El Niño Development Looking More Likely Now

By Anthony Watts – Re-Blogged From WUWT

ENSO-neutral conditions still reign as of the beginning of the month, but we’re starting to see some clearer signs of the development of El Niño.

Forecasters estimate that El Niño conditions will develop in the next few months, and there’s a 70-75% chance El Niño will be present through the winter.  Most computer models are currently predicting a weak El Niño event.

Over the past several weeks, surface temperature anomalies (difference from the long-term average) have gradually increased across much of the tropical Pacific. All four of the Niño-monitoring-region temperatures are now above average.

Animation showing sea surface temperature departure from the long-term average from August through early October 2018. Graphic by climate.gov; data from NOAA’s Environmental Visualization Lab.

The temperature in the Niño3.4 region (our primary metric for monitoring El Niño’s development) was 0.7°C above the long-term average in the latest weekly measurement. Yep, that’s above the El Niño threshold of 0.5°C, but we’ll need the monthly temperature in the Nino3.4 region to average above that threshold, plus an expectation that it will stay above, and indications that the atmosphere is responding to the change in the ocean before we’d declare El Niño.

ENSO diagnostic flowchart

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

Regular ENSO Blog readers will know that we go on about the winds that blow across the tropical Pacific. At times, we probably get pretty windy about the wind! That’s because these winds are very important to the development and maintenance of El Niño and La Niña. ENSO—short for El Niño-Southern Oscillation—is a coupled system, meaning the ocean causes changes in the atmosphere and the atmosphere in turn affects the ocean.

The trade winds normally blow from east to west (“easterly” winds, in meteorological parlance) along the equator in the Pacific. They help bring colder water up from the depths of the ocean to the surface near South America and also pile up warmer waters in the far western Pacific, near Indonesia. When these winds slow down, the surface water can warm, and warmer waters from Indonesia begin to slosh eastward (a downwelling Kelvin wave). It takes a few months for the warm blob of water to travel across the Pacific, and when it reaches the coast of South America, the blob can rise to the surface, providing a months-long source of warmer water to the surface.

The reason I’m rattling on about this effect of the winds is that we’ve recently had a pretty substantial slowing down of the trade winds in the central and eastern Pacific—one of the strongest such episodes during September/October since 1979, when our real-time reanalysis data records begin.

Wind anomalies (departure from the long-term average) during early October, 2018. Shading shows the strength of the anomaly; arrows indicate the direction of the anomaly.

This slowdown in the winds has already allowed the surface to warm, and will help to reinforce the warmer subsurface waters that have been developing since August. The temperature anomaly in the upper ~1000 feet of the central-eastern Pacific, elevated since the spring, has increased over the past month.

Area-averaged upper-ocean heat content anomaly (°C) in the equatorial Pacific (5°N-5°S, 180º-100ºW). The heat content anomaly is computed as the departure from the 1981-2010 base period pentad (5-day) means. Climate.gov figure from CPC data.

The development of El Niño in the late fall isn’t unusual, with nine El Niño events since 1950 starting in August­–October or later in the fall. Of these, only one (1986-87) had a peak Niño3.4 Index greater than 1.0 degree; all the others were weaker events. Since El Niño events peak in November or December, there probably isn’t enough time for sea surface temperature anomalies to grow very large.

The strength of El Niño doesn’t necessarily indicate the strength of its impacts on global weather. But a stronger El Niño can increase the likelihood that impacts of some kind will happen. The Climate Prediction Center’s winter outlook will be released next Thursday (October 18th), so stay tuned to see what effect El Niño may have on U.S. winter weather. We’ll also have a post here at the ENSO Blog on that outlook.

Source: climate.gov



issued by
and the International Research Institute for Climate and Society

11 October 2018

ENSO Alert System Status: El Niño Watch

Synopsis: El Niño is favored to form in the next couple of months and continue through the Northern Hemisphere winter 2018-19 (70-75% chance).

ENSO-neutral continued during September, but with increasingly more widespread regions of above-average sea surface temperatures (SSTs) across the equatorial Pacific Ocean [Fig. 1]. Over the last month, all four Niño index values increased, with the latest weekly values in each region near +0.7°C [Fig. 2]. Positive subsurface temperature anomalies (averaged across 180°-100°W) also increased during the last month [Fig. 3], due to the expansion and strengthening of above-average temperatures at depth across the equatorial Pacific [Fig. 4]. Convection was increasingly suppressed over Indonesia and around the Date Line [Fig. 5]. Low-level westerly wind anomalies were evident over the western and east-central Pacific, with some of the strongest anomalies occurring over the eastern Pacific during the past week. Upper-level wind anomalies were easterly over the east-central Pacific. Overall, the oceanic and atmospheric conditions reflected ENSO-neutral, but with recent trends indicative of a developing El Niño.

The majority of models in the IRI/CPC plume predict El Niño to form during the fall and continue through the winter [Fig. 6]. The official forecast favors the formation of a weak El Niño, consistent with the recent strengthening of westerly wind anomalies and positive temperature trends in the surface and subsurface ocean. In summary, El Niño is favored to form in the next couple of months and continue through the Northern Hemisphere winter 2018-19 (70-75% chance; click CPC/IRI consensus forecast for the chance of each outcome for each 3-month period).

This discussion is a consolidated effort of the National Oceanic and Atmospheric Administration (NOAA), NOAA’s National Weather Service, and their funded institutions. Oceanic and atmospheric conditions are updated weekly on the Climate Prediction Center web site (El Niño/La Niña Current Conditions and Expert Discussions). Forecasts are also updated monthly in the Forecast Forum of CPCs Climate Diagnostics Bulletin. Additional perspectives and analysis are also available in an ENSO blog. The next ENSO Diagnostics Discussion is scheduled for 11 October 2018.

Source: CPC/NCEP


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