Upwelling occurs in the equatorial waters of the ocean.

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Upwelling is a common phenomenon that occurs in the equatorial waters of the ocean. It is caused by the wind-driven motion of cold and nutrient-rich water from deeper ocean layers to the surface, supporting the growth of phytoplankton and providing an important source of food for marine organisms. Upwelling zones also play a crucial role in regulating global climate and oceanic carbon cycling.

Upwelling Occurs in the Equatorial Waters of the Ocean