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Tropical rainfall and SST outlook: June to August 2015

The dynamical model forecasts indicate that the central and eastern equatorial Pacific is likely to experience above normal rainfall in June – August 2015. In contrast, large regions of the southwest and southeast Pacific are expected to experience reduced rainfall, due to El Niño conditions continuing over the forecast period.

Below normal rainfall is forecast for Fiji, Tonga, Vanuatu and Papua New Guinea. Normal or below normal rainfall is forecast for the southern Cook Islands, Samoa, the Society Islands, the northern Cook Islands, the Marquesas, Niue, the Solomon Islands, Tokelau, the Tuamotu archipelago, Wallis & Futuna and New Caledonia. Above normal rainfall is forecast for western Kiribati, eastern Kiribati and Tuvalu. Normal or above normal rainfall is forecast for Pitcairn Island. No clear guidance is available this month for the Federated States of Micronesia.

The global model ensemble forecast for SSTs indicates higher than normal SSTs over the central and east equatorial Pacific, with maximum anomalies now positioned to the east of the International Dateline. Above normal SSTs are forecast for western Kiribati and eastern Kiribati. Normal or above normal SSTs are forecast for the Marquesas, the northern Cook Islands, Tokelau and Tuvalu. Normal or below normal SSTs are forecast for Fiji, Niue, Papua New Guinea, the southern Cook Islands, Tonga, Vanuatu and Wallis & Futuna.

The confidence for the rainfall outlooks is generally high. The average region-wide hit rate for rainfall forecasts issued for the June-August season is about 63%, comparable to the average for all months combined. The confidence for the SST forecasts is moderate to high. Note that climatological forecasts are typically associated with moderate confidence.

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 June-August 2015 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 June-August 2015.
SST anomaly outlook map for June-August 2015.
NOTE: Rainfall and sea surface temperature 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 June-August 2015 period.