NOAA January 2020 ENSO Update: New Year, New You

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Summary of the decision process in determining El Niรฑo conditions. NOAA Climate.gov drawing by Glen Becker and Fiona Martin.

This post was written by Emily Beckerย and first appeared on the NOAA ENSO Blog

Ocean and atmospheric conditions in the tropical Pacific are ENSO-neutral, and forecasters favor neutral through the spring. Wait, donโ€™t go! As usual, thereโ€™s a lot more to the ENSO story.

Get organized

The sea surface temperature in the Niรฑo3.4 region in the east-central equatorial Pacific, our primary location for monitoring the El Niรฑo-Southern Oscillation (ENSO) climate phenomenon, has been above average for a few months now. In fact, the 3-month-average (the Oceanic Niรฑo Index) in Octoberโ€“December was 0.46ยฐC above normal, which rounds to 0.5ยฐC. โ€œHey!โ€ you say. โ€œIsnโ€™t that the El Niรฑo threshold?โ€ Indeed it is, but of course, El Niรฑo requires more than a couple months of above-average sea surface temperature. According to the El Niรฑo criteria, we also need an expectation that the sea surface temperature will stay above the threshold for several more seasons. (In climate-speak, โ€œseasonโ€ is any three-month-average period.)ย  In addition, thereโ€™s that pesky requirement that the tropical Pacific atmospheric circulation shows a response.

Most climate models predict that the Niรฑo3.4 sea surface temperature will stay above the long-term average for a couple more months, hovering around the El Niรฑo threshold, before decreasing to near-average through the spring. Weโ€™re not yet into the time of year when we have to worry about the spring predictability barrier (essentially, dynamical model forecasts made during April and May tend to be less reliable than those made during other times of the year), lending weight to these predictions.

Based in large part on these model predictions, forecasters estimate a greater than 50% chance the Novemberโ€“January, and Decemberโ€“February Oceanic Niรฑo Index values will be about 0.5ยฐC above average. A downwelling Kelvin wave that will continue moving eastward under the surface of the tropical Pacific over the next month or so will also provide a source of warmer-than-average water to keep the surface temperature elevated for at least another month or two.

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Departure from average of the surface and subsurface tropical Pacific sea temperature averaged over the 5-day period centered on January 3, 2020. The vertical axis is depth below the surface (meters) and the horizontal axis is longitude, from the western to eastern tropical Pacific. This cross-section is right along the equator. A downwelling (warm anomaly) Kelvin wave is moving across the equatorial Pacific Ocean. Climate.gov figure from CPC data.

After that, the largest share of the probability pie, about 60%, goes to neutral, meaning the Oceanic Niรฑo Index between -0.5ยฐC and 0.5ยฐC. What all this boils down to is that forecasters do not expect the current warmer equatorial Pacific water to develop into a full-blown El Niรฑo. That said, the recent warm surface conditions do bear monitoring, and the chance of El Niรฑo through the spring is estimated at about 30%. La Niรฑa has the smallest chance of developing through the spring, at around 10%.

Embrace uncertainty

All this โ€œx chance of whatever,โ€ โ€œy chance of some other whateverโ€ can seem unnecessarily complicated. Wouldnโ€™t it be easier if our forecast just said โ€œneutral will remainโ€ or โ€œLa Niรฑa is coming,โ€ sort of like how your weather forecast just says โ€œhigh of 70ยฐF tomorrow?โ€ Perhaps, but it wouldnโ€™t give a complete picture of the possible futures. ย When weโ€™re making climate forecasts the future is just more uncertain.ย  By assigning probabilities to each of the three categories, forecasters can provide decision-makers with potentially useful information. Knowing that neutral is most likely (6-in-10 chance) but there is still a 3-in-10 chance of El Niรฑo advises people to remain attentive to this potential. For more on how to understand probabilistic forecasts, check out Tony and Michelleโ€™s posts โ€œWhy do ENSO forecasts use probabilitiesโ€ and โ€œBetting on climate predictions.โ€

noaa, enso
Illustration by Emily Greenhalgh, NOAA Climate.gov.

Exercise more

Over the few weeks, the positive Indian Ocean Dipole pattern (colder-than-average water in the eastern Indian Ocean, warmer-than-average in the western Indian Ocean) has finally abated.

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Animation showing sea surface temperature departure from the long-term average from September 2019 through early January 2020. Graphic by climate.gov; data from NOAAโ€™s Environmental Visualization Lab.

Colder-than-average water in the eastern Indian Ocean and the islands of Southeast Asiaโ€”the โ€œMaritime Continentโ€โ€”has the effect of suppressing convection, meaning there is less rising air, cloud formation, and rain than usual. This contributed to the devastating fire conditions Australia has experienced over the past few months. As the positive Indian Ocean Dipole has weakened, convection has re-emerged over the Maritime Continent in the last week.

Learn a new hobby

Our resolution is the same as everโ€”keep you updated on all things ENSO. And maybe get to the gym a little more oftenโ€ฆ.


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