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Technical ENSO Update

17 June 2010


> Current conditions
> Expected conditions

Current Conditions

As of mid-June 2010, SSTs are at borderline La Niña levels in the central and eastern equatorial Pacific, following the rapid dissipation of the moderate(+) El Niño of 2009/10 in early May 2010. For May the SST anomaly in the NINO3.4 region was -0.03 C, indicative of ENSO-neutral conditions, while for the Mar-Apr-May season the anomaly was 0.60 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 Jun-Jul-Aug and the Jun-Jul-Aug seasons are approximately (-0.50C, 0.45) and (-0.50, 0.45), respectively.

Expected Conditions

 The most recent weekly SST anomaly in the NINO3.4 region is -0.5 C, indicating borderline La Niña conditions in the tropical Pacific; this is somewhat lower than the -0.03 C level observed in May, suggesting that the SST is in the process of decreasing. What is the outlook for the ENSO status going forward? June is a month of the year, together with April and May, historically associated with transitions in the ENSO state. With the demise of the moderate(+) El Niño and now attainment of borderline La Niña conditions, the question is whether cool-neutral or just borderline La Niña conditions conditions will persist over the coming several months, or alternatively if the current condition represents an intermediate point within a transition toward a more clearly and strongly La Niña state. A clue to the answer lies in the fact that negative subsurface sea temperature anomalies prevail at depth in the central and eastern Pacific, having replaced the above-average water temperatures with the ending of the 2009/10 El Niño. Sea temperature anomalies below the surface often precede sea surface temperature anomalies to be expected in the following months, as they are subject to the climatological upwelling in the eastern part of the basin. Current low-level wind anomalies indicate slightly enhanced trades across most of the tropical Pacific, and positive traditional and equatorial SOI indices. These atmospheric features imply average to somewhat above-average upwelling activity in the eastern tropical Pacific, at least for the near term, and suggest that the negative subsurface sea temperature anomalies will likely find their way to the surface during the coming months. The surfacing of below-average subsurface waters portend a likelihood for developing La Niña conditions, and this process has already been underway as pockets of below-average SST have been appearing along the equator in the eastern Pacific since mid-May. This below-average SST has been meridionally limited within about 3-5 degrees latitude of the equator; but the spatial extent would increase, as would the peak anomaly magnitudes, with further development of La Niña conditions.

Presently, the models and observations taken together indicate probabilities of about 58% for developing La Niña conditions, 41% for maintaining ENSO-neutral conditions, and 1% for returning to El Niño conditions during the June-July-August season in progress. Going forward, probabilities for La Niña increase to approximately 62% by Aug-Sep-Oct, while probabilities for neutral and El Niño conditions become 37% and 1%, respectively. These probabilities extend through December-January-February 2010/11, after which the tilt of the odds toward La Niña begin to weaken.

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.

The models show general agreement regarding the very low probability for El Niño conditions over the remainder of 2010 and into early 2011, but nonetheless indicate some divergence throughout most of the period. The statistical models are divided mainly between cool-neutral conditions and weak La Niña conditions throughout the period, while the dynamical models mainly predict some magnitude (in some cases, very strong) of La Niña condition. Collectively the average of the model predictions is for weak La Niña conditions. For the current Jun-Jul-Aug season, 57% of the models are predicting ENSO-neutral conditions, while 43% predict La Niña conditions. However, for the coming Jul-Aug-Sep season, only 39% of the models predict ENSO-neutral conditions while 61% predict La Niña conditions, and this tilt of the odds is maintained throughout the remainder of 2010 and into early 2011. 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, none indicate El Niño conditions for the Oct-Nov-Dec season, 6 of 15 (40%)  predict ENSO-neutral SSTs, and 9 of 15 (60%) predict La Niña conditions. (Note 1). (Note that La Niña conditions for Oct-Nov-Dec require a NINO3.4 SST anomaly of -0.75 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 about 64% and 70% for Jun-Jul-Aug and Jul-Aug-Sep, respectively, and approximately 55-60% from Aug-Sep-Oct through the rest of 2010 and into early 2011. (Note that the threshold for La Niña increases from approximately -0.50C to -0.75C between Jul-Aug-Sep and Oct-Nov-Dec, and some of the model predictions for La Niña do not increase in strength in parallel with this seasonality of the interannual variance). 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. It indicates a 58% probability for La Niña conditions in the Jun-Jul-Aug season in progress, increasing to near 62% for Aug-Sep-Oct forward into early 2011, while ENSO-neutral probabilities begin at 41% for Jun-Jul-Aug and decrease to 37% from Aug-Sep-Oct onward through early 2011. The probability for a return to El Niño conditions are approximately 1% from the present until early 2011.

See also: 

Note 1 - Only models that produce a new ENSO prediction every month are included in the above statement.
 
 

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