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

Bibliographic Details
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Greenland
Greenland-Scotland Ridge
Labrador Sea
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.608.7753
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spelling 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
institution Open Polar
collection Unknown
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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
author2 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
genre_facet 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
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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