The first image, based on data from January 1997 when El Nio was still strengthening shows a sea level
rise along the Equator in the eastern Pacific Ocean of up to 34 centimeters with the red colors indicating an associated change in sea surface temperature of up to 5.4 degrees C.
Not exact matches
El Nino's mass of warm water puts a lid on the normal currents of cold, deep water that typically
rise to the surface
along the
equator and off the coast of Chile and Peru, said Stephanie Uz, ocean scientist at Goddard Space Flight Center in Greenbelt, Maryland.
When that warm water reaches the western Pacific it
rises and, in the main, tracks back
along the
equator in the upper atmosphere and loses its heat to space.
The primary effect of the two tropical Hadley cells (one for each hemisphere) is for the
rising hot air at the
equator to suck surface air from the higher latitudes (north and south)
along the surface towards the
equator, pump it vertically at the
equator, and at a suitable height push it polewards, one pole per cell, up where the jet planes fly.
The descended air then travels toward the
equator along the surface, replacing the air that
rose from the equatorial zone, closing the loop of the Hadley cell.