The 1950 - 1995 climatological mean
temperature along the equator at the 500mb level.
Not exact matches
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.
In the tropical Pacific, the distance from Indonesia to South America and the way tropical winds push warm water west combine to allow special waves to travel
along the
equator and are amplified by the atmospheric wind response to produce large fluctuations in
temperatures (up to 3 degrees Celsius) in the Eastern Pacific that last for months.
The attached figure shows the tropospheric
temperature trends versus the surface
temperature trends in units of K per decade for 1979 — 2004: the tropospheric
temperature trends are astonishingly uniform
along the
equator with a variation of about a factor of 5 smaller than that in the surface
temperature trends.
El Ni o an irregular variation of ocean current that, from January to February, flows off the west coast of South America, carrying warm, low - salinity, nutrient - poor water to the south; does not usually extend farther than a few degrees south of the
Equator, but occasionally it does penetrate beyond 12 S, displacing the relatively cold Peruvian current; usually short - lived effects, but sometimes last more than a year, raising sea - surface
temperatures along the coast of Peru and in the equatorial eastern Pacific Ocean, having disastrous effects on marine life and fishing
At irregular intervals (roughly every 3 - 6 years), the sea surface
temperatures in the Pacific Ocean
along the
equator become warmer or cooler than normal.
Farther from the
equator, Earth's rotation combines with
temperature contrasts between the tropics and polar regions to create midlatitude westerlies,
along with cyclones and anticyclones, that move heat from the subtropics to higher latitudes.
In the tropical Pacific, the distance from Indonesia to South America and the way tropical winds push warm water west combine to allow special waves to travel
along the
equator and are amplified by the atmospheric wind response to produce large fluctuations in
temperatures (up to 3 degrees Celsius) in the Eastern Pacific that last for months.
It also creates warm sea surface
temperature anomalies
along the
equator from the international dateline in the Pacific to the coast of South America.