ENSO Updates

[Ptarmigan]

This Week's ENSO
Niño 4 0.6ºC
Niño 3.4 0.4ºC
Niño 3 0.2ºC
Niño 1+2 0.3ºC

Things are cooling down in Region 3.4 and 4, while 3 and 1+2 are warming.

http://www.cpc.ncep.noaa.gov/products/a ... ts-web.pdf

[Ptarmigan]

This Week's ENSO
Niño 4 0.6ºC
Niño 3.4 0.4ºC
Niño 3 0.1ºC
Niño 1+2 0.2ºC

No change. El Nino looks like DOA.

http://www.cpc.ncep.noaa.gov/products/a ... ts-web.pdf

[Ptarmigan]

This Week's ENSO
Niño 4 0.7ºC
Niño 3.4 0.5ºC
Niño 3 0.2ºC
Niño 1+2 -0.5ºC

http://www.cpc.ncep.noaa.gov/products/a ... ts-web.pdf

Looks like warming up is happening again.

[Ptarmigan]

This Week's ENSO
Niño 4 0.5ºC
Niño 3.4 0.3ºC
Niño 3 0.1ºC
Niño 1+2 -0.7ºC

Cooling down again. No El Nino for now.

http://www.cpc.ncep.noaa.gov/products/a ... ts-web.pdf

[Ptarmigan]

The ENSO Precipitation Index (ESPI) for the last 30 days is -0.40

http://trmm.gsfc.nasa.gov//trmm_rain/Ev ... y_day.html

[Ptarmigan]

This Week's ENSO
Niño 4 0.4ºC
Niño 3.4 0.2ºC
Niño 3 -0.1ºC
Niño 1+2 -1.4ºC

Region 1+2 is in full La Nina. Not good for El Nino.

http://www.cpc.ncep.noaa.gov/products/a ... ts-web.pdf

[Ptarmigan]

Q: Why NOAA uses ENSO Region 3.4?
A: A new region, called Niño 3.4 (120°-150°W and 5°N-5°S) is now used as it corrolates better with the Southern Oscillation Index and is the prefered region to monitor sea surface temperature.

El Niño Southern Oscillation (ENSO)
http://www.srh.noaa.gov/jetstream/tropics/enso.htm

[Ptarmigan]

This Week's ENSO
Niño 4 0.1ºC
Niño 3.4 -0.1ºC
Niño 3 -0.2ºC
Niño 1+2 -0.9ºC

All ENSO regions dropped, while 1+2 rose.

http://www.cpc.ncep.noaa.gov/products/a ... ts-web.pdf

Looks to be Neutral. The strong cool PDO overpowered any hopes for El Nino due to teleconnection.

Climate Prediction Center 12/6/12 December update
http://www.cpc.ncep.noaa.gov/products/a ... odisc.html

Cool PDOs are less likely to see El Nino, especially strong ones with the exception of 1972-1973, which occurred in cool PDO. Strong ones appear in warm PDOs like 1982-1983, 1991-1992, and 1997-1998.

[MontgomeryCoWx]

The latest weekly SST departures are:
Niño 4 0.4ºC
Niño 3.4 -0.1ºC
Niño 3 -0.3ºC
Niño 1+2 -0.8ºC

[Ptarmigan]

This Week's ENSO
Niño 4 0.2ºC
Niño 3.4 -0.2ºC
Niño 3 -0.3ºC
Niño 1+2 -0.6ºC

[Ptarmigan]

This Week's ENSO
Niño 4 0.2ºC
Niño 3.4 -0.1ºC
Niño 3 -0.3ºC
Niño 1+2 -0.6ºC

http://www.cpc.ncep.noaa.gov/products/a ... ts-web.pdf

[Ptarmigan]

This Week's ENSO
Niño 4 0.0ºC
Niño 3.4 -0.6ºC
Niño 3 -0.7ºC
Niño 1+2 -0.4ºC

http://www.cpc.ncep.noaa.gov/products/a ... ts-web.pdf

Region 3 and 3.4 have gone into La Nina.

[wxman57]

Technically, La Nina is defined by the 3-month average SST anomaly of -.5C or colder. The forecast is for slowly warming SSTs in the Tropical Pacific through next fall, but temps remaining in the "neutral" range through the hurricane season.

[MontgomeryCoWx]

I hate La Nina's with a fiery passion.

[Ptarmigan]

This Week's ENSO
Niño 4 -0.2ºC
Niño 3.4 -0.6ºC
Niño 3 -0.6ºC
Niño 1+2 -0.4ºC

http://www.cpc.ncep.noaa.gov/products/a ... ts-web.pdf

No change in Region 1+2 and 3.4. However, it has warmed slightly in Region 3, while Region 4 was cooled.

[Ptarmigan]

This Week's ENSO
Niño 4 0.0ºC
Niño 3.4 -0.2ºC
Niño 3 -0.5ºC
Niño 1+2 -0.6ºC

http://www.cpc.ncep.noaa.gov/products/a ... ts-web.pdf

Warmed up in all regions except for 1+2.

[Ptarmigan]

This Week's ENSO
Niño 4 0.0ºC
Niño 3.4 -0.5ºC
Niño 3 -0.9ºC
Niño 1+2 -0.5ºC

http://www.cpc.ncep.noaa.gov/products/a ... ts-web.pdf

Warm up at Region 1+2. Cool down at Region 3 and 3.4. No change for Region 4.

