Issued on Tuesday 22 May | Product Code IDCKGEWWOO
Tropical Pacific climate indicators remain in the neutral range (i.e., neither El Niño nor La Niña). This includes the Southern Oscillation Index (SOI), trade winds, cloudiness, and sea surface temperatures. Ocean temperatures below the surface are clearly warmer than average in the central and western Pacific.
Climate models surveyed by the Bureau of Meteorology indicate that the tropical Pacific Ocean is likely to warm further over the next six months. All seven models surveyed indicate conditions are likely to approach, or possibly exceed, El Niño thresholds during the second half of the year. This suggests an enhanced risk of El Niño conditions developing during 2012. No climate models favour a return to La Niña.
Model outlooks suggest the Indian Ocean Dipole (IOD) will remain neutral during the coming months.
Next update expected by 5 June 2012 | print version
Sea surface temperature (SST) in the central and eastern equatorial Pacific Ocean continued to warm during April. The SST anomaly map for April shows SSTs were near normal across most of the tropical Pacific. While still present, the area of slightly cool anomalies north of the equator has decreased substantially when compared to the map for March. Warm anomalies in the far eastern Pacific, near the equator and along the South American coast, have increased in extent and strength over the past month, with a small area of ocean more than 2 °C warmer than usual.
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The distribution of warm and cool sea-surface temperature (SST) anomalies across the tropical Pacific Ocean remains similar to that of two weeks ago, and generally has moved closer to normal values for this time of year − weak warm anomalies south of the equator in the central and eastern Pacific have decreased in extent, as have warm anomalies north of Indonesia. The SST anomaly map for the week ending 20 May shows an area of weak cool anomalies remains north of the equator in the central Pacific, although sea-surface temperatures across most of the equatorial Pacific are near average for this time of the year.
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| The four-month sequence of sub-surface Pacific Ocean equatorial temperature anomalies to 21 May shows an absence of cool anomalies in the sub-surface of the eastern Pacific and a decrease in the strength of warm anomalies in the western Pacific. Water between about 160°E and the Date Line is more than 3 °C warmer than average. |
| When compared with two weeks ago, the map for the 5 days ending 20 May shows the distribution and strength of subsurface temperature anomalies in the equatorial Pacific remains largely unchanged. Most of the water in the shallow sub-surface is slightly warmer than usual across the equatorial Pacific, with the focus of warm anomalies being somewhat deeper in the west, and slightly below average at depth. There are volumes of water more than 2 °C warmer than usual in both the western and far eastern equatorial Pacific. |
Animation of recent sub-surface changes | Archive of sub-surface temperature charts
The Southern Oscillation Index (SOI) has remained within neutral values over the past two weeks, rising to +5.5 before falling again. The latest (20 May) 30-day SOI value is +0.2.
Sustained positive values of the SOI above +8 may indicate a La Niña event, while sustained negative values below −8 may indicate an El Niño event. Values of between about +8 and −8 generally indicate neutral conditions.
Trade winds have weakened slightly over the western and central tropical Pacific during the past two weeks. Trade winds are generally near normal over the tropical Pacific, while there are westerly winds present over the Maritime Continent (see wind anomaly map for the 5 days ending 20 May).
During La Niña events, there is a sustained strengthening of the trade winds across much of the tropical Pacific, while during El Niño events there is a sustained weakening of the trade winds.
Cloudiness near the Date Line continues to fluctuate, but generally remains close to average.
Cloudiness along the equator, near the Date Line, is an important indicator of ENSO conditions, as it typically increases (negative OLR anomalies) near and to the east of the Date Line during an El Niño event and decreases (positive OLR anomalies) during a La Niña event.
While all international climate models surveyed by the Bureau indicate neutral ENSO conditions are expected for early winter, most models forecast that the Pacific is likely to reach El Niño conditions before the end of spring.
The IOD is currently neutral, with an index value of +0.6 for the week ending 20 May.
Recent forecasts from the POAMA model predict neutral IOD conditions for winter and spring.