Why Does the Deep Western Boundary Current “Leak” around Flemish Cap?
نویسندگان
چکیده
منابع مشابه
Attribution of Deep Western Boundary Current variability at 26.51N
Observed variations in the Deep Western Boundary Current (DWBC) at 26.51N, which carries the deep limb of the Atlantic Meridional Overturning Circulation (MOC), have been shown to greatly exceed in magnitude the variations of the overall basin-wide MOC, with strong variability at a range of time scales from weeks to multiple-months. Attribution of these strong DWBC variations will be crucial fo...
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[1] Transport fluctuations of the deep limb of the Meridional Overturning Circulation (MOC) near the western boundary are presented from a line of inverted echo sounders, bottom pressure sensors, and a deep current meter east of Abaco Island, Bahamas, at 26.5 N from September 2004 through September 2005. The mean southward flow between 800 dbar and 4800 dbar was 39 10m s , with a northward reci...
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ژورنال
عنوان ژورنال: Journal of Physical Oceanography
سال: 2020
ISSN: 0022-3670,1520-0485
DOI: 10.1175/jpo-d-19-0247.1