Monthly climate

Climate developments in August 2003
Extremely dry in New Caledonia and Vanuatu
A large area of suppressed convection occurred from the Solomon Islands southward to include Vanuatu and New Caledonia, and eastward to encompass Western Kiribati, Rawaki, and Tokelau. Many sites in these areas recorded less than 25% of their normal August rainfall, especially Vanuatu and northern areas of New Caledonia where it was extremely dry and some gauges recorded totals below 10 mm.

Climate developments in August 2003

Extremely dry in New Caledonia and Vanuatu

A large area of suppressed convection occurred from the Solomon Islands southward to include Vanuatu and New Caledonia, and eastward to encompass Western Kiribati, Rawaki, and Tokelau. Many sites in these areas recorded less than 25% of their normal August rainfall, especially Vanuatu and northern areas of New Caledonia where it was extremely dry and some gauges recorded totals below 10 mm. Rainfall was also well below normal in Western Samoa, and below normal in the Caroline and Marshall Islands.

Although the South Pacific Convergence Zone (SPCZ) was near its average location west of the Date Line, it was less active than usual there. It was more active and much further south than usual in the east from southern Tonga to southern French Polynesia, with enhanced convection and rainfall at least 100% of normal over that region, including Niue and the southern Cook Islands. Rainfall was at least 200% of normal in parts of southern Tonga. Rainfall was also well above normal in Pitcairn, and isolated areas in Fiji’s Western Division. So far, the 2003 dry season (April-August) has been particularly dry over much of Kiribati, where rainfall has been 50% or less of normal.

Frequent southerly airflow kept air temperatures well below average in parts of Fiji and New Caledonia. In contrast, well above average mean air temperatures occurred in the Society Islands of French Polynesia.

Tarawa, Western Kiribati recorded its lowest frequency of easterlies (64% of observations) since January this year, and highest frequency of calms (30%) since May 2002.

Climate extremes in August 2003

Country Location Rainfall (mm) % of normal Comments
New Caledonia Koumac 5 12 Extremely low
Fiji Labasa Airport 5 11 Extremely low
Fiji Matei Airport 8 6 Extremely low
Eastern Kiribati Kanton Island 6 7 Extremely low
French Polynesia Tahiti-Faaa 8 18 Well below normal
Tonga Nuku’alofa 265 248 Well above normal
Country Location Mean Air Temp (°C) Dep. from Av Comments
New Caledonia La Roche 17.4 -1.0 Well below average
New Caledonia Ouanaham 17.9 -1.6 Extremely low
Fiji Nacocolevu 21.6 -1.1 Extremely low
Fiji Nadