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El Nino Weather Phenomenon Definition

The Best 11 El Nino Weather Phenomenon Definition - In a nutshell, El Nio is a weather pattern that occurs in the Pacific Ocean. Unusual winds cause warm surface water from the equator to move east, toward Central and South America, during this time. El Nio can bring more rain to South and Central America, as well as the United States. In Spanish, El Nio means "Little Boy" or "Christ Child." In the 1600s, South American fishermen first noticed periods of unusually warm water in the Pacific Ocean. El Nio de Navidad was the full name they used because El Nio typically peaks in December. El Nio can have a significant impact on our weather.

El Nio (Spanish for "Christ Child") refers to an increase in ocean surface temperature (or above-average sea surface temperatures) in the central and eastern tropical Pacific Ocean. El Nio is defined as an irregularly recurring flow of unusually warm surface waters from the Pacific Ocean toward and along South America's western coast, preventing upwelling of nutrient-rich cold deep water and disrupting typical regional and global weather patterns. compare the nia Did you know that?

The El Nio-Southern Oscillation (ENSO) is a recurring climate pattern characterized by changes in the temperature of waters in the central and eastern tropical Pacific Ocean, as well as patterns of sea level pressure, lower- and upper-level temperatures. El Nio is a weather phenomenon that occurs when surface waters in the Pacific Ocean and near the Equator become unusually warm. Learn what El Nio is and how it works.

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