NOAA July 2018 ENSO Update: Chance of an El NiƱo Winter? Currently About 70%

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July 2018 ENSO Update: Dog days

Author: Emily Becker

The chance that El NiƱo conditions will be in place across the tropical Pacific by the fall is about 65%, and close to 70% by the winter, continuing the El NiƱo Watch from last month. Here in the U.S., with sultry weather from coast to coast, itā€™s hard to think about winter right nowā€¦but thatā€™s our job! After a trip through the tropical Pacific, weā€™ll get into what El NiƱo could mean for global weather and climate this winter.

A splash in the pool

The tropical Pacific is still well within neutral limits. The temperature of the ocean surface in the NiƱo3.4 region has edged above average, with June 2018 coming in about 0.11 degrees Celsius above the long-term average, based on our best-quality data set. Most climate models predict that the NiƱo3.4 region temperatures will reach the El NiƱo threshold (0.5Ā°C above the long-term average) by the fall.

noaa, enso, el nino
Monthly sea surface temperature in the NiƱo 3.4 region of the tropical Pacific for 2018 (purple line) and all other years since 1950 that started from La NiƱa conditions. In all but one of those years, a positive temperature anomaly by this point in the summer foreshadowed El NiƱo by winter. Climate.gov graph based on ERSSTv5 temperature data. Credit: NOAA

Much of the rest of the equatorial Pacific is warmer than average now, as well, with only the NiƱo1+2 region (the farthest east region, next to the coast of South America) still cooler than average.

The temperature of the water below the surface of the Pacific is elevated, too. The downwelling Kelvin wave that was initiated a few months ago has sloshed to the east across the Pacific, bringing warmer waters toward the surface. Itā€™s likely the surface will continue to warm over the next few months, helping to support the forecast for El NiƱoā€™s development.

noaa, enso, el nino
Departure from average of the surface and subsurface tropical Pacific sea temperature averaged over 5-day periods starting in early June 2018. 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. Climate.gov figure from CPC data. Credit: NOAA

Fans & sprinklers

The atmosphere over the tropical Pacific is demonstrably neutral right now. Cloud cover and rain over the central Pacific are still reduced compared to average, a hold-over from this past winterā€™s La NiƱa. On the other hand, atmospheric conditions over Indonesia have returned to near-average.

Both the Southern Oscillation Index and the Equatorial Southern Oscillation Index were near zero during June, reflecting neutral conditions. These indexes compare the surface air pressure in the central-eastern Pacific to the pressure in the western Pacific, a useful metric for the Walker circulation.

If the pressure in the eastern Pacific is relatively lower (more rising air than average, resulting from warmer-than-average sea surface temps) and the pressure to the west is relatively higher (less rising air, due to cooler waters), it can be another indication the Walker circulation has weakened, representing the atmospheric component of El NiƱo. Donā€™t forgetā€”the ā€œSOā€ part of ENSO stands for ā€œSouthern Oscillation.ā€

Weā€™ll keep an eye on these indexes and the other indicators of the atmospheric component of ENSO while weā€™re sweating it out over the summer and into the fall. El NiƱo is a coupled system, meaning it requires both the NiƱo3.4 region to be more than 0.5Ā°C above average and for the atmosphere to respond to those warmer-than-average waters. When both conditions are met, and expected to continue for several months, El NiƱo conditions will have arrived.

noaa, enso, el nino
Summary of decision process in determining El NiƱo conditions. NOAA Climate.gov drawing by Glen Becker and Fiona Martin. Credit: NOAA

Dreaming of winter

Soā€¦ who cares? Why do we even spend so much time and energy on El NiƱo? Because, to quote my blog-brother Tom, itā€™s a seasonal forecasterā€™s best friend. When the normal location and intensity of thunderstorms and winds in the Pacific basin are disturbed, itā€™s like a cannonballer sending waves through a pool: the effects are felt around the globe. Because El NiƱo and La NiƱa are generally predictable months in advance, forecasting an El NiƱo during the winter means we can often anticipate certain U.S. weather patterns during the winter.

noaa, enso, el nino
Typical rainfall and temperature patterns during El NiƱo events. Such teleconnections are likely during El NiƱo events, but not certain. Map by climate.gov.

Of course, the atmosphere is a huge, chaotic system, and we donā€™t see every expected effect every time El NiƱo shows up. More than half of the events since 1950 have some kind of wet signal over California, for example, but it can be confined to the southern part of the state in some events and shifted northward during others. (Hereā€™s the corresponding image for temperature.)

Also, El NiƱo is never the only player on the field (check out the index page, under ā€œPosts about things other than ENSOā€). That said, a forecast for an El NiƱo winter can give us an early glimpse of our winter weather, even while weā€™re sweltering under summerā€™s heat domes.


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