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Technical ENSO Update
17 June 2010
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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