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Sub-tropical western boundary currents are warm, deep, narrow, and fast-flowing currents that form on the west side of ocean basins due to western intensification. They carry warm water from the tropics poleward. Examples include the Gulf Stream, the Agulhas Current, and the Kuroshio Current. Low-latitude western boundary currents are similar ...
Low-latitude western boundary currents (LLWBC) are western boundary currents located between the subtropical gyres, within 20° of the equator. They are important for closing the tropical circulation driven by the equatorial zonal flow, [ 1 ] and facilitate inter-ocean transport between the subtropical gyres.
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A slope of one part in one million in sea surface height, for example, will result in a current of 10 cm/s at mid-latitudes. The fact that the Coriolis effect is largest at the poles and weak at the equator results in sharp, relatively steady western boundary currents which are absent on eastern boundaries. Also see secondary circulation effects.
In general, strong currents called western boundary currents form at the eastern boundary of continents. These strong currents can transport water masses over a large distance, bringing them in contact with water masses that have very different properties. These differences in properties together with factors such as speed cause very strong ...
The current reaches its maximum transport near the Agulhas Bank where it ranges between 95 and 136 Sv. [4] The core of the current is defined as where the surface velocities reach 100 cm/s (39 in/s), which gives the core an average width of 34 km (21 mi). The mean peak speed is 136 cm/s (54 in/s), but the current can reach 245 cm/s (96 in/s).
The Mindanao Current is a low-latitude western boundary current located in the North Pacific and formed at the Philippine Sea by the bifurcation of the NEC. The jet transports approximately 13 − 39 {\displaystyle 13-39} Sv (where 1 {\displaystyle 1} S v = 10 6 m 3 s − 1 {\displaystyle Sv=10^{6}m^{3}s^{-1}} ) to the equator. [ 3 ]
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