El Nino (redirected from El Niño)

El Niño  (l nny) A warming of the surface water of the eastern and central Pacific Ocean, occurring every 4 to 12 years and causing unusual global weather patterns. An El Niño is said to occur when the trade winds that usually push warm surface water westward weaken, allowing the warm water to pool as far eastward as the western coast of South America. When this happens, the typical pattern of coastal upwelling that carries nutrients from the cold depths to the ocean surface is disrupted, and fish and plankton die off in large numbers. El Niño warming is associated with the atmospheric phenomenon known as the southern oscillation, and their combined effect brings heavy rain to western South American and drought to eastern Australia and Indonesia. El Niño also affects the weather in the United States, but not as predictably. Compare La Nina.

El Niño top: normal water temperatures, with warm water concentrated in the western tropical Pacific; bottom: El Niño conditions, with warm water extending from the western tropical Pacific to the eastern Pacific

Thesaurus

Noun	1.	El Nino - (oceanography) a warm ocean current that flows along the equator from the date line and south off the coast of Ecuador at Christmas time oceanography, oceanology - the branch of science dealing with physical and biological aspects of the oceans ocean current - the steady flow of surface ocean water in a prevailing direction El Nino southern oscillation - a more intense El Nino that occurs every few years when the welling up of cold nutrient-rich water does not occur; kills plankton and fish and affects weather patterns
	2.	El Nino - the Christ child Spanish - the Romance language spoken in most of Spain and the countries colonized by Spain