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El Niño–Southern Oscillation - Wikipedia 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 semblance of cycles The occurrence of ENSO is not predictable
What is ENSO? - National Weather Service The El Niño-Southern Oscillation (ENSO) is a recurring climate pattern involving changes in the temperature of waters in the central and eastern tropical Pacific Ocean
El Niño Southern Oscillation (ENSO) | National Centers for . . . El Niño and the Southern Oscillation, also known as ENSO is a periodic fluctuation (i e , every 2–7 years) in sea surface temperature (El Niño) and the air pressure of the overlying atmosphere (Southern Oscillation) across the equatorial Pacific Ocean
IRI – International Research Institute for Climate and . . . The latest set of ENSO prediction models from mid-November 2025 is now available in the IRI ENSO prediction plume These are used to assess the probabilities of the three ENSO categories by using the average value of the NINO3 4 SST anomaly predictions from all models in the plume, equally weighted
Climate Prediction Center: ENSO Diagnostic Discussion ENSO Alert System Status: La Niña Advisory Synopsis: La Niña is favored to continue into the Northern Hemisphere winter, with a transition to ENSO-neutral most likely in January-March 2026 (61% chance)