[Ptarmigan]

This Week's ENSO
Niño 4 -0.1ºC
Niño 3.4 -0.5ºC
Niño 3 -0.7ºC
Niño 1+2 -0.2ºC

http://www.cpc.ncep.noaa.gov/products/a ... ts-web.pdf

Region 1+2 and 4 warmed, while Region 3 and 3.4 cooled.

[Ptarmigan]

This Week's ENSO
Niño 4 0.0ºC
Niño 3.4 -0.3ºC
Niño 3 -0.4ºC
Niño 1+2 -0.1ºC

All regions have warmed up.

[Ptarmigan]

Technical ENSO Update

21 February 2013

Recent and Current Conditions
After a brief period of borderline El Niño SST conditions between July and September 2012, the SST anomaly in the Nino3.4 region returned to neutral levels during October and has remained neutral through mid-February 2013. For January 2013 the Nino3.4 SST anomaly was -0.41 C, indicative of cool-neutral ENSO conditions, and for November-January the anomaly was -0.05 C. Since late 2011, the IRI's definition of El Niño conditions has become the same as that of NOAA/Climate Prediction Center, in which the SST anomaly in the NINO3.4 region (5S-5N; 170W-120W) exceeds 0.5 C. Similarly, for La Niña, the anomaly must be -0.5 C or less. The climatological probabilities for La Niña, neutral, and El Niño conditions vary seasonally, and are shown in a table at the bottom of this page for each 3-month season. The most recent weekly SST anomaly in the NINO3.4 region was -0.3 C, indicating cool-neutral ENSO conditions in the tropical Pacific; this is similar to the -0.41 C level observed in January.
Expected Conditions

What is the outlook for the ENSO status going forward? The most recent official diagnosis and outlook was issued earlier this month in the NOAA/Climate Prediction Center ENSO Diagnostic Discussion, produced jointly by CPC and IRI; it called for a high likelihood of neutral ENSO conditions enduring through the first quarter of 2013, with probabilities of El Niño or La Niña each less than 30% through northern summer 2013. The latest set of model ENSO predictions, from mid-February, is now available in the IRI/CPC ENSO prediction plume, discussed below. Currently, SSTs are in the cool half of the ENSO-neutral range (anomaly of 0 to -0.5 C), and SST is above average in the western part of the basin. Subsurface temperatures across the equatorial Pacific average close to the climatological average, but are above average in the western half of the basin and below average in the east-central and eastern Pacific. In the atmosphere, the basin-wide sea level pressure pattern (e.g. the SOI), has been near to slightly below average (toward El Niño) but the low-level zonal winds have slightly favored enhanced trade winds. Anomalous convection (as measured by OLR) has generally been below average in the central tropical Pacific, and above average in the far western part of the basin. Together, although these last features exhibit gradients similar to those found during La Niña, all of the the features collectively reflect ENSO-neutral conditions, leaning to the cool side.

As of mid-February, 28% of the set of dynamical and statistical models models predicts weak La Niña SST conditions for the Feb-Apr 2013 season, none predicts El Niño conditions, and 72% indicates neutral ENSO. At lead times of 3 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. For the May-Jul season, among models that do use subsurface temperature information, 100% predict ENSO-neutral SSTs, 0% predicts El Niño conditions and 0% predicts La Niña contitions. For all model types, the probability for neutral ENSO conditions is 80% or greater from Apr-Jun to the end of the forecast period in northern autumn 2013. (Note 1). 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 more quantitatively precise and less vulnerable to sampling errors than the categorical tallying method used above. This alternative method uses the mean of the predictions of all models on the plume, equally weighted, and constructs a standard error function centered on that mean. The standard error is Gaussian in shape, and has its width determined by an estimate of overall expected model skill for the season of the year and the lead time. Higher skill results in a relatively narrower error distribution, while low skill results in an error distribution with width approaching that of the historical observed distribution. This method shows probabilities for La Niña at 26% for Feb-Apr 2013, 28% for Mar-May, and 27% for Apr-Jun 2013, remaining in the middle to upper 20s through northern autumn. Model probabilities for ENSO-neutral conditions are 74% for Feb-Apr 2013, 71% for Mar-May, and 69% for Apr-Jun 2013, decreasing into the 50s thereafter through autumn 2013. Probabilities for El Niño are near 0% for Feb-Apr 2013, 1% for Mar-May, rising to the 15-20% range from Jun-Aug through northern autumn. In words, the models collectively favor neutral ENSO conditions straight through to the third quarter of 2013, but during the first season or two La Niña is favored over El Niño. A plot of the probabilities generated from this most recent IRI/CPC ENSO prediction plume using the multi-model mean and the Gaussian standard error method summarizes the model consensus out to about 10 months into the future. The same cautions mentioned above for the distributional count of model predictions apply to this Gaussian standard error 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 total range across the models, nor the ensemble range within individual models.

The probabilities derived from the 24 or more models on the IRI/CPC plume describe, on average, maintenance of neutral ENSO conditions during the coming months, continuing through into the latter half of 2013. Uncertainty increases greatly from around the Apr-Jun 2013 season onward, when the probablilities for neutral ENSO settle into the 50s and probabilities for non-neutral ENSO increase to approximately one-in-four for La Niña and one-in-five for El Niño. Following this latest model-based ENSO plume prediction, factors such as known specific model biases and recent changes that the models may have missed will be taken into account in the next official outlook to be generated and issued in early January by CPC and IRI, which will include some human judgement in combination with the model guidance.

http://portal.iri.columbia.edu/portal/s ... 2&userID=2

None of the forecast models are predicting La Nina or El Nino to the peak of hurricane season. It is most likely going to be Neutral.