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El Nino, also called the "El Nino-Southern Oscillation" or ENSO, is a change in the ocean-atmosphere system in the eastern Pacific that occurs about every five to seven years. It contributes to significant weather changes around the world, according to the National Oceanic and Atmospheric Administration. Among these changes are increased rainfall across the southern region of the U.S. and in Peru and drought in the West Pacific, affecting Australia and its neighboring nations.
During El Nino, the winds at the equator blow from west to east in the Pacific. These winds travel along the surface of the ocean and bring warm surface water heated by the tropical sun to the western coasts of North and South America. Rainfall follows the warm water eastward, with associated flooding in Peru and drought in Indonesia and Australia. A key indicator of El Nino is usually warm temperature along and on both sides of the equator in the central and eastern Pacific.
The warming typically starts in the north during late spring or summer and builds to a peak at the end of the year. The events are usually over by the following summer. The changes in ocean temp
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“So What is an El Nino Anyway?(a non-technical description)” Downloaded from
meteora. Sea lion pups also died in masses on the coast of Chile. Fish in Chile are also being pushed from their normal limits and instead of spending more time awa!
y from their pups searching for food, mother sea lions are just abandoning their young. Similar conditions were seen all along the coast Peru and the ecosystem there slowly fell apart in a domino effect.
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