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• W2180231387 startingPage "1440" @default.
• W2180231387 abstract "A synthesis of WOCE (and other) hydrographic data shows that the deep western boundary current of Antarctic Bottom Water has a double-core structure, and that it is differentially modified during its northward transit through the Brazil Basin. At 25°S, it descends about 200 m while continuing equatorward as a paired, double-core current over the relatively broad, sloping topography of the western region. The downslope core is faster, 4–6 cm s−1 versus 3 cm s−1, and is coincident with the high-density core. Equatorward of 19°S the cores begin to diverge and by 15°S, the velocity cores have separated and the high-speed pattern has inverted. Between 13° and 11°S the colder, slower-flowing branch (around 3 cm s−1) deepens by 350 m, with a noticeable decrease in the vertical stratification of overlying water characteristics. Subsequently, it continues to the equator toward the Romanche–Chain Fracture Zones. The warmer, faster-flowing branch (around 8 cm s−1) proceeds to the equator along the continental slope, eventually becoming the flow entering the equatorial channel." @default.
• W2180231387 created "2016-06-24" @default.
• W2180231387 creator A5014587166 @default.
• W2180231387 creator A5061321460 @default.
• W2180231387 date "2001-06-01" @default.
• W2180231387 modified "2023-10-16" @default.
• W2180231387 title "Evolution of the Deep Western Boundary Current of Antarctic Bottom Water in the Brazil Basin" @default.
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• W2180231387 doi "https://doi.org/10.1175/1520-0485(2001)031<1440:eotdwb>2.0.co;2" @default.
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