Walker circulation

Pacific pressure oscillation

Walker circulation is a large-scale atmospheric pattern over the tropical Pacific Ocean, driven by differences in sea surface temperature and pressure between the western and eastern Pacific.

Air rises over the warm western Pacific, flows eastward at high altitude, descends over the cooler eastern Pacific, and returns westward along the surface.

Disruptions to this circulation are associated with El Niño and La Niña events.

Named for British meteorologist Gilbert Walker.

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Categories
Opposites
circulation phase

Walker circulationEl Niño

Periodic Pacific warming event

circulation scale/type

Walker circulationmonsoon

Seasonal tropical wind pattern

polar vortex · jet stream · sea breeze · land breeze

Family

circulation, Walker

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