👉 The Atlantic Fluid, also known as the Atlantic Meridional Overturning Circulation (AMOC), is a crucial component of the global ocean circulation system. It refers to the large-scale movement of warm, salty surface water from the tropics towards the North Atlantic, where it cools and becomes denser. This dense water then sinks and flows southward along the ocean floor, eventually returning to the tropics after thousands of years. This process plays a vital role in regulating Earth's climate by redistributing heat and influencing weather patterns across the globe. The Atlantic Fluid is part of a larger system that includes other currents like the Gulf Stream, which transport warm water northward, affecting regional climates in Europe and North America.
atlantic fluid