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ENSO (El Niño Southern Oscillation)

ENSO (El Niño Southern Oscillation):

The recent La Niña event in the tropical Pacific Ocean has officially ended, with the climate system now transitioning to ENSO-neutral conditions as confirmed by the National Oceanic and Atmospheric Administration (NOAA).

  • ENSO (El Niño Southern Oscillation): ENSO is a significant climate phenomenon that involves changes in sea-surface temperatures (SST) in the central and eastern tropical Pacific Ocean.
  • It affects various global weather patterns, including wind behavior, atmospheric pressure, and rainfall distribution.
  • El Niño: Warmer-than-usual sea surface temperatures, associated with unusual global warming patterns.
  • La Niña: Cooler-than-usual sea surface temperatures, often linked with colder atmospheric patterns and stronger trade winds.
  • ENSO-Neutral: Neither El Niño nor La Niña dominates the climate system, making forecasts less certain, but often acting as a transitional phase between the two extreme conditions.
  • ENSO-Neutral Phase is typically seen as a transition period between El Niño and La Niña.
  • In March 2025, NOAA scientists observed that SST anomalies in the Niño-3.4 region had reached -0.01°C, much warmer than the La Niña threshold of -0.5°C.
  • The cool waters that had characterized La Niña in previous months have now faded.