Forecast Forum

The canonical correlation analysis (CCA) forecast of SST in the central Pacific (Barnett et al. 1988, Science, 241, 192‑196; Barnston and Ropelewski 1992, J. Climate, 5, 1316‑1345), is shown in Figs. F1 and F2. This forecast is produced routinely by the Prediction Branch of the Climate Prediction Center. The predictions from the National Centers for Environmental Prediction (NCEP) Coupled Forecast System Model (CFSv2) are presented in Figs. F3 and F4a, F4b. Predictions from the Markov model (Xue, et al. 2000: J. Climate, 13, 849‑871) are shown in Figs. F5 and F6. Predictions from the latest version of the LDEO model (Chen et al. 2000: Geophys. Res. Let., 27, 2585‑2587) are shown in Figs. F7 and F8. Predictions from the ENSO‑CLIPER statistical model (Knaff and Landsea 1997, Wea. Forecasting, 12, 633‑652) are shown in Fig. F9. Nino 3.4 predictions are summarized in Fig. F10, provided by the Forecasting and Prediction Research Group of the IRI.

The CPC and the contributors to the Forecast Forum caution potential users of this predictive information that they can expect only modest skill.

 

Notice: As of 1 February, 2026, sea surface temperature anomalies are now based on relative sea surface temperature anomalies for ENSO monitoring and forecasting. See NWS Public Information Statement 26-05.

 

ENSO Alert System Status: El Nino Advisory

 

Outlook: El Nino is strengthening, with a greater than 90% chance of a very strong event during the Northern Hemisphere fall and winter 2026-27.

 

Discussion:

 

El Nino strengthened over the past month, with sea surface temperature anomalies exceeding +2.0C in the eastern equatorial Pacific (Fig. T18a). The July Nino index values were +1.4C in Nino-3.4, +1.7C in Nino-3, and +2.9C in Nino-1+2 (https://www.cpc.ncep.noaa.gov/data/indices/rel_mthsst9120.txt). The equatorial subsurface temperature index (average from 180-100W) increased during July, reflecting a deeper-than-average thermocline (Fig. T17). Subsurface temperature anomalies were significant, reaching +10.0C at depth. Low-level westerly wind anomalies and upper-level easterly wind anomalies extended from the western to east-central equatorial Pacific (Figs. T20 & T21). Convection and rainfall were enhanced from the central to eastern Pacific and were suppressed over Indonesia (Fig. T25). The traditional and equatorial Southern Oscillation indices were significantly negative, with values near 2 standard deviations during July (Figs. T1 & T2). Collectively, the coupled ocean-atmosphere system reflected a strengthening El Nino.

The CPC Official ENSO outlook, which synthesizes multiple models from North America and abroad, indicates El Nino will continue to strengthen through the end of the year (Figs. 6-8). During the October-December 2026 season, there is a 69% chance of a historic event that would exceed the strength of previous El Nino events dating back to 1950 (+2.5C or more for a 3-month RONI value). With an event of this magnitude, the chances of experiencing impacts consistent with El Nino are larger, but they are not guaranteed (see CPC outlooks for probabilities of seasonal anomalies).  In summary, El Nino is strengthening, with a greater than 90% chance of a very strong event during the Northern Hemisphere fall and winter 2026-27.

Weekly updates of oceanic and atmospheric conditions are available on the Climate Prediction Center homepage (El Nino/La Nina Current Conditions and Expert Discussions).