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Cap in 1–5 years. As a result, the transport in the Deep Western Boundary Current is mostly correlated with convection in

Bibliographic Details
Main Authors: Introductionjulie Deshayesa, Claude Frankignoula, Helge Drangeb
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
North Atlantic subpolar gyre circulation
Labrador Sea Water
Convection
Deep water spreading
Deep Western Boundary Current
Interannual variability
Labrador Sea
North Atlantic
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.513.4560
http://folk.uib.no/ngfhd/Papers/deshayes_etal_2007.pdf
Description
Summary:Cap in 1–5 years. As a result, the transport in the Deep Western Boundary Current is mostly correlated with convection in

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