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Climate of the Past An interactive open-access journal of the European Geosciences Union
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Volume 9, issue 2 | Copyright

Special issue: Progress in paleoclimate modelling

Clim. Past, 9, 517-524, 2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 01 Mar 2013

Research article | 01 Mar 2013

Southern westerlies in LGM and future (RCP4.5) climates

Y. Chavaillaz1, F. Codron1, and M. Kageyama2 Y. Chavaillaz et al.
  • 1LMD/IPSL, Laboratoire de Météorologie Dynamique, UMR8539, CNRS, Université Pierre et Marie Curie, Case Postale 99, 4 Place Jussieu, 75252 Paris Cedex 05, France
  • 2LSCE/IPSL, Laboratoire des Sciences du Climat et de l'Environnement, UMR8112, CEA-CNRS-UVSQ – CE Saclay, L'Orme des Merisiers, Bat. 701, 91191 Gif-sur-Yvette Cedex, France

Abstract. Mid-latitude westerlies are a major component of the atmospheric circulation and understanding their behaviour under climate change is important for understanding changes in precipitation, storms and atmosphere–ocean momentum, heat and CO2 exchanges. The Southern Hemisphere westerlies have been particularly studied in terms of the latter aspects, since the Southern Ocean is a key region for the global oceanic circulation as well as for CO2 uptake. In this study, we analyse, mainly in terms of jet stream position, the behaviour of the southern westerlies for the Last Glacial Maximum (LGM, 21 000 yr ago, which is the last past cold extreme) and for a future climate, obtained after stabilisation of the RCP4.5 scenario. The a priori guess would be that the behaviour of the westerly jet stream would be similar when examining its changes from LGM to pre-industrial (PI) conditions and from PI to RCP4.5, i.e. in both cases a poleward shift in response to global warming. We show that this is in fact not the case, due to the impact of altitude changes of the Antarctic ice sheet and/or to sea ice cover changes.

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