Oceanic Conveyor Belt

The oceanic conveyor belt, also known as the thermohaline circulation, is a global system of deep-ocean currents driven by differences in water temperature and salinity. Cold, dense water sinks in polar regions and flows along the ocean floor toward the equator, while warmer, less dense water rises and moves toward the poles. This continuous circulation helps regulate Earth's climate by redistributing heat, supporting marine life, and maintaining the Earth's energy balance. It's a vital component of the planet's climate system, connecting all the world's oceans in a large, ever-moving conveyor of water.