The Deep Western Boundary Current at Cape Farewell: Results from a Moored Current Meter Array
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...
متن کاملVariability in Deep Western Boundary Current transports: Preliminary results from 26.5 N in the Atlantic
[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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Aminoglycosides are first-line antibiotics in treating infections of Gram-negative micro-organisms that are resistant to less toxic agents. They have potent concentrationdependent bactericidal activity, a post-antibiotic effect (PAE), relatively predictable pharmacokinetics and act synergistically with many other antibiotics. With susceptible organisms, clinical responses are rapid and understa...
متن کاملNeogene history of the Deep Western Boundary Current at Rekohu sediment drift, Southwest Paci¢c (ODP Site 1124)
ODP Site 1124, located 600 km east of the North Island of New Zealand, records post-middle Oligocene variations in the Pacific Deep Western Boundary Current (DWBC) and New Zealand’s climatic and tectonic evolution. Sediment parameters, such as terrigenous grain size, flux, magnetic fabric, and non-depositional episodes, are used to interpret DWBC intensity and Antarctic climate. Interpretations...
متن کاملThe Interaction of a Deep Western Boundary Current and the Wind-Driven Gyres as a Cause for Low-Frequency Variability
Recent modeling and observational studies have indicated that the interaction of the Gulf Stream and the deep western boundary current (DWBC) in the North Atlantic may induce low-frequency (decadal timescale) variability. To understand the origin of this low-frequency variability, a line of studies is continued here addressing the stability and variability of the wind-driven circulation using t...
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ژورنال
عنوان ژورنال: Journal of Physical Oceanography
سال: 2010
ISSN: 1520-0485,0022-3670
DOI: 10.1175/2009jpo4091.1