What is El nino explain its significant
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El Niño is the warm phase of the El Niño Southern Oscillation (commonly called ENSO) and is associated with a band of warm ocean water that develops in the central and east-central equatorial Pacific (between approximately the International Date Line and 120°W), including off the Pacific coast of South America. El Niño Southern Oscillation refers to the cycle of warm and cold temperatures, as measured by sea surface temperature, SST, of the tropical central and eastern Pacific Ocean. El Niño is accompanied by high air pressure in the western Pacific and low air pressure in the eastern Pacific. The cool phase of ENSO is called "La Nina" with SST in the eastern Pacific below average and air pressures high in the eastern and low in western Pacific. The ENSO cycle, both El Niño and La Niña, cause global changes of both temperatures and rainfall.
An understanding of El Niño is important for two reasons: 1) it is a useful model for predicting both long and short term climate changes, 2) it impacts global economies and ecologies.
An understanding of El Niño is important for two reasons: 1) it is a useful model for predicting both long and short term climate changes, 2) it impacts global economies and ecologies.
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El-Nino is a warm ocean current which sometimes appears off the coast of Peru in South America during the month of December. It increases the surface temperature of the sea and affects the movement of monsoon winds in the Indian Ocean and causes weak drought-like situation in the Indian sub-continent.
Explanation:
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