Reference Terms
from Wikipedia, the free encyclopedia

El Niño-Southern Oscillation

El Niño-Southern Oscillation (ENSO) is a global coupled ocean-atmosphere phenomenon.

The Pacific ocean signatures, El Niño and La Niña (also written in English as El Nino and La Nina) are major temperature fluctuations in surface waters of the tropical Eastern Pacific Ocean.

The names, from the Spanish for "the little boy" and "the little girl", refer to the Christ child, because the phenomenon is usually noticed around Christmas time in the Pacific Ocean off the west coast of South America.

Their effect on climate in the southern hemisphere is profound.

These effects were first described in 1923 by Sir Gilbert Thomas Walker from whom the Walker circulation, an important aspect of the Pacific ENSO phenomenon, takes its name.

The atmospheric signature, the Southern Oscillation (SO) reflects the monthly or seasonal fluctuations in the air pressure difference between Tahiti and Darwin.

El Nino affects Australia by drought.

Note:   The above text is excerpted from the Wikipedia article "El Niño-Southern Oscillation", which has been released under the GNU Free Documentation License.
Related Stories

Earth & Climate News
May 22, 2017

Latest Headlines
updated 12:56 pm ET