El Niño is a climate phenomenon affecting global weather patterns, influenced by global warming and altering climate conditions worldwide.
El Niño is a short-term climate phenomenon characterized by warm water moving to the eastern Pacific Ocean from the western Pacific, disrupting the normal ocean-atmosphere system and impacting global weather patterns. This condition leads to varying impacts worldwide, with some regions experiencing heavy rainfall while others face drought conditions.
Scientists have reported that global warming may intensify the effects of El Niño events, causing changes in wind patterns and dry conditions in specific regions. For example, during El Niño years, some areas may receive more rainfall than usual while others may face abnormally dry conditions.
El Niño events alter atmospheric and oceanic circulation, leading to global climate pattern changes such as increased rainfall in certain regions like the west coast of North and South America, Southern U.S., and Western Europe, and drought in other parts of the world.
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