Three-month article

Rainfall outlook for August to October 2004
Above average rainfall likely in Eastern and Western Kiribati
Suppressed convection in Papua New Guinea and the Coral Sea is expected
The continuing lack of coherence between the atmosphere and the ocean in the equatorial Pacific Ocean means that the mix of global model seasonal rainfall forecast guidance is still inconsistent.

Rainfall outlook for August to October 2004

Above average rainfall likely in Eastern and Western Kiribati

Suppressed convection in Papua New Guinea and the Coral Sea is expected

The continuing lack of coherence between the atmosphere and the ocean in the equatorial Pacific Ocean means that the mix of global model seasonal rainfall forecast guidance is still inconsistent. Therefore, local climate effects are important for the upcoming three months.

Enhanced convection in the equatorial Pacific Ocean is likely to result in above average rainfall in Eastern and Western Kiribati, trending south-south east to include Tuvalu, the Cook Islands and the Austral and Tuamotu Islands of French Polynesia.

Average or below average rainfall is forecast for Papua New Guinea, New Caledonia, Vanuatu and Fiji. Rainfall is expected to be near average elsewhere in the region. The forecast model skill ranges from low to moderate at this time of year.

Rainfall outlook map for August to October 2004

Probabilities of rainfall departures from average

Broad-scale rainfall patterns and anomalies in the southern tropical Pacific area are estimated from the state of large-scale regional climate factors, such as La Niña or El Niño, their effect on the South Pacific and Tropical Convergence Zones, surface and sub-surface sea temperatures, and computer models of the global climate.

Rainfall estimates for the next three months for Pacific Islands are given in the adjacent table. The tercile probabilities (e.g. 20:30:50) are derived from the interpretation of several global climate models. They correspond to the odds of the observed rainfall being in the lowest (driest) one third of the rainfall distribution, the middle one third, or the highest (wettest) one third of the distribution. On the long-term average, rainfall is equally likely (33% chance) in any tercile.

The probabilities shown express the expected shift in the distribution from the long-term average, based on predictions of oceanic and atmospheric conditions. The amount of inter-model forecast consistency is indicated by the levels of confidence expressed in the table.

Island Group Rainfall Outlook Confidence in the Outlook
Western Kiribati 20:30:50 (Above) Moderate
Eastern Kiribati 20:30:50 (Above) Moderate
Tuvalu 20:40:40 (Average or above) Moderate
Northern Cook Islands 20:40:40 (Average or above) Low – Moderate
Southern Cook Islands 15:45:40 (Average or above) Low – Moderate
Austral Islands 20:40:40 (Average or above) Moderate
Tuamotu Islands 20:35:45 (Average or above) Low
Solomon Islands 20:50:30 (Near average) Low – Moderate
Wallis and Futuna 25:45:30 (Near average) Moderate
Tokelau 20:45:35 (Near average) Moderate
Samoa 20:50:30 (Near average) Low – Moderate
Tonga 30:50:20 (Near average) Low – Moderate
Niue 25:50:25 (Near average) Low – Moderate
Society Islands 30:50:20 (Near average) Moderate
Marquesas Islands 30:40:30 (Near average) Low
Pitcairn Island 30:50:20 (Near average) Moderate
Papua New Guinea 40:35:25 (Average or below) Moderate
Vanuatu 40:40:20 (Average or below) Low – Moderate
New Caledonia 35:40:25 (Average or below) Low – Moderate
Fiji 35:40:25 (Average or below) Low – Moderate

Rainfall outcomes as estimated from models and historical records. The third column indicates the probability of bottom (below), middle (average) or top (above) tercile rainfall, where a percentage is given. The rainfall outlook (second column) is subjectively estimated from the probabilities of bottom, middle and top terciles.