No sé si a lo mejor deberíamos abrir un hilo distinto para hablar de la teoría de formación de estos cicloncetes tan particulares... habría mucho que debatir...

Cita de: Gale en Abril 14, 2013, 22:29:50 pm

¿Conclusiones para este año?

    sólo he analizado dos años,  y apenas sé de Huracanes ... no estoy en posición de concluir nada para this year ...

Os he dado algunas herramientas que pueden ser útiles para ver como puede venir  la temporada ... Si aprendes a usarlas con lo que sabes de HURACANES , te aseguro que podrás sacar unos pronósticos fantásticos .... :D1

Hmmm... No sé... seguiremos observando... Pero esos pronósticos no me dicen mucho, la verdad...

Technical ENSO Update

18 April 2013

Recent and Current Conditions
After a brief period approaching borderline La Niña SST conditions in January and February 2013, the SST anomaly in the Nino3.4 region returned to more clearly neutral levels during March and has remained neutral through mid-April 2013. For March 2013 the Nino3.4 SST anomaly was -0.22 C, indicative of cool-neutral ENSO conditions, and for January-March the anomaly was -0.34 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 0.0 C, indicating neutral ENSO conditions in the tropical Pacific; this is not far from the -0.22 C level observed in March.

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 second quarter of 2013, with probabilities of El Niño or La Niña each less than 25% through northern summer 2013. The latest set of model ENSO predictions, from mid-April, is now available in the IRI/CPC ENSO prediction plume, discussed below. Currently, SSTs have been in the middle of the ENSO-neutral range (anomaly of about -0.3 to 0.1 C), and SST is slightly above average in the far western part of the basin. Subsurface temperatures across the equatorial Pacific average close to the climatological average, but are above average in the western quarter of the basin and near average in the east-central tropical Pacific. In the east-central part of the basin, a large pocket of below-average sea temperature at depth is currently overlain by a 50-meter deep layer of near to slightly above average sea temperature, protecting the surface (SST) from the anamalously colder water beneath. In the atmosphere, the basin-wide sea level pressure pattern (e.g. the SOI), has been mainly to slightly above average and the low-level zonal winds have also been near average. Anomalous convection (as measured by OLR) has generally been negative in the central tropical Pacific, and positive in the far western part of the basin. Together, these features collectively reflect ENSO-neutral conditions, and the tendency toward cooler than average ENSO conditions has weakened over the last month.

As of mid-April, 20% of the set of dynamical and statistical models models predicts weak La Niña SST conditions for the Apr-Jun 2013 season, none predicts El Niño conditions, and 80% 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 Jul-Sep season, among models that do use subsurface temperature information, 85% predicts ENSO-neutral SSTs, 5% predicts El Niño conditions and 10% predicts La Niña conditions. For all model types, the probability for neutral ENSO conditions is 65% or greater from Apr-Jun to the end of the forecast period in northern winter 2013/14. (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 16% for Apr-Jun 2013, 24% for May-Jul, and also 24% for Jun-Aug 2013, remaining between 20% and 25% throughout 2013. Model probabilities for ENSO-neutral conditions are 83% for Apr-Jun 2013, 69% for May-Jul, and 64% for Jun-Aug 2013, decreasing to between 55% and 65% from Jul-Sep through the calendar year. Probabilities for El Niño are 1% for Apr-Jun 2013, 7% for May-Jul, rising to approximately 15% from Jun-Aug through the rest of 2013. In words, the models collectively favor neutral ENSO conditions through to the remainder of 2013; La Niña is very slightly favored over El Niño during all of the period. 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 second half of 2013. Uncertainty exists, because we are in the period of typically most likely new ENSO event evolution from now until about late June. The model forecast spread expresses that undertainty in the spread between weak La Nina and borderline El Nino conditions, even though the majority of the forecasts is in the neutral range. A caution regarding this latest set of model-based ENSO plume predictions, is that 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.