The Atlantic Meridional Overturning Circulation (AMOC) is a system of ocean currents that transports warm, salty water from the tropics to the northern Atlantic. As the water cools, it becomes denser and sinks, in a process ...
Earth Sciences
Jan 11, 2022
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The Pacific North Equatorial Countercurrent (NECC) is a major upper-ocean zonal flow of the wind-driven circulation in the tropical Pacific, flowing eastward across the Pacific Ocean basin between 2°N and 10°N. The NECC ...
Earth Sciences
Mar 6, 2019
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The mesoscale activities (or mesoscale structures) in the ocean possess immense energy. Such structures (including oceanic fronts and eddies) can induce mesoscale air-sea interaction (MASI) and then greatly impact oceanic ...
Earth Sciences
Feb 21, 2019
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