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Hypotheses and inferences concerning the nature of abrupt climate change, exemplified by the Dansgaard–Oeschger (D–O) events, are reviewed. There is little concrete evidence that these events are more than a regional Greenland phenomenon. The partial coherence of ice core y 18 O and CH 4 is a possib...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.334.348 2023-05-15T16:00:04+02:00 www.elsevier.com/locate/yqres Carl Wunsch The Pennsylvania State University CiteSeerX Archives 2005 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.334.348 http://ocean.mit.edu/~cwunsch/papersonline/abrupt2006.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.334.348 http://ocean.mit.edu/~cwunsch/papersonline/abrupt2006.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://ocean.mit.edu/~cwunsch/papersonline/abrupt2006.pdf Abrupt climate change Dansgaard–Oeschger events Ocean circulation text 2005 ftciteseerx 2016-09-11T00:07:29Z Hypotheses and inferences concerning the nature of abrupt climate change, exemplified by the Dansgaard–Oeschger (D–O) events, are reviewed. There is little concrete evidence that these events are more than a regional Greenland phenomenon. The partial coherence of ice core y 18 O and CH 4 is a possible exception. Claims, however, of D–O presence in most remote locations cannot be distinguished from the hypothesis that many regions are just exhibiting temporal variability in climate proxies with approximately similar frequency content. Further suggestions that D–O events in Greenland are generated by shifts in the North Atlantic ocean circulation seem highly implausible, given the weak contribution of the high latitude ocean to the meridional flux of heat. A more likely scenario is that changes in the ocean circulation are a consequence of wind shifts. The disappearance of D–O events in the Holocene coincides with the disappearance also of the Laurentide and Fennoscandian ice sheets. It is thus suggested that D–O events are a consequence of interactions of the windfield with the continental ice sheets and that better understanding of the wind field in the glacial periods is the highest priority. Wind fields are capable of great volatility and very rapid global-scale teleconnections, and they are efficient generators of oceanic circulation changes and (more speculatively) of multiple states relative to great ice sheets. Connection of D–O events to the possibility of modern abrupt climate change rests on a very weak chain of assumptions. Text Dansgaard-Oeschger events Fennoscandian Greenland ice core North Atlantic Unknown Greenland |
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Abrupt climate change Dansgaard–Oeschger events Ocean circulation |
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Abrupt climate change Dansgaard–Oeschger events Ocean circulation Carl Wunsch www.elsevier.com/locate/yqres |
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Abrupt climate change Dansgaard–Oeschger events Ocean circulation |
description |
Hypotheses and inferences concerning the nature of abrupt climate change, exemplified by the Dansgaard–Oeschger (D–O) events, are reviewed. There is little concrete evidence that these events are more than a regional Greenland phenomenon. The partial coherence of ice core y 18 O and CH 4 is a possible exception. Claims, however, of D–O presence in most remote locations cannot be distinguished from the hypothesis that many regions are just exhibiting temporal variability in climate proxies with approximately similar frequency content. Further suggestions that D–O events in Greenland are generated by shifts in the North Atlantic ocean circulation seem highly implausible, given the weak contribution of the high latitude ocean to the meridional flux of heat. A more likely scenario is that changes in the ocean circulation are a consequence of wind shifts. The disappearance of D–O events in the Holocene coincides with the disappearance also of the Laurentide and Fennoscandian ice sheets. It is thus suggested that D–O events are a consequence of interactions of the windfield with the continental ice sheets and that better understanding of the wind field in the glacial periods is the highest priority. Wind fields are capable of great volatility and very rapid global-scale teleconnections, and they are efficient generators of oceanic circulation changes and (more speculatively) of multiple states relative to great ice sheets. Connection of D–O events to the possibility of modern abrupt climate change rests on a very weak chain of assumptions. |
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The Pennsylvania State University CiteSeerX Archives |
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Text |
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Carl Wunsch |
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Carl Wunsch |
author_sort |
Carl Wunsch |
title |
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title_full |
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publishDate |
2005 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.334.348 http://ocean.mit.edu/~cwunsch/papersonline/abrupt2006.pdf |
geographic |
Greenland |
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Greenland |
genre |
Dansgaard-Oeschger events Fennoscandian Greenland ice core North Atlantic |
genre_facet |
Dansgaard-Oeschger events Fennoscandian Greenland ice core North Atlantic |
op_source |
http://ocean.mit.edu/~cwunsch/papersonline/abrupt2006.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.334.348 http://ocean.mit.edu/~cwunsch/papersonline/abrupt2006.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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