Escribe texto en ingles sobre el fenomeno del niño
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The child is a climate phenomenon linked to the warming of the eastern equatorial Pacific, which manifests erratically Arthur Strahler cyclical speaks of cycles of three to eight years, one that is actually in the warm phase of the equatorial Pacific weather pattern called El Niño-Southern Oscillation (El Niño-Southern Oscillation, ENSO English), 2 where the cooling phase called La Niña. This phenomenon, in its most intense manifestations, causes havoc in the inter-tropical and equatorial zone due to heavy rains, affecting mainly the Pacific coastal region of South America. Günther D. Roth defines it as an occasional burst of warm surface water, located in the Pacific Ocean off the coast of Peru and Ecuador territories because of instabilities in atmospheric pressure located between the eastern and western sections of the nearby Pacific Ocean to the line of Ecuador. El Niño is the supposed cause of more than one anomaly climática.3 The name "El Niño" is due to the association of this phenomenon with the current call of the Child, anomaly known by fishermen from the port of Paita in northern Peru, who observed that the waters increased temperature during "the time the holidays "and shoals or fish shoals disappeared from the ocean surface, deducing that the abnormality was due to a stream of hot air from the Gulf of Guayaquil (Ecuador). The first official records of the phenomenon were reported by the Peruvian captain Camilo Carrillo in 1892, who noted the periodic existence of a warm ocean current off the coast of Peru, normally very cold water. There are other interesting developments related to the most intense El Niño years. Between 1789 and 1793, the British historian Richard Grove reports that several contemporary observers reported serious drought in Asia, Australia, Mexico and South Africa, so it is suspected that this phenomenon may have caused the famine that preceded the Revolution French. Between 1791 and 1793 in Mexico he lowered the level of Lake Pátzcuaro.4 The meteorologist Jacob Bjerknes postulated in 1969 that El Niño is normally associated with the Southern Oscillation, as a physical relationship between the phase of abnormally high pressure in the western Pacific, with the heating phase rare eastern Pacific, is present as which it is accompanied by a weakening of the easterly trade winds; so the low pressure in the western Pacific is linked to a cooling of the eastern Pacific (La Niña), with strengthening winds.
Günther D. Roth defines it as an occasional burst of warm surface water, located in the Pacific Ocean off the coast of Peru and Ecuador territories because of instabilities in atmospheric pressure located between the eastern and western sections of the nearby Pacific Ocean to the line of Ecuador. El Niño is the supposed cause of more than one anomaly climática.3
The name "El Niño" is due to the association of this phenomenon with the current call of the Child, anomaly known by fishermen from the port of Paita in northern Peru, who observed that the waters increased temperature during "the time the holidays "and shoals or fish shoals disappeared from the ocean surface, deducing that the abnormality was due to a stream of hot air from the Gulf of Guayaquil (Ecuador).
The first official records of the phenomenon were reported by the Peruvian captain Camilo Carrillo in 1892, who noted the periodic existence of a warm ocean current off the coast of Peru, normally very cold water. There are other interesting developments related to the most intense El Niño years. Between 1789 and 1793, the British historian Richard Grove reports that several contemporary observers reported serious drought in Asia, Australia, Mexico and South Africa, so it is suspected that this phenomenon may have caused the famine that preceded the Revolution French. Between 1791 and 1793 in Mexico he lowered the level of Lake Pátzcuaro.4
The meteorologist Jacob Bjerknes postulated in 1969 that El Niño is normally associated with the Southern Oscillation, as a physical relationship between the phase of abnormally high pressure in the western Pacific, with the heating phase rare eastern Pacific, is present as which it is accompanied by a weakening of the easterly trade winds; so the low pressure in the western Pacific is linked to a cooling of the eastern Pacific (La Niña), with strengthening winds.