Details on the August 7th ENSO Discussion: how has the forecast changed?
This month’s ENSO Diagnostic Discussion starts off with “the chance of El Niño has decreased to about 65% during the Northern Hemisphere fall and early winter.” The last few months, chances were estimated to be around 80% for El Niño to have formed by the fall/early winter. So, we’ve gone from an estimated 1-in-5 chance that we won’t have an El Niño to a nearly 1-in-3 chance. However, 65% is still almost twice the climatological likelihood – that is, the long-term average of how often we experience El Niño conditions – so forecasters are still predicting El Niño will develop.
So, why the decrease in the odds of El Niño?
Last month, we discussed how the atmosphere has yet to respond to the sea-surface temperatures, and Michelle went into a bit more depth about a possible explanation for why the atmospheric response may be delayed. As of the beginning of August, we still haven’t seen a strong atmospheric response (the SOI is -0.2, and the EQSOI is 0.1), and the sea-surface temperature in the central-Eastern Pacific has cooled, leading the weekly Niño3.4 index to drop to -0.1°C by the end of the month. A few other observations have contributed to the somewhat more conservative forecasts, such as the slightly below-average (cooler) ocean heat content.
Given these observed conditions, why are chances even as high as 65%? There are a few different considerations that are leading forecasters to these probabilities, including computer model forecasts of sea-surface temperature, and forecasts that the recently developed westerly wind anomalies along the equatorial Pacific may continue.
The forecast takes into account several dynamical climate models, including the Climate Forecast System version 2 (CFSv2, Fig. 1) and the eight-model National Multi-Model Ensemble (NMME). One of the many products of these models is the forecast for the Niño3.4-region sea surface temperature. The models are run many times to form an ensemble of forecasts, each time with a slightly different set of “initial conditions” – that is, the observed fields (such as temperature, air pressure, and so on) that provide the starting point for the forecast. A common way to get different initial conditions is to run the model a few times per day, for example at midnight, 6 a.m., noon, and 6 p.m. The results of the many runs are averaged to yield the ensemble mean, a kind of model consensus.
CFSv2, which is run four times per day (each colored line in Fig. 1 represents one “model run”, and the black dashed line shows the ensemble mean) continues to consistently forecast a weak-to-moderate El Niño, peaking in the early winter. In addition, all of the NMME models are still calling for El Niño conditions to develop, with most in the “weak” range of +0.5°C to +0.9°C (Fig. 2).
Why do forecasters lean toward trusting the models, despite the fact that conditions seem to be trending away from an El Niño-friendly state? Among the reasons is that the CFSv2 predicted the current dip in sea surface temperatures in the Niño3.4 region in both May and June, which indicates they have a good handle on how the climate is behaving. That lends credibility to the prediction of El Niño by fall/winter. Several of the NMME models also predicted the dip in July (Fig. 2; the CFSv2 that’s included in the NMME is the same model as that shown in Fig. 1.)
One way that forecasters evaluate model output is by counting how many of the individual runs fall into a specific category, such as “above normal”, “near normal”, or “below normal.” The number of runs in each category, divided by the total number of model runs, gives us a percentage (see Fig. 3 for an example.) The black box in Fig. 3 indicates the Niño3.4 region; as you can see, more than 70% of the model runs fall in the “above average” category for the December-January-February sea surface temperature forecast.
The climate models look out several months into the future. A near-term factor that is being closely watched by forecasters is the change in the winds along the equatorial Pacific. As we’ve mentioned earlier, the winds along the equator usually blow from east to west, keeping warmer water piled up in the Western Pacific. If these winds relax, or even reverse, this warmer water can move to the east. (A couple of these “westerly wind bursts” back in the winter kicked off the downwelling Kelvin wave this spring.) Toward the end of July, the typical easterly winds again relaxed some (westerly wind anomalies appeared), and there is some suggestion these wind anomalies may continue.
As Tony explained a few weeks ago, climate forecasting (including ENSO forecasting) is all a matter of probabilities. While the forecast chance has decreased, there is always plenty of uncertainty on just what will happen. As we’ve said, even a forecast of 80% for an event means there’s a 1-in-5 chance that the event won’t happen; now, while we’re estimating a 65% chance that El Niño will happen, that means a roughly 1-in-3 chance that it won’t.
The ENSO blog is written, edited, and moderated by Michelle L’Heureux (NOAA CPC), Emily Becker and Tom DiLiberto (contractors to CPC), Anthony Barnston (IRI), and Rebecca Lindsey (contractor to NOAA CPO). Posts reflect the views of the bloggers themselves and not necessarily Climate.gov, NOAA, or Columbia University/IRI.