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: La Niña Advisory
Outlook:
Though La Niña is favored to continue, the odds for La Niña decrease into the late Northern Hemisphere summer
(58% chance in August-October 2022) before slightly increasing through the
Northern Hemisphere fall and early winter 2022 (61% chance).
Discussion:
Below-average
sea surface temperatures (SSTs) persisted during April across most of the
central and eastern equatorial Pacific Ocean (Fig. T18). Most Niño index values decreased, with the
latest monthly values ranging from -0.7C to -1.4C (Table T2), which are quite negative
for this time of year. Subsurface
temperatures anomalies (averaged between 180-100W and 0-300m depth) remained
negative, reflecting an extensive area of below-average temperatures from the
surface to ~100m depth across the central and eastern equatorial Pacific Ocean
(Fig. T17). For the monthly average, low-level easterly and
upper-level westerly wind anomalies dominated the equatorial Pacific (Figs. T20
& T21). Convection remained significantly suppressed
around the Date Line and was enhanced over the Philippines (Fig. T25). Overall, the coupled ocean-atmosphere system
reflected the continuation of La Niña.
The
most recent IRI/CPC plume average for the Niño-3.4 SST index forecasts borderline
La Niña conditions during the Northern Hemisphere summer, with increasing odds
for La Niña into the fall (Figs. F1-F12). Similar to last month, the forecaster
consensus predicts Niño-3.4 index values to weaken into the summer, but remaining
below the threshold of La Niña (Niño-3.4 values equal to or less than -0.5C). In the near-term, westerly wind anomalies are
predicted for mid-late May which supports the weakening of below-average
surface and subsurface oceanic temperatures in the coming months. However, much of the model guidance is also hinting
at a re-strengthening of La Niña conditions again in the fall and upcoming
winter. In summary, though La Niña is favored to continue, the odds for La Niña decrease into the late Northern Hemisphere summer
(58% chance in August-October 2022) before slightly increasing through the
Northern Hemisphere fall and early winter 2022 (61% 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).