Britannica AI Icon

wind-driven circulation

oceanography

Quick Summary

Wind-driven circulation is a primary type of ocean circulation, powered by the energy transferred from wind stress on the sea surface. This process creates large, circular current systems known as gyres that are most vigorous in the ocean's surface layer.1

The wind's force on the water creates an effect called Ekman transport, where the average water particle movement is about 90 degrees to the wind direction—to the right in the Northern Hemisphere and to the left in the Southern Hemisphere. This transport leads to areas of water convergence and divergence, resulting in downwelling and upwelling of water masses. These movements are crucial for distributing heat and nutrients throughout the ocean.23

Summary created from Britannica articles using AI. AI can make mistakes, so verify using Britannica articles.

Ask Britannica AI about this topic

Britannica doesn't have a full article on this topic, so we've curated a list of our relevant coverage.