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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 October and will likely intensify during the next three months. El Niño has around a 100% chance of persisting during through January 2024.

The monthly NINO3.4 Index anomaly (in the central equatorial Pacific) at the end of October was +1.60˚C, within the range of a strong El Niño (classified when the NINO3.4 Index is greater than 1.5˚C). The October 2023 NINO3.4 Index is exceeded by 2015, 1997, and 1982 with data back to 1981. From an oceanic perspective, this El Niño continues to rank with the most significant events in recent decades.

The Southern Oscillation Index (SOI) was near the El Niño threshold from August-October (-0.9) but on the El Niño side of neutral territory during October (-0.4), suggestive of an El Niño event that is displaying unusual atmospheric tendencies, which is unusual considering its oceanic strength.

Trade wind strength was was below or well below normal in the Pacific during October, particularly just north of the equator. In parts of the region, this qualified as a Westerly Wind Burst (WWB). This WWB will be responsible for the eastward propagation of warm sea water along the equator through the end of the year, via an oceanic Kelvin Wave.

In the sub-surface eastern equatorial Pacific Ocean, anomalies of +3˚C to +6˚C were occurring in the upper 100 metres in the east as of late October. A new area of anomalies greater than 3˚C developed in the west-central equatorial Pacific during the month, in response to a downwelling oceanic Kelvin Wave. This will transfer ocean heat eastward on the time horizon of the next 1-2 months, lending credence to the models that suggest a peak El Niño strength in early 2024.

The associated abnormally warm water, sitting near and north of both Vanuatu and Fiji, may be a common genesis zone for tropical cyclone activity in the months ahead. Extra vigilance around early tropical cyclone activity is encouraged.

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Island Climate Update - November 2023 [PDF 5.35 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.

Development and production of the ICU is supported by NIWA Strategic Science Investment Funding under contract PRAS2301. The Island Climate Update bulletin and associated video and products are prepared as soon as possible at the start of each month. Delays in data availability occasionally arise. While every effort is made to verify the data, NIWA does not guarantee the accuracy and reliability of the analysis and forecast information presented and accepts no liability for any losses incurred through the use of this bulletin and its contents. The contents of this bulletin and all associated products produced by the Island Climate Update may be freely disseminated provided the source is acknowledged.

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Issues

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.
The NINO3.4 Index anomaly over the last month (to 3 April) was -0.79˚C, near the La Niña threshold. The March monthly Southern Oscillation Index (SOI) was +1.4, in the La Niña range.
The NINO3.4 Index anomaly (in the central Pacific) during February was -0.60˚C, near the La Niña threshold. The monthly Southern Oscillation Index (SOI) was +0.7 and the three-month average SOI was +0.8, the latter near the La Niña threshold.
The NINO3.4 Index anomaly (in the central Pacific) during January was -0.70˚C, in the La Niña range. The monthly SOI was +0.3 and the three-month average SOI was +0.9, the latter near the La Niña threshold.
The NINO3.4 Index anomaly (in the central equatorial Pacific) over the last month was -0.68˚C, near the La Niña threshold. The monthly Southern Oscillation Index (SOI) was +1.3 and the three-month average SOI was +1.0, both in the La Niña range.
The NINO3.4 Index anomaly (in the central Pacific) during November (through the 28th) was -0.59˚C and the Southern Oscillation Index (SOI) was +1.1, both near the La Niña threshold. The three month average SOI was +0.9.

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