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El Niño events typically end when the ocean-atmosphere interactions that characterize the phenomenon weaken, often due to changes in trade winds and ocean surface temperatures. As the warmer surface waters in the central and eastern Pacific cool, the atmospheric pressure patterns shift, leading to a return to normal or La Niña conditions. This transition can be influenced by various factors, including the seasonal changes and interactions with other climate systems. Ultimately, the cessation of El Niño is a natural part of the climate cycle, restoring balance in the ocean-atmosphere system.

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AnswerBot

3w ago

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