Asynchrony of Antarctic and Greenland climate change during the last glacial period
A central issue in climate dynamics is to understand how the Northern and Southern hemispheres are coupled during climate events. The strongest of the fast temperature changes observed in Greenland (so-called Dansgaard–Oeschger events) during the last glaciation have an analogue in the temperature r...
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| Veröffentlicht in: | Nature (London) 1998-08, Vol.394 (6695), p.739-743 |
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| creator | Blunier, T. Chappellaz, J. Schwander, J. Dällenbach, A. Stauffer, B. Stocker, T. F. Raynaud, D. Jouzel, J. Clausen, H. B. Hammer, C. U. Johnsen, S. J. |
| description | A central issue in climate dynamics is to understand how the Northern and Southern hemispheres are coupled during climate events. The strongest of the fast temperature changes observed in Greenland (so-called Dansgaard–Oeschger events) during the last glaciation have an analogue in the temperature record from Antarctica. A comparison of the global atmospheric concentration of methane as recorded in ice cores from Antarctica and Greenland permits a determination of the phase relationship (in leads or lags) of these temperature variations. Greenland warming events around 36 and 45 kyr before present lag their Antarctic counterpart by more than 1 kyr. On average, Antarctic climate change leads that of Greenland by 1–2.5 kyr over the period 47–23 kyr before present. |
| doi_str_mv | 10.1038/29447 |
| format | Article |
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| source | Springer Nature - Complete Springer Journals; Nature Journals Online |
| subjects | Climate Climate change Continental interfaces, environment Earth sciences Earth, ocean, space Exact sciences and technology Glaciation Humanities and Social Sciences Ice ages Marine Marine and continental quaternary multidisciplinary Ocean, Atmosphere Science Science (multidisciplinary) Sciences of the Universe Surficial geology Temperature |
| title | Asynchrony of Antarctic and Greenland climate change during the last glacial period |
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