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Island Climate Update

A summary of the climate across the islands of Te Moana-niu-a-kiwa (Pacific Ocean), with an outlook for the coming months.

El Niño continued during March but continues to weaken. ENSO neutral conditions are favoured to develop by June 2024.

The monthly NINO3.4 Index anomaly (in the central equatorial Pacific) at the end of March was +1.24˚C, remaining within the El Niño range. Oceanic El Niño has weakened by about 0.55˚C since January.

The Southern Oscillation Index (SOI) was in the neutral range during March (+0.1) and January-March (-0.2).

Trade wind strength was well above normal near and west of the International Date Line during March. This generated an upwelling Kelvin Wave in the west-central equatorial Pacific, which should see cooler than average sub-surface ocean water move across the Pacific over the next two months.

Enhanced trade winds are forecast to continue near the International Date Line during April, which should result in additional oceanic cooling.

At the end of March, the subsurface equatorial Pacific was cooler than average across most of the basin below 100 m depth, with below average temperatures moving closer to the surface in the east during March. Notably, subsurface waters were 3˚C to 5˚C below average in the east, lending credence to the eventual development of La Niña later this year.

During March, convective forcing favoured the western Pacific with subsidence over the eastern Pacific and South America, a La Niña-like pattern. This was linked to a strong, early-month pulse of the Madden-Julian Oscillation (MJO) as well as a South Pacific Convergence Zone that was displaced well south-west of its climatological position. This delivered excessive rainfall to Vanuatu, Fiji, and parts of Tonga during the month. By late March, the pulse had propagated into the eastern Pacific, generating an El Niño-like response. Such variability is to be expected from an ocean-atmosphere system that is transitioning toward an ENSO-neutral state.

The tropical cyclone season continues through April. Activity looks unlikely through the first half of the month.

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Island Climate Update - April 2024 [5.5 MB]

Additional resources

Additional regional and country situation summary and forecast information can be obtained below. Current rainfall accumulation status and other derived summary information are updated on a daily basis (with a 2-day lag), with seasonal forecast information updated once per month.

 

About the Island Climate Update

NIWA is the Network co-lead for the WMO RA V Regional Climate Centre Node on Long Range Forecast and consortium member for nodes on Climate Monitoring, Operational Data Services and Training.

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Issues

El Niño continued during March but continues to weaken. ENSO neutral conditions are favoured to develop by June 2024.
The El Niño event is now past its peak oceanic intensity and it is likely to weaken further during March.
El Niño was active during January and will very likely continue over the next three months.
El Niño continued during December and has around a 100% chance of persisting through March.
El Niño continued during November and will likely remain in place during the next three months. El Niño has around a 100% chance of persisting through February 2024.
El Niño continued during October and will likely intensify during the next three months.
El Niño has officially arrived. A majority of NIWA’s criteria for classifying an El Niño event were satisfied during September.
The monthly NINO3.4 Index anomaly (in the central equatorial Pacific) at the end of August was +1.34˚C. The weekly value reached +1.5˚C at the end of the month – the traditional threshold for a strong oceanic El Niño.
The monthly NINO3.4 Index anomaly (in the central equatorial Pacific) at the end of July was 1.11 ˚C . At the same point during the developmental phase of strong past El Niño events , it was +1.35˚C in 2015, +1.31˚C in 1997, and +0.26˚C in 1982.
The monthly NINO3.4 Index anomaly (in the central equatorial Pacific) at the end of June was +0.93˚C. This is warmer than it was at the same time during the development of strong El Niño events in 1997 and 1982.
The monthly NINO3.4 Index anomaly (in the central equatorial Pacific) at the end of May was 0.49˚C, an increase of nearly 0.3˚C from April and trending toward NIWA’s El Niño threshold of 0.7˚C.
The monthly NINO3.4 Index anomaly (in the central equatorial Pacific) at the beginning of May was 0.21˚C, in the neutral range, but gradually warming.
The monthly NINO3.4 Index anomaly (in the central equatorial Pacific) at the end of March was -0.01˚C, in the neutral range for the second consecutive month.
The monthly NINO3.4 Index anomaly (in the central equatorial Pacific) at the end of February was -0.47˚C, in neutral territory for the first time since July-August 2022.
The NINO3.4 Index anomaly (in the central equatorial Pacific) over the last month was -0.69˚C, close to La Niña thresholds.
The NINO3.4 Index anomaly (in the central equatorial Pacific) over the last month was -0.83˚C (climatology: 1991-2020), showing a slight warming trend compared to November.
The NINO3.4 Index anomaly (in the central equatorial Pacific) over the last month was 0.92˚C (climatology: 1991 2020), showing a cooling trend compared to October.
The NINO3.4 Index anomaly (in the central equatorial Pacific) over the last month was -0.80˚C (climatology: 1991-2020), in the La Niña range for the third consecutive month.
The NINO3.4 Index anomaly (in the central equatorial Pacific) over the last month (through 30 September) was -0.93˚C (climatology: 1991-2020). In the last four decades, only four Septembers hadcooler central equatorial Pacific SSTs than 2022, including September 2010, 1999, 1998, and 1988.
The NINO3.4 Index anomaly (in the central equatorial Pacific) over the last month (through 31 August) was -1.00˚C (climatology: 1991-2020), showing a strong cooling trend compared to July. In the last four decades, only four Augusts had cooler central equatorial Pacific SSTs than 2022, including August 2010, 1999, 1998, and 1988.
The NINO3.4 Index anomaly (in the central equatorial Pacific) over the last month (through 31 July) was -0.34˚C (climatology: 1961-1990); the latest weekly anomaly was -0.43˚C, showing a late-month cooling trend.
The NINO3.4 Index anomaly (in the central equatorial Pacific) over the last month was -0.40˚C, in the “cool-neutral range”. The three-monthly NINO3.4 Index remained near the La Niña threshold.
The NINO3.4 Index anomaly over the last month (to 5 June) was 0.71˚C, near the La Niña threshold and a slight decrease compared to April.
The NINO3.4 Index anomaly over the last month (to 1 May) was -0.66˚C, an increase compared to the previous month but still near the La Niña threshold.

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