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Global winds and currents

Review your understanding of global winds and currents in this free article aligned to NGSS standards.

Key points:

  • A current is the steady flow of a fluid (such as air or water) within a larger body of that fluid.
  • Prevailing winds are air currents that blow mainly in one direction. The global pattern of prevailing winds is caused by the uneven heating of Earth’s surface.
  • As prevailing winds blow across the ocean, they create surface currents in the water. Both prevailing winds and surface currents appear to curve due to Earth’s rotation. This is known as the Coriolis effect.
  • Surface currents connect to form large, rotating systems called gyres. Gyres circulate heat around Earth by moving warm water from the equator to the poles.
  • The ocean also contains deep currents that are driven by differences in density. Denser water, which is colder and saltier, sinks into the ocean. Less dense water, which is warmer and less salty, rises.
  • These vertical currents are connected by horizontal currents at the surface and in the deep ocean. Together, this system of currents is called the overturning circulation.
Bent trees on a rocky plateau.
Trees can be permanently bent by strong prevailing winds. Image credit: “Wind-formed trees" by Mike Green, CC BY-SA 2.0.

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