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  1. 20 de dic. de 2016 · This nexus brief* explains the phenomenon of the El Niño–Southern Oscillation (ENSO) and details in particular the 2015/2016 El Niño event, which faded out in May 2016, but has impacts and effects on environmental and societal systems that will extend well into 2017.

  2. Because of El Niño. El Niño is a climate pattern that affects weather in many places, including the United States—and particularly the West Coast. During an El Niño year, there are more hurricanes and more severe rainstorms. One effect of these storms is landslides as large waves erode seaside cliffs. El Niño affects temperatures as well ...

  3. 8 Further reading. Toggle the table of contents. 2023–2024 El Niño event. 1 language. ... The 2023–2024 El Niño was regarded as the fourth-most powerful El Niño–Southern Oscillation ... In mid-January 2023, weather forecasts regarding the probable occurrence of the El Niño phenomenon in 2023 and 2024 were published in ...

  4. 18 de ene. de 2016 · They nicknamed the phenomenonEl Niño” (Spanish for little boy) in connection with the celebration of the Christian holiday marking the birth of Jesus. In the 1980s, when the opposite phase of El Niño was discovered (i.e., cooler-than-normal ocean temperatures), ...

  5. 30 de abr. de 2024 · ENSO is the oscillation between El Niño and La Niña conditions. This climate influence is related to: El Niño La Niña The Australian Monsoon. What is it? The term El Niño refers to the extensive warming of the central and eastern tropical Pacific Ocean which leads to a major shift in weather patterns across the Pacific.

  6. El Niño. El Niño is a natural climate phenomenon, in which surface waters of the central and eastern Pacific Ocean become unusually warm and cause changes in weather patterns around the world. On average, it re-occurs every 2 to 7 years and typically lasts 9-12 months. Since El Niño can often be predicted months in advance, has a slow onset ...

  7. El Niño is generally a recursive phenomenon of 2–7 years having large spatial scale of influence expanding from ISM region to the west coast of South America but it has no definite time period. The time span of El Niño depends upon its length of its decay phase (e.g., Chowdary et al., 2017 ).

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