ENSO Quick Look IRI ENSO Update / Prediction IRI Probabilistic ENSO Prediction Technical ENSO Update ENSO Prediction Plume Monthly Archive Technical ENSO Update20 October 2011
Current ConditionsAs of mid-October 2011, SST anomalies remain in in weak La Niña territory in the central and eastern equatorial Pacific. For September the SST anomaly in the NINO3.4 region was -0.74 C, indicative of weak La Niña conditions, and for the June-August season the anomaly was -0.55 C. Currently the IRI's definition of El Niño conditions rests on an index of SST anomalies, averaged over the NINO3.4 region (5S-5N; 170W-120W), exceeding the warmest 25%-ile of the historical distribution, and similarly for La Niña relative to the 25%-ile coldest conditions in the historical distribution. The NINO3.4 anomaly necessary to qualify as La Niña or El Niño conditions for the Oct-Nov-Dec and the Nov-Dec-Jan seasons are approximately (-0.75C, 0.75) and (-0.70, 0.75), respectively.Expected ConditionsThe most recent weekly SST anomaly in the NINO3.4 region is -0.8 C, indicating weak La Niña conditions in the tropical Pacific; this is about the same as the -0.74 C level observed in September. A moderate to strong La Niña episode ended during early May, followed by neutral ENSO conditions between May and early August, and a return to weak La Niña conditions beginning in early August. What is the outlook for the ENSO status going forward? The currently weak La Niña SSTs and increasingly below average subsurface temperatures across the equatorial Pacific imply a strong likelihood of maintaining at least weak La Niña conditions in the short term, with some chance for further strengthening, possibly into the moderate strength range, during the coming month or two.Presently, the models and observations taken together indicate
probabilities of approximately 78% for maintaining at least weak
La Niña conditions, 22% for returning to ENSO-neutral conditions,
and near 0% for developing El Niño conditions, during the Oct-Dec
2011 season in progress. Probabilities for La Niña stay at 70% or higher
through the Dec-Feb 2011/11 season. Probabilities for El Niño conditions remain below
10% through Feb-Apr 2012. La Niña conditions are the most likely scenario
during the remainder of 2011 and into early 2012, although a return to neutral
conditions during this time period also has a slight possibility. La Niña
probabilities decrease to 51% by Feb-Apr 2012 before returning to the climatological
value of 25% by the May-Jul season 2012. During the remainder of 2011, the probability
for neutral conditions is at roughly 25%.
The above assessment was made in part on the basis of an examination of the current predictions of ENSO prediction models as well as the observed conditions. For purposes of this discussion, El Niño SST conditions are defined as SSTs in the NINO3.4 region being in the warmest 25% of their climatological distribution for the 3-month period in question over the 1950-present timeframe. The corresponding cutoff in terms of degrees C of SST anomaly varies seasonally, being close to 0.40 degrees C in boreal late-spring to early-summer season and as high as 0.75 degrees C in late boreal autumn. La Niña conditions are defined as NINO3.4 region SSTs being in the coolest 25% of the climatological distribution. Neutral conditions occupy the remaining 50% of the distribution. These definitions were developed such that the most commonly accepted El Niño and La Niña episodes are reproduced. Even though La Niña conditions have already been observed
for a few months, a slight majority of the dynamical and statistical models
continue to forecast neutral ENSO conditions for the Oct-Dec season and for most
of the subsequent seasons into early 2012. For both the Oct-Dec and
Nov-Jan seasons, 40% of the models indicate La
Niña conditions, and 60% indicate neutral conditions.
For Dec-Feb, 48% show neutral conditions, 48% show La Niña
conditions, and 4% show El Niño development. At lead times of 4 or more
months into the future, statistical and dynamical models that incorporate
information about the ocean's observed subsurface thermal
structure generally exhibit higher predictive skill than those that do
not. Among models that do use subsurface temperature information,
10 of 18 (56%) predict ENSO-neutral SSTs for the Feb-Apr 2012 season,
7 of 18 (39%) predict La Niña conditions, and 1 of 18 (6%) predict
El Niño conditions.
(Note
1). (Note that La Niña conditions for Feb-Apr require
a NINO3.4 SST anomaly of -0.45 or stronger, and El
Niño conditions require 0.40 or stronger.) Caution is
advised in interpreting the distribution of model predictions as the
actual probabilities. At longer leads, the skill of the models
degrades, and skill uncertainty must be convolved with the
uncertainties from initial conditions and differing model physics,
leading to more climatological probabilities in the long-lead ENSO
Outlook than might be suggested by the suite of models.
Furthermore, the expected skill
of one model versus another has not been established using uniform
validation procedures, which may cause a difference in the true
probability distribution from that taken verbatim from the raw
model predictions. An alternative way to assess the probabilities of the three
possible ENSO conditions is to use the mean of the predictions of all
models, and to construct a standard error function centered on that
mean. The standard error would be Gaussian in shape, and would have its
width determined by an estimate of overall expected model skill for the
season of the year and the lead time. Higher skill would result in a
relatively narrower error distribution, while low skill would result in
an error distribution with width approaching that of the historical
observed distribution. This method shows probabilities for La
Niña at 41% for Oct-Dec, increasing to 50% for Dec-Feb and hovering
between 46 and 51% into early 2012.
Model probabilities for El Niño are near
0% for Nov-Jan and remain below 10% through Apr-Jun 2012.
Probabilities for ENSO-neutral
conditions are 59% for Oct-Dec and hover near 50% through Jan-Mar 2012, rising
slightly toward 55% through northern spring 2012.
The same cautions mentioned above for the distribution of model predictions apply
to this alternative method of inferring probabilities, due to differing model
biases and skills. In particular, this approach considers only the
mean of the predictions, and not the range across the models, nor the
ensemble range within individual models. The IRI's probabilistic ENSO prediction takes into account the indications of this set of models, the outcome of the standard error approach described above, and additional factors such as the very latest observations that may have developed after the initialization times of some of the models. In the case of this forecast, the forecasters have increased the probability of continuation of La Niña above the levels indicated by the models, based on the recent and current La Niña observations and the increasing negative heat content anomaly in the central and eastern tropical Pacific. It indicates a 78% probability for La Niña conditions in the Oct-Dec season in progress, dropping slowly to 70% by Dec-Feb 2011-12 and to 51% by Mar-May 2012. Probabilities for ENSO-neutral conditions are between 22% and 29% through Dec-Feb 2011-12, rising to 50% or higher from Mar-May 2012 onward. This indicates that continuation of La Niña is more likely than neutral conditions until early 2012, and that a return to neutral conditions during the remainder of 2011, while possible, is relatively less likely than persistence of at least weak La Niña conditions. Probabilities for El Niño conditions do not rise to 5% until Feb-Apr 2012, and remain below 10% until Mar-May 2012. See also: Note 1 - Only models that produce a new ENSO prediction every month are included in the above statement. |