Oceanic Circulation

Oceanic circulation refers to the large-scale movement of seawater throughout the world's oceans, driven by factors like wind, water temperature, and salinity differences. It includes surface currents, like the Gulf Stream, which transport warm water, and deep currents, which carry colder water. This circulation is crucial for regulating the Earth’s climate, distributing heat, and supporting marine ecosystems. Essentially, it acts like a global conveyor belt, connecting different regions of the oceans and impacting weather patterns and marine life across the planet.