BUSCO RECOMENDACIONES ANTE EL FENOMENO DE EL NIÑO XFA EN INGLES Y ESPAÑOL GRACIAS
mielesmiguel
The El Niño - Southern Oscillation (ENSO) is a recurring weather pattern that involves changes in water temperatures in the central and eastern tropical Pacific. In periods ranging from three to seven years, the surface waters of a large swath of tropical Pacific Ocean, are heated or cooled between 1 ° C and 3 ° C, compared to normal. This oscillating warming and cooling pattern is known as the cycle ENSO (or ENSO in English), directly affecting the distribution of rainfall in the tropics and can have a strong influence on climate in other parts of the world. El Niño and La Niña are the extreme phases of ENSO cycle; between these two phases is a third phase called Neutral. The name El Niño (referring to the baby Jesus) was given by Peruvian fishermen to a warm current that appears every year around Christmas. What we now call El Niño it seemed like a stronger event itself, and the term was changed to refer only to irregularly strong facts. It was not until the 1960s that it was noted that this was not a Peruvian local phenomenon, and is associated with changes across the tropical Pacific and beyond. The warm phase of El Niño usually lasts about 8-10 months. The entire ENSO cycle usually lasts between 3 and 7 years, and often includes a cold phase (La Niña) that can be equally strong, and some years are not abnormally cold or warm. However, the cycle is not a regular oscillation as the seasons change, can be highly variable in both intensity and duration. At present, still not fully understood what causes these changes in the ENSO cycle
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