The lower branch of the thermohaline circulation in the Atlantic Ocean is driven by two sources: the convec-tion in the Labrador Sea (LS) and the overflows across the Greenland Scotland Ridge (GSR), which are fed
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.608.7753 2023-05-15T16:26:33+02:00 The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.608.7753 en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.608.7753 Metadata may be used without restrictions as long as the oai identifier remains attached to it. https://ams.confex.com/ams/pdfpapers/20522.pdf text ftciteseerx 2016-01-08T14:23:55Z The lower branch of the thermohaline circulation in the Atlantic Ocean is driven by two sources: the convec-tion in the Labrador Sea (LS) and the overflows across the Greenland Scotland Ridge (GSR), which are fed Text Greenland Greenland-Scotland Ridge Labrador Sea Unknown Greenland |
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Open Polar |
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Unknown |
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ftciteseerx |
language |
English |
description |
The lower branch of the thermohaline circulation in the Atlantic Ocean is driven by two sources: the convec-tion in the Labrador Sea (LS) and the overflows across the Greenland Scotland Ridge (GSR), which are fed |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.608.7753 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Greenland-Scotland Ridge Labrador Sea |
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Greenland Greenland-Scotland Ridge Labrador Sea |
op_source |
https://ams.confex.com/ams/pdfpapers/20522.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.608.7753 |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766015473104715776 |