Regional insolation forcing of late Quaternary climate change in the Southern Hemisphere

Marcus J. Vandergoes (), Rewi M. Newnham, Frank Preusser, Chris H. Hendy, Thomas V. Lowell, Sean J. Fitzsimons, Alan G. Hogg, Haino Uwe Kasper and Christian Schlüchter
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Marcus J. Vandergoes: University of Maine
Rewi M. Newnham: University of Plymouth
Frank Preusser: University of Bern
Chris H. Hendy: Department of Chemistry
Thomas V. Lowell: University of Cincinnati
Sean J. Fitzsimons: University of Otago
Alan G. Hogg: University of Waikato
Haino Uwe Kasper: Universität zu Köln
Christian Schlüchter: University of Bern

Nature, 2005, vol. 436, issue 7048, 242-245

Abstract: North and south Southern New Zealand, positioned within the important southwesterly wind system, is a prime site for examining interhemispheric linkages in climate change. A series of cores drilled in the Okarito Pakihi peat bog now provides a continuous record of vegetation and climate change that may become a benchmark for the region. The data include clear evidence for modification of the global climate change signal in the Southern Hemisphere by local variation in the intensity of solar radiation.

Date: 2005
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DOI: 10.1038/nature03826

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