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Relative Timing of Deglacial Climate Events in Antarctica and Greenland
Citation
Morgan, VI and Delmotte, M and van Ommen, TD and Jouzel, J and Chappellaz, J and Woon, S and Masson-Delmotte, V and Raynaud, D, Relative Timing of Deglacial Climate Events in Antarctica and Greenland, Science, 297, (5588) pp. 1862-1864. ISSN 0036-8075 (2002) [Refereed Article]
DOI: doi:10.1126/science.1074257
Abstract
The last deglaciation was marked by large, hemispheric, millennial-scale climate variations: the Bølling-Allerød and Younger Dryas periods in the north, and the Antarctic Cold Reversal in the south. A chronology from the high-accumulation Law Dome East Antarctic ice core constrains the relative timing of these two events and provides strong evidence that the cooling at the start of the Antarctic Cold Reversal did not follow the abrupt warming during the northern Boiling transition around 14,500 years ago. This result suggests that southern changes are not a direct response to abrupt changes in North Atlantic thermohaline circulation, as is assumed in the conventional picture of a hemispheric temperature seesaw.
Item Details
| Item Type: | Refereed Article |
|---|---|
| Research Division: | Chemical Sciences |
| Research Group: | Analytical Chemistry |
| Research Field: | Separation Science |
| Objective Division: | Expanding Knowledge |
| Objective Group: | Expanding Knowledge |
| Objective Field: | Expanding Knowledge in the Chemical Sciences |
| UTAS Author: | Morgan, VI (Mr Vincent Morgan) |
| UTAS Author: | van Ommen, TD (Dr Tas van Ommen) |
| UTAS Author: | Woon, S (Ms Suenor Woon) |
| ID Code: | 26206 |
| Year Published: | 2002 |
| Web of Science® Times Cited: | 70 |
| Deposited By: | CRC-Antarctic and Southern Ocean Environm |
| Deposited On: | 2003-05-21 |
| Last Modified: | 2014-05-28 |
| Downloads: | 0 |
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