El Nino Watch
How much warmer than normal the top 300 m of the equatorial Pacific is: the fuel tank of El Nino.
Indices
A monthly NOAA CPC index: the average temperature anomaly of the upper 300 m of the equatorial Pacific, for three boxes (130E-80W, 160E-80W, 180W-100W), against the 1981-2010 average. Series heat_content_130e_80w_anom, heat_content_160e_80w_anom, heat_content_180w_100w_anom (degC).
Limits. Monthly, published early in the following month. It is an average over large boxes and does not show where exactly the warm water is.
Above 0 = more heat stored below the surface than normal. Values above about +1 C in the east (180W-100W) keep El Nino going; a fall back toward 0 or below usually announces the end of the event a few months later. August 2026: +3.2 C in the eastern box, a very high value.
The surface (Nino 3.4) follows the sub-surface with a lag of 1-3 months, so this is an early signal of how long and how strong the El Nino will stay, and so how long Samui should expect El Nino-type dry conditions.