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Clim. Past Discuss., 7, 4375-4399, 2011
www.clim-past-discuss.net/7/4375/2011/
doi:10.5194/cpd-7-4375-2011
© Author(s) 2011. This work is distributed
under the Creative Commons Attribution 3.0 License.


Precipitation variability in the winter rainfall zone of South Africa during the last 1400 yr linked to the austral westerlies

J. C. Stager1,2, P. A. Mayewski1, J. White2, B. M. Chase3,4, F. H. Neumann5,6, M. E. Meadows7, C. D. King2, and D. A. Dixon1
1Climate Change Institute, University of Maine, Orono, ME 04473, USA
2Natural Sciences, Paul Smith's College, Paul Smiths, NY 12970, USA
3Institut des Sciences de l'Evolution de Montpellier, Département Paléoenvironnements et Paléoclimats (PAL), UMR5554, Université Montpellier 2, Montpellier cedex 5, France
4Department of Archaeology, History, Culture and Religion, University of Bergen, P.O. Box 7805, 5020, Bergen, Norway
5Forschungsstelle für Paläobotanik, Westfälische Wilhelms-Universität Münster, Hindenburgplatz 57, 48143 Münster, Germany
6Bernard Price Institute for Palaeontological Research, University of the Witwatersrand Private Bag 3, Wits 2050, South Africa
7Department of Environmental and Geographical Science, University of Cape Town, Private Bag X3, Rondebosch 7701, South Africa

Abstract. The austral westerlies strongly influence precipitation and ocean circulation in the southern temperate zone, with important consequences for cultures and ecosystems. Global climate models anticipate poleward contraction of the austral westerlies with future warming, but the available paleoclimate records that might test these models have been largely limited to South America, are not fully consistent with each other, and may be complicated by influences from other climatic factors. Here we present the first fine-interval diatom and sedimentological records from the winter rainfall region of South Africa, representing precipitation during the last 1400 yr. Inferred rainfall increased ~1400–1200 cal yr BP and most notably during the Little Ice Age with pulses centered on ~600, 530, 470, 330, 200, and 90 cal yr BP. Synchronous fluctuations in Antarctic ice core chemistry strongly suggest that these variations are linked to changes in the westerlies. Partial inconsistencies among South African and South American records warn against the simplistic application of local-scale histories to the Southern Hemisphere as a whole. Nonetheless, these findings in general do support model projections of increasing aridity in austral winter rainfall zones with future warming.

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Citation: Stager, J. C., Mayewski, P. A., White, J., Chase, B. M., Neumann, F. H., Meadows, M. E., King, C. D., and Dixon, D. A.: Precipitation variability in the winter rainfall zone of South Africa during the last 1400 yr linked to the austral westerlies, Clim. Past Discuss., 7, 4375-4399, doi:10.5194/cpd-7-4375-2011, 2011.   Bibtex   EndNote   Reference Manager    XML