lf, a decrease with Allerød cooling, and a recovery through the ttersrelationship with the millennial perturbations of NADW flux to the deep Southern Ocean. The data indicate that the baseline intensity of NADW reaching the Cape Basin is paced by Northern Hemisphere insolation and that North Atlanti...
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| Format: | Text |
| Language: | English |
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2004
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.548.7252 http://www.ldeo.columbia.edu/~peter/Resources/Seminar/readings/Piotrowski_etal_EPSL04.pdf |
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.548.7252 2023-05-15T17:13:49+02:00 The Pennsylvania State University CiteSeerX Archives 2004 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.548.7252 http://www.ldeo.columbia.edu/~peter/Resources/Seminar/readings/Piotrowski_etal_EPSL04.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.548.7252 http://www.ldeo.columbia.edu/~peter/Resources/Seminar/readings/Piotrowski_etal_EPSL04.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.ldeo.columbia.edu/~peter/Resources/Seminar/readings/Piotrowski_etal_EPSL04.pdf thermohaline circulation deep water deglacial neodymium Younger Dryas last glacial text 2004 ftciteseerx 2016-01-08T11:24:53Z lf, a decrease with Allerød cooling, and a recovery through the ttersrelationship with the millennial perturbations of NADW flux to the deep Southern Ocean. The data indicate that the baseline intensity of NADW reaching the Cape Basin is paced by Northern Hemisphere insolation and that North Atlantic sea ice coverage acts as a major amplifying link between the oceans and the atmosphere. Text NADW North Atlantic Sea ice Southern Ocean Unknown Southern Ocean |
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Open Polar |
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Unknown |
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ftciteseerx |
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English |
| topic |
thermohaline circulation deep water deglacial neodymium Younger Dryas last glacial |
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thermohaline circulation deep water deglacial neodymium Younger Dryas last glacial |
| topic_facet |
thermohaline circulation deep water deglacial neodymium Younger Dryas last glacial |
| description |
lf, a decrease with Allerød cooling, and a recovery through the ttersrelationship with the millennial perturbations of NADW flux to the deep Southern Ocean. The data indicate that the baseline intensity of NADW reaching the Cape Basin is paced by Northern Hemisphere insolation and that North Atlantic sea ice coverage acts as a major amplifying link between the oceans and the atmosphere. |
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The Pennsylvania State University CiteSeerX Archives |
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Text |
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2004 |
| url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.548.7252 http://www.ldeo.columbia.edu/~peter/Resources/Seminar/readings/Piotrowski_etal_EPSL04.pdf |
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Southern Ocean |
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Southern Ocean |
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NADW North Atlantic Sea ice Southern Ocean |
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NADW North Atlantic Sea ice Southern Ocean |
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http://www.ldeo.columbia.edu/~peter/Resources/Seminar/readings/Piotrowski_etal_EPSL04.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.548.7252 http://www.ldeo.columbia.edu/~peter/Resources/Seminar/readings/Piotrowski_etal_EPSL04.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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