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. Niño 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.
ENSO Alert System Status: El Nino Advisory/ La Nina
Watch
Outlook: A transition from
El Nino to ENSO-neutral is likely in the next month. La Nina may develop in June-August (49%
chance) or July-September (69% chance).
Discussion:
During April 2024, below-average equatorial sea
surface temperatures (SSTs) emerged in small regions of the eastern Pacific
Ocean. However, above-average SSTs prevailed across the rest of the equatorial
Pacific (Fig. T18). The monthly Niño index values
remained between +0.6C and +0.8C in all regions, except for Nino-1+2 which was
+0.1C (Table T2). Below-average
subsurface temperatures held steady during the month, with negative anomalies
extending from the Date Line to the eastern Pacific Ocean (Fig. T17). Low-level wind
anomalies were easterly over the western equatorial Pacific, while upper-level
winds were near average (Figs. T20 & T21). Convection was near average overall across
the equatorial Pacific Ocean and Indonesia (Fig. T25). Collectively, the
coupled ocean-atmosphere system reflected the continued weakening of El Nino
and transition toward ENSO-neutral.
The
most recent IRI plume favors an imminent transition to ENSO-neutral, with La
Nina developing during July-September 2024 and then persisting through the
Northern Hemisphere winter (Figs. F1-F12). The forecast team continues to favor the
dynamical model guidance, which suggests La Nina could form as early as
June-August 2024, with higher confidence of La Nina during the following
seasons. La Nina generally tends to follow strong El Nino events, which also
provides added confidence in the model guidance favoring La Nina. In summary, a
transition from El Nino to ENSO-neutral is likely in the next month. La Nina may develop in June-August (49%
chance) or July-September (69% chance).
Weekly
updates of oceanic and atmospheric conditions are available on the Climate
Prediction Center homepage (El
Niño/La Niña Current Conditions and Expert Discussions).