|Insolation-driven changes in atmospheric circulation over the past 116,000 years in subtropical Brazil.|
Insolation-driven changes in atmospheric circulation over the past
116,000 years in subtropical Brazil.
Nature, Vol. 434, No. 7029, pp. 63 - 66, 3 March 2005.
Francisco W. Cruz Jr.1,2, Stephen J. Burns1, Ivo Karmann2, Warren D. Sharp3, Mathias Vuille1, Andrea O. Cardoso4, José A. Ferrari5, Pedro L. Silva Dias4 and Oduvaldo Viana Jr2
1 Department of Geosciences, University of Massachusetts, Amherst, 01002 Massachusetts, USA
2Instituto de Geociencias,Universidade de São Paulo, Rua do Lago 562, São Paulo, SP, 05508-080, Brazil
3Berkeley Geochronology Center, 2455 Ridge Rd, Berkeley, California 94709, USA
4Departamento de Ciencias Atmosféricas, Instituto de Astronomia, Geofísica e Ciencias Atmosféricas,Universidade de São Paulo, Rua do Matão 1226, São Paulo, SP 05508-090, Brazil
5Instituto Geológico, Av. Miguel Stefano 3900, São Paulo, SP 04301-903, Brazil
During the last glacial period, large millennial-scale temperature oscillations-the 'Dansgaard/Oeschger' cycles-were the primary climate signal in Northern Hemisphere climate archives from the high latitudes to the tropics. But whether the influence of these abrupt climate changes extended to the tropical and subtropical Southern Hemisphere, where changes in insolation are thought to be the main direct forcing of climate, has remained unclear. Here we present a high-resolution oxygen isotope record of a U/Th-dated stalagmite from subtropical southern Brazil, covering the past 116,200 years. The oxygen isotope signature varies with shifts in the source region and amount of rainfall in the area, and hence records changes in atmospheric circulation and convective intensity over South America. We find that these variations in rainfall source and amount are primarily driven by summer solar radiation, which is controlled by the Earth's precessional cycle. The Dansgaard/ Oeschger cycles can be detected in our record and therefore we confirm that they also affect the tropical hydrological cycle, but that in southern subtropical Brazil, millennial-scale climate changes are not as dominant as they are in the Northern Hemisphere.
Download data from the WDC Paleo archive:
Botuverá Cave Stalagmite Stable Isotope Data
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It was published in Nature, Vol. 434, pp. 63 - 66, 3 March 2005.
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National Oceanic and Atmospheric Administration
16 March 2005