Were Heinrich events forced from the southern hemisphere?

South African Journal of Science

Volumn 98, Issue 1-2, 2002, Pages 43-46

  Partridge, T C ^a  

^a UNIVERSITY OF THE WITWATERSRAND   (South Africa)

Author keywords

[No Author keywords available]

Indexed keywords

CARBON ISOTOPE; CLIMATE CHANGE; HEINRICH EVENT; SOUTHERN HEMISPHERE;

SOUTH AFRICA;

EID: 0036212983     PISSN: 00382353     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Review

References (28)

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3. Orbital forcing of climate over South Africa: A 200 000-year rainfall record from the Pretoria Saltpan
4. Tswaing: Investigations into the origin, age and palaeoenvironments of the Pretoria Saltpan
5. New chronological evidence for the nature and timing of linear dune development in the southwest Kalahari Desert
6. Multiple episodes of aridity in southern Africa since the last interglacial
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8. Late Quaternary evolution of the central southern Kalahari: Environmental responses to changing climatic conditions
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10. Diatoms from the Pretoria Saltpan - A record of lake evolution and environmental change
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12. Fission-track age of the Pretoria Saltpan impact crater
13. Conclusions and implications for a model of regional palaeoclimates during the last two glacial cycles
14. Origin of the northern Atlantic's Heinrich events
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16. Palaeoclimates of the arid and semi-arid zones of southern Africa during the last climatic cycle
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18. Iceberg discharges into the North Atlantic on millennial time scales during the last glaciation
19. Past and future reorganizations in the climate system
20. Climate change during the last deglaciation in Antarctica
21. Evolution of Cenozoic climates
22. Oceanic mechanisms for amplification of the 23 000-year ice-volume cycle
23. Oceanic response to orbital forcing in the late Quaternary: Observational and experimental strategies
24. Trade wind forcing of upwelling, seasonality, and Heinrich events as a response to sub-Milankovitch climate variability
25. Mechanisms forcing abrupt fluctuations of the Indian Ocean summer monsoon during the last deglaciation
26. Synchronous high-frequency oscillations in tropical sea surface temperatures and North Atlantic deep water production during the last glacial cycle
27. Evidence from U-Th dating against northern hemisphere forcing of the penultimate deglaciation