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Global climate phenomenon
El Niño–Southern Oscillation (ENSO) is a global climate phenomenon that emerges from variation in winds and sea surface temperatures over the tropical Pacific Ocean. Those variations have an irregular pattern, but do have some appearance of cycles. The occurrence of ENSO is not easily predictable. It affects the climate of much of the tropics and subtropics, and has links (teleconnections) to higher-latitude regions of the world. The warming phase of the sea surface temperature is known as "El Niño" and the cooling phase as "La Niña".
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This year's El Niño will intensify before peaking in December and is nearly 100% certain to last until February 2027, the World Meteorological Organization said.
El Nino is forecasted to intensify and peak by December, lasting through February 2027. Sea surface temperatures are expected to reach unprecedented levels during this phenomenon, affecting global weather patterns. It could be one of the strongest El Ninos since at least 1950, according to the World Meteorological…
The El Niño phenomenon is intensifying and expected to peak in December, potentially becoming one of the strongest since 1950, with global impacts on temperatures, rainfall, and drought risks through early 2027.