El Nino Watch

ENSO (El Nino-Southern Oscillation)

A natural see-saw of ocean temperature and winds in the tropical Pacific. It has three phases: El Nino (warm), La Nina (cool) and neutral.

El Nino basics

ENSO is the name scientists use for one big climate pattern with two halves:

  • El Nino / La Nina: the ocean half. The surface of the central and eastern tropical Pacific becomes warmer (El Nino) or cooler (La Nina) than normal.
  • Southern Oscillation: the atmosphere half. Air pressure swings between the western Pacific (around Darwin, Australia) and the central Pacific (Tahiti). When the pressure changes, the winds change too.

The two halves push on each other. Warmer water weakens the winds; weaker winds let even more warm water spread east. That feedback is why an El Nino can grow for months and then last most of a year.

ENSO is natural. It existed long before modern climate change. Episodes typically come back every 3 to 5 years, but the gap has varied from 2 to 7 years in the record.

How to read it

The phase is read from the sea surface temperature in the Nino 3.4 region: +0.5 °C or more above normal for several months = El Nino, -0.5 °C or less = La Nina, in between = neutral. The atmosphere must also respond (winds, pressure, rain) for an official declaration.

Why it matters for Koh Samui

ENSO is the single biggest reason why one year in Thailand is drier or wetter than the next. It does not decide tomorrow's weather on Koh Samui, but it tilts the odds for whole seasons.

Sources

Related

ENSO status now

ONI (NOAA CPC)
+1.80 °C, JJA 2026 (previous +1.39 °C)
RONI (NOAA CPC)
+1.36 °C, JJA 2026
Nino 3.4 weekly (NOAA CPC / OISST)
+3.0 °C anomaly, week of 16 Sep 2026 (SST 29.6 °C)