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Tropical rainfall and SST outlook: September to November 2014

The dynamical models forecasts forecasts indicate that several regions of the Pacific south of the Equator are likely to receive less rainfall than normal during the September to November 2014 season.

Normal or below normal rainfall is forecast for the Marquesas, the Society Islands, Tonga, the Tuamotu archipelago, Vanuatu, the Northern Cook Islands, Fiji, New Caledonia, Tokelau, Tuvalu and Wallis & Futuna.

Normal or above normal rainfall is forecast for the Austral Islands, the Southern Cook Islands and Eastern Kiribati.

Near normal rainfall is expected for the Austral Islands and Pitcairn Island

No clear guidance is available for Western Kiribati, the Federated States of Micronesia and Niue.

The global model ensemble forecast for SSTs indicate higher than normal SSTs in the central and eastern Equatorial Pacific.

Above normal SSTs are also forecast to persist from previous months to the east of New Zealand at subtropical and mid-latitudes.

Normal or above normal SSTs are forecast for Western Kiribati and Eastern Kiribati.

Near normal SSTs are forecast for Fiji, the Marquesas, New Caledonia, the Northern and Southern Cook Islands, Pitcairn, Tokelau, the Tuamotu archipelago, Tuvalu and Vanuatu.

No guidance was available this month for the remaining regions of the southwest Pacific.

The confidence for the rainfall outlook is generally high.

Climatological probabilities for Niue, Papua New Guinea and the Tuamotu archipelago are typically associated with moderate confidence.

The average region–wide hit rate for rainfall forecasts issued in September is 66 %, two points higher than the average for all months combined.

Confidence for the SST forecasts is generally high, but many island groups are lacking strong guidance from the ensemble of models forecasts for the September – November .

The figure on the bottom right presents the last six months rainfall anomalies for each Island group alongside the latest ICU rainfall forecast for the September-November 2014 period.

The past 6 months rainfall anomalies are based on the near-real-time TRMM (Tropical Rainfall Measurement Mission) merged satellite product available from http://trmm.gsfc.nasa.gov. The data has been downloaded and available on the link below:

TRMM rainfall anomalies

For each Island group, the monthly value is derived from the average of all grid-points (or "pixels") in the TRMM Dataset that intersect a coastline, to ensure that the values correspond as closely as possible to rainfall on land, and excluding rainfall falling on ocean surfaces.

The climatology used has been established over the 2001 – 2012 period. The categories ("Well-below", "Below", etc) are determined according to the percentage of the normal rainfall for that month. The thresholds are indicated in the colorbar at the bottom: to give an example, "Well-below" normal rainfall means the rainfall for that month was under 40 % of the normal rainfall, "Below" normal rainfall means that between 40 and 80 % of normal rainfall was received, etc.

IMPORTANT NOTE:

Please note that, while we use the same color-scheme for the past rainfall anomalies and the ICU forecast, the type of information presented is different. In the case of the past 6 months, actual rainfall has been estimated by satellite, and the categories are well-defined by monthly estimated rainfall compared to the long-term mean. The ICU forecast, on the other hand, is probabilistic: it indicates the likelihood (percentage chance) of rainfall being at, above, or below normal for the season as a whole. When the percentage chances in two categories are close to each other, we indicate both categories: for example if the forecast is for 35 % chance of receiving below rainfall, and 40 % chance of normal rainfall, the outcome is "Normal or below".

Rainfall anomaly outlook map for September 2014 - November 2014
SST anomaly outlook map for September 2014 - November 2014
NOTE: Rainfall and sea surface termperature estimates for Pacific Islands for the next three months are given in the tables below. The tercile probabilities (e.g., 20:30:50) are derived from the averages of several global climate models. They correspond to the odds of the observed rainfall or sea surface temperatures being in the lowest one third of the distribution, the middle one third, or the highest one third of the distribution. For the long term average, it is equally likely (33% chance) that conditions in any of the three terciles will occur. *If conditions are climatology, we expect an equal chance of the rainfall being in any tercile.
The last six months rainfall anomalies for each Island group alongside the latest ICU rainfall forecast for the September 2014 - November 2014 period.