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 (CFS03) 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 using linear inverse modeling (Penland and Magorian 1993: J.
Climate, 6, 1067‑1076) are shown in Figs. F9 and F10. Predictions from the Scripps / Max Planck
Institute (MPI) hybrid coupled model (Barnett et al. 1993: J. Climate, 6,
1545‑1566) are shown in Fig. F11.
Predictions from the ENSO‑CLIPER statistical model (Knaff and Landsea 1997, Wea.
Forecasting, 12, 633‑652) are shown in Fig. F12. Niño 3.4 predictions are summarized in Fig.
F13, 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 Niño Advisory
Outlook:
A transition to
ENSO-neutral is likely during late Northern Hemisphere spring or early summer
2016, with close to a 50% chance for La Niña conditions to develop by the fall.
Discussion:
Sea surface temperature (SST) anomalies decreased across most of the
central and eastern equatorial Pacific Ocean during February (Fig. T18). The monthly Niño-3.4 and Niño-3 weekly values
were near 2°C, while the Niño-4 and Niño-1+2 indices were 1.5°C and 0.7°C
respectively (Table T2). The subsurface
temperature anomalies in the central and eastern Pacific decreased
substantially in association with the eastward shift of below-average
temperatures at depth (Fig. T17). Low-level westerly wind anomalies and upper-level
easterly wind anomalies continued, but were weaker relative to January (Figs.
T20, T21). The traditional and equatorial Southern Oscillation
Index (SOI) remained strongly negative (Table T1 & Fig. T2). In addition, convection
was much enhanced over the central and east-central tropical Pacific and
suppressed over parts of Indonesia and northern Australia (Fig. T25). Collectively, these anomalies reflect the
continuation of a strong El Niño.
All
models indicate that El Niño will weaken, with a transition to ENSO-neutral
likely during the late spring or early summer 2016 (Figs. F1-F13).
Thereafter, the chance of La Niña conditions increases into the fall. While there is both
model and physical support for La Niña following a strong El Niño,
considerable uncertainty remains. A transition to
ENSO-neutral is likely during late Northern Hemisphere spring or early summer
2016, with close to a 50% chance for La Niña
conditions to develop by the fall.
Weekly
updates of oceanic and atmospheric conditions are available on the Climate
Prediction Center homepage (El
Niño/La Niña Current Conditions and Expert Discussions).