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Mozambique Current, relatively warm surface current of the western Indian Ocean.
Monsoon Current, also called Monsoon Drift, surface current of the northern Indian Ocean.
A surface current flows eastward through the centre of the channel, except when affected by easterly winds.
A general surface current (8 miles a day) flows toward the east and is strongest along the south shore.
Usually a surface current of warm water flows northward in the Atlantic toward Greenland and Europe, then cools and sinks, returning south in the deep ocean.
Starting from using sea surface current only, we gradually added forcing terms representing the actions of atmospheric drag and wind waves on buoyant debris.
There is a rapid surface current from the Sea of Marmara to the Aegean and a compensatory undercurrent returning more saline water.
a, b, Climatological surface current direction (in arrows) and speed (shaded, m s−1) obtained from the control simulation with HadGEM3-GC2 and the satellite product OSCAR.
To reduce the maximum surface current, we increased the spacing between resonators.
Additionally, the maximum surface current is approximately 17% less than that of the conventional filter.
The stream function associated with the shield surface current is also determined.
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