0657-3235; Connolley, W.M.; Turner, John ORCID: https://orcid.org/0000-0002-6111-5122; Roscoe, Howard K.; Marshall, Gareth J. ORCID: https://orcid.org/0000-0001-8887-7314; Colwell, Steve R.; Höpfner, M.; Ingram, W.. 2009 Antarctic winter tropospheric warming - the potential role of polar stratospheric clouds, a sensitivity study. Atmospheric Science Letters, 10 (4). 262-266. https://doi.org/10.1002/asl.237
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Text (This article has been accepted for publication and will appear in a revised form in Atmospheric Science Letters, published by Wiley. Copyright Royal Meteorological Society. )
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Abstract/Summary
Over the last 30 years, Antarctic mid-tropospheric temperatures in winter have increased by 0.5 K per decade, the largest regional tropospheric warming observed. Over this period, amounts of polar stratospheric cloud(PSC) have also increased, as rising CO2 concentrations cooled the stratosphere. By imposing an idealisation of these increases in PSC within the radiation scheme of an atmosphere-only general circulation model, we find that they could have contributed to the observed warming. The present generation of global climate models do not properly represent PSCs, and so these results demonstrate the need to improve the representation of PSCs. Copyright. (C) 2009 Royal Meteorological Society and Crown Copyright
Item Type: | Publication - Article |
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Digital Object Identifier (DOI): | https://doi.org/10.1002/asl.237 |
Programmes: | BAS Programmes > Polar Science for Planet Earth (2009 - ) > Climate |
ISSN: | 1530-261X |
Additional Keywords: | polar meteorology; polar stratospheric clouds; climate change |
NORA Subject Terms: | Meteorology and Climatology Physics Earth Sciences Atmospheric Sciences |
Date made live: | 13 Dec 2010 14:34 +0 (UTC) |
URI: | https://nora.nerc.ac.uk/id/eprint/11118 |
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