Effect of the Canary Islands in the blockage and mixing of the North Atlantic eastern water masses
We apply an inverse model to a hydrographic cruise that completely closes the Canary Islands to investigate their effect on the water masses transports. Most central waters are transported south between the eastern islands and the African coast, with 2.5 Sv out of a total of 3.5 Sv. Intermediate wat...
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Published in | Geophysical research letters Vol. 33; no. 4; pp. L04605 - n/a |
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Main Authors | , |
Format | Journal Article |
Language | English |
Published |
Washington, DC
American Geophysical Union
01.02.2006
Blackwell Publishing Ltd |
Subjects | |
Online Access | Get full text |
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Summary: | We apply an inverse model to a hydrographic cruise that completely closes the Canary Islands to investigate their effect on the water masses transports. Most central waters are transported south between the eastern islands and the African coast, with 2.5 Sv out of a total of 3.5 Sv. Intermediate waters are effectively blocked by the islands passages, with Mediterranean/Antarctic waters predominantly found north/south of the islands, and most deep waters loop around the archipelago plateau. A process model upholds the existence of intense two‐way exchange between central and intermediate waters along the eastern passage, with vertical velocities of order 10−5 m s−1. |
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Bibliography: | ArticleID:2005GL025048 istex:31C0D179415B925472B0A2D85FA362E03611B0D8 ark:/67375/WNG-8MB51VRR-8 ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 ObjectType-Article-2 ObjectType-Feature-1 |
ISSN: | 0094-8276 1944-8007 |
DOI: | 10.1029/2005GL025048 |