Official NOAA El Nino Update: Extreme Neutral!

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August 2017 ENSO update: Extreme neutral!

August 10, 2017

Now that itโ€™s summer in the Northern Hemisphere, weโ€™re more firmly on the other side of the infamousย spring barrier. So, forecasters have growing confidence that this coming winter in the Northern Hemisphere will most likely be a continuation of โ€œENSO-Neutral,โ€ and dominated by near average temperatures across the Pacific Ocean. Theย most recent forecast by CPC/IRIย favors the continuation of these conditions through the winter 2017-18 (56% chance during December-February 2017-18).

ENSO-Neutral = El Niรฑo or La Niรฑa is not present

Following some weakly warm conditionsย last month, this past month was characterized by an impressive span of near-average sea surface temperatures over the tropical Pacific Ocean.

July 2017 SST anomalies
Average sea surface temperature (SST) during July 2017, shown as departure from the long-term (1981-2010) average. Red shading shows where SSTs were above average and blue shading shows where they were below average. Climate.gov figure from OISSTv2 data at CPC.

Impressive because usually at least one region of the tropical Pacific Ocean (the so-called โ€œNiรฑo regionsโ€) contains either below or above average temperatures. In July 2017,ย all fourย Niรฑo regions were between +0.3ยฐC and -0.3ยฐC. This has happened only about 4% of the time since 1950, most recently in December 2013 (usingย ERSSTv4 data). So itโ€™s been a while since surface temperatures across the tropical Pacific Ocean have been so very normal.

The atmosphere was livelier, as it is prone to be, given that air moves rapidly across the tropical Pacific, especially relative to the heavy, slower moving ocean. In the past month, we saw a weak, short-livedย Madden-Julian Oscillation, which resulted in some increased rainfall near the International Date Line. But rainfall continues to persevere near the Maritime Continent, as do slightly stronger-than-average trade winds over the west-central Pacific.

July 2017 OLR anomalies
Places that were more (purple) or less (orange) cloudy than the 1981-2010 average during July 2017, based on satellite observations of outgoing longwave radiation (heat). Thick clouds block heat from radiating out to space, so less radiation equals more clouds, and more radiation equals clearer skies. Climate.gov map from CPC OLR data.

Despite the warm ocean conditionsย earlier this year, the atmosphere never locked into an El Niรฑo. The official outlook reflects the models, which mostly show Niรฑo-3.4 index hovering within ENSO-Neutral ranges (-0.5ยฐC to +0.5ยฐC). But because nothing in prediction isย a sure thing, forecasters are assigning smaller, but non-zero chances to La Niรฑa (28% chance) and El Niรฑo (16% chance) this coming winter (December-February 2017-18). This also represents a flip from previous months when El Niรฑo was slightly favored over La Niรฑa. Now weโ€™re seeing a clearer cooling trend in the observations and model guidance.

Does ENSO-Neutral cause Typical or Average Weather?

Nope. What Neutral means is that there is little-to-noย forcingย coming from either El Niรฑo or La Niรฑa in the tropical Pacific. You can think of a forcing as a push in a certain direction. El Niรฑo and La Niรฑa shove around the global atmospheric circulation, and the lack of either means this pushing motion is absent.

ENSO neutral cartoon
Concept by Tom Di Liberto and illustration by Emily Greenhalgh, NOAA Climate.gov.

As weโ€™ve coveredย here,ย here, andย here, El Niรฑo and La Niรฑa are linked to large changes in rainfall and convection patterns over the tropical Pacific Ocean. Those changes can then alter the tropicalย Walker circulationย and theย jet streamsย over the middle latitudes of the Northern and Southern Hemispheres.

So, Neutral conditions mean that atmospheric flow isnโ€™t pushed around in a way that is predictable. Climate forecasters like having an El Niรฑo and La Niรฑa around because it canย provides some useful informationย many months in advance. In the absence of an El Niรฑo and La Niรฑa, the predictable signals are weaker.

This doesnโ€™t mean that there arenโ€™t any other patterns out there that are influencing our weather and climate (there areย tons), but it is harder toย predict them months in advance. For example, we could seeย Arctic Oscillationย orย Madden-Julian Oscillationย activity, which are very important, and can have a substantial influence on temperature and precipitation, but are not clearly anticipated months into the future.

Despite the lack of forcing from ENSO, forecasters will still be closely examining the models to suss out other possible sources of prediction skill. These other more predictable forcings commonly come in the form of longer-term trends in temperature and changes in the land surface (soil moisture, snow, ice).

Whereโ€™s Emily? Free Emily!

Sheโ€™s around! She is away this week doing work stuff. Sheโ€™ll be the editor later this month on a guest post written by Phil Klotzbach on what is happening with the hurricanes this year. And make sure you check out herย recent post on climate models.

Also, because there isnโ€™t much going on with ENSO these days, we are looking to cover other climate and weather subjects in the coming months. If you have burning questions or an idea youโ€™d like us to cover, just drop it in the comments section below.


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