Antarctic winter tropospheric warming—the potential role of polar stratospheric clouds, a sensitivity study

Abstract 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 CO 2 concentrations cooled the stratos...

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Bibliographic Details
Published in:Atmospheric Science Letters
Main Authors: Lachlan‐Cope, T. A., Connolley, W. M., Turner, J., Roscoe, H., Marshall, G. J., Colwell, S. R., Höpfner, M., Ingram, W.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2009
Subjects:
Antarctic
Antarc*
Online Access:http://dx.doi.org/10.1002/asl.237
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fasl.237
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/asl.237
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Summary:Abstract 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 CO 2 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 © 2009 Royal Meteorological Society and Crown Copyright

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