Updated on 13 May 2019

ENSO status

The El Niño Southern Oscillation (ENSO) monitoring system remains in the “Watch” status this month. Warm sea-surface temperature (SST) anomalies over the Nino3.4 region are still present but showing slight weakening recently. The Nino3.4 index was 0.67°C for March 2019 and 0.58°C for January-March 2019 three-month average. Sub-surface temperatures continue to show cooling trend seen since the beginning of March, especially for regions east of the dateline (i.e. over the Central and Eastern Pacific). Trade winds are still neutral, and the coupling of the SST and atmosphere over the tropical Pacific is inconsistent.

While there are partial signs of El Niño conditions presently, future development remains uncertain. Model outlooks from international centres for the 2nd half of 2019 still show a wide spread of possible outcomes ranging from neutral to moderate El Niño. This high degree of uncertainty is due to the low predictability at this time of year for El Niño. The range of possible outcomes from model predictions can be expected to become narrower from June 2019 onwards.

Further Information on ENSO

ENSO conditions are monitored by analysing Pacific sea surface temperatures (SSTs), low level winds, cloudiness (using outgoing longwave radiation), and sub-surface temperatures. Special attention is given to SSTs, as they are one of the key indicators used to monitor ENSO. Here, three different datasets are used: HadISST, ERSSTv5, and COBE datasets. As globally, SSTs have gradually warmed over the last century under the influence of climate change, the SST values over the Nino3.4 will increasingly be magnified with time, and hence appear warmer than they should be. Therefore, this background trend is removed from the SST datasets (Turkington, Timbal, & Rahmat, 2018), before calculating SST anomalies using the climatology period 1976-2014. So far, there has been no noticeable background trend in the low-level winds or cloudiness.

El Niño (La Niña) conditions are associated with warmer (colder) SSTs in the central and eastern Pacific. The threshold for an El Niño (La Niña) in the Nino3.4 region is above 0.65°C (below -0.65°C). El Niño (La Niña) conditions also correspond to an increase (decrease) in cloudiness around or to the east of the international dateline (180°), with a decrease (increase) in cloudiness in the west. There is also a decrease (increase) in the trade winds in the eastern Pacific. Sub-surface temperatures in the eastern Pacific should also be warmer (colder) than average, to sustain the El Niño (La Niña) conditions.

For ENSO outlooks, information from the World Meteorological Organization (WMO) and international climate centres are assessed. The centres include the Climate Prediction Center (CPC) USA, the Bureau of Meteorology (BoM) Australia, as well as information from the International Research Institute for Climate and Society (IRI) which consolidates model outputs from other centres around the world. Each centre uses different criteria, including different SST thresholds. Therefore, variations between centres on the current ENSO state should be expected, especially when conditions are borderline.

 

The SSTs over the central and eastern Pacific were still warmer than average in March 2019 (Figure 1). These warmer temperatures over the Nino3.4 region (black box) strengthened marginally compared to February 2019, but in April 2019 (partial data available; not shown) they weakened slightly.

Sea surface temperature anomaly plot

Figure 1: Detrended SST anomalies for March 2019 with respect to 1976-2014 climatology using ERSST v5 data. Warm shades show regions of relative warming, while cool shades show regions of relative cooling. The tropical Pacific Ocean Nino3.4 Region is outlined in black.

Looking at the Nino3.4 index over the past year (Figure 2), after the 2017-2018 La Niña, the 1-month Nino3.4 value continued warming until reaching its peak in November 2018 and having crossed the El Niño threshold (0.65°C) for 2 months (October and November 2018). Subsequently the Nino3.4 value fluctuated around the threshold from December 2018 and March 2019. For El Niño conditions to be present, 1-month warm SST anomalies (observed or forecast) should persist for at least four months above the threshold, with at least one of the months observed along supporting atmospheric observations.

Observed Nino3.4 index

Figure 2: The Nino3.4 index using the 1-month SST anomalies. Warm anomalies (≥ +0.65; brown) correspond to El Niño conditions while cold anomalies (≤ -0.65; blue) correspond to La Niña conditions; otherwise neutral (> -0.65 and < +0.65; grey).

The ENSO forecasts from Copernicus C3S (Figure 3), show a wide range of forecast of Nino3.4 levels. From May 2019 onwards, while most model ensemble members show a continued increase in the Nino3.4 values, there are some members that show the warming to ease. The high degree of uncertainty is consistent with the poor predictability at this time of year for El Niño.

Forecast Nino3.4 index

Figure 3: Forecasts of Nino3.4 index’s strength for 2019 from various seasonal prediction models of international climate centres (image credit: Copernicus C3S).

Historical ENSO Variability

To classify a historical El Niño event, the 3-month average Nino3.4 value must be above 0.65°C for 5 or more consecutive months. For La Niña events, the threshold is -0.65°C. Otherwise it is considered neutral. ENSO events with a peak value above 1.5°C (El Niño) or below -1.5°C (La Niña) are considered strong. Otherwise, the events are considered weak to moderate in strength. The following figure (Figure 4) shows the development of the Nino3.4 index in 2015-18 in comparison to other El Niño/La Niña events.

Past ENSO events

Figure 4: Three-month Nino3.4 index development and retreat of different El Niño (left)/La Niña (right) events since the 1960s. The most recent El Niño and La Niña events are in red and purple, respectively.

Impact of El Niño/La Niña on Southeast Asia

Typically, the impact of El Niño on Southeast Asia is drier-than-average rainfall conditions, especially during the period June and October, and over the Maritime Continent. Warmer temperature conditions typically follow drier periods. Typically during March-May (MAM), El Niño if it occurs would be in the decay phase of its life-cycle (Figure 4). Even during the decay phase, the El Niño can bring drier conditions to the northern and eastern parts of the region (Figure 5, left). The opposite is observed during La Niña years (Figure 5, right).

The impact on the region’s rainfall and temperature from ENSO events is more significantly felt during strong or moderate intensity events. Also, no two El Niño events or two La Niña events are alike in terms of their impact.

Figure 5: March to May rainfall anomaly composites (mm/day) for El Niño (left) and La Niña (right) years. Brown shades show regions of drier conditions while regions in green shades wetter conditions. Note that this anomaly composite was generated using a limited number of El Niño/La Niña occurrences between 1979 and 2017 and therefore should be interpreted with caution (data: NOAA CPC CAMS_OPI).

References

Turkington, T., Timbal, B., & Rahmat, R. (2018). The impact of global warming on sea surface temperature based El Nino Southern Oscillation monitoring indices. International Journal of Climatology, 39(2).

El Niño/La Niña
  • For El Niño/La Niña updates, information provided by the World Meteorological Organization (WMO) and various international climate centres are assessed. The centres include the Climate Prediction Center (CPC) USA, the Bureau of Meteorology (BoM) Australia, as well as information from the International Research Institute for Climate and Society (IRI) which consolidates model outputs from various other centres around the world.