History of the atmosphere from ice cores
Ice cores are an excellent way of finding out how the atmosphere has changed because climate signals and many forcing factors for climate are present in the same core. Their main disadvantage is that they are only available in the polar regions and at a few unusual sites elsewhere. Cores range from...
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ftnerc:oai:nora.nerc.ac.uk:502794 2023-05-15T13:48:07+02:00 History of the atmosphere from ice cores Wolff, E.W. Boutron, C. 2000 http://nora.nerc.ac.uk/id/eprint/502794/ unknown EDP Sciences Wolff, E.W. 2000 History of the atmosphere from ice cores. In: Boutron, C., (ed.) From weather forecasting to exploring the solar system. European Research Course on Atmospheres, Grenoble, France. Les Ulis, France, EDP Sciences, 142-177. (ERCA, 4). Publication - Book Section NonPeerReviewed 2000 ftnerc 2023-02-04T19:37:29Z Ice cores are an excellent way of finding out how the atmosphere has changed because climate signals and many forcing factors for climate are present in the same core. Their main disadvantage is that they are only available in the polar regions and at a few unusual sites elsewhere. Cores range from short ones designed to understand seasonal deposition up to the 6.6 km deep/400 kyr record from Vostok, Antarctica. Signals exist in the water isotopes, in the soluble and insoluble impurities, and in the trace gases trapped in air bubbles. On short timescales, ice cores are the only means by which we know how greenhouse gas concentrations have altered in the last few centuries. On long timescales, ice cores have shown how temperature and greenhouse gases track each other through climatic cycles. They have also been responsible for revealing the very rapid switches in climate (Dansgaard-Oeschger events) that occurred during the last glacial period. Book Part Antarc* Antarctica Dansgaard-Oeschger events Natural Environment Research Council: NERC Open Research Archive |
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Natural Environment Research Council: NERC Open Research Archive |
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Ice cores are an excellent way of finding out how the atmosphere has changed because climate signals and many forcing factors for climate are present in the same core. Their main disadvantage is that they are only available in the polar regions and at a few unusual sites elsewhere. Cores range from short ones designed to understand seasonal deposition up to the 6.6 km deep/400 kyr record from Vostok, Antarctica. Signals exist in the water isotopes, in the soluble and insoluble impurities, and in the trace gases trapped in air bubbles. On short timescales, ice cores are the only means by which we know how greenhouse gas concentrations have altered in the last few centuries. On long timescales, ice cores have shown how temperature and greenhouse gases track each other through climatic cycles. They have also been responsible for revealing the very rapid switches in climate (Dansgaard-Oeschger events) that occurred during the last glacial period. |
author2 |
Boutron, C. |
format |
Book Part |
author |
Wolff, E.W. |
spellingShingle |
Wolff, E.W. History of the atmosphere from ice cores |
author_facet |
Wolff, E.W. |
author_sort |
Wolff, E.W. |
title |
History of the atmosphere from ice cores |
title_short |
History of the atmosphere from ice cores |
title_full |
History of the atmosphere from ice cores |
title_fullStr |
History of the atmosphere from ice cores |
title_full_unstemmed |
History of the atmosphere from ice cores |
title_sort |
history of the atmosphere from ice cores |
publisher |
EDP Sciences |
publishDate |
2000 |
url |
http://nora.nerc.ac.uk/id/eprint/502794/ |
genre |
Antarc* Antarctica Dansgaard-Oeschger events |
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Antarc* Antarctica Dansgaard-Oeschger events |
op_relation |
Wolff, E.W. 2000 History of the atmosphere from ice cores. In: Boutron, C., (ed.) From weather forecasting to exploring the solar system. European Research Course on Atmospheres, Grenoble, France. Les Ulis, France, EDP Sciences, 142-177. (ERCA, 4). |
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1766248667577057280 |