 Atlantic meridional overturning circulation

The Atlantic Meridional Overturning Circulation (AMOC) is a large system of ocean currents in the Atlantic Ocean that plays a crucial role in regulating climate, particularly in the North Atlantic region. It involves the movement of warm, salty water from the tropics towards the North Atlantic, where it cools, becomes denser, and sinks to the ocean floor. This deep water then travels back southward, completing a global conveyor-belt-like circulation pattern.