Under normal conditions:
Easterly winds blow strongly into the western tropical
Pacific, forcing atmospheric convection west of the dateline and oceanic
upwelling in the eastern tropical Pacific.
Under El Nino conditions:
The easterly winds are weaker and the region of strong
atmospheric convection is located farther east. Oceanic upwelling
in the eastern tropical Pacific is much weaker.
Changes of wind at the sea surface reveal changes of climate
over a broad region of both the atmosphere and ocean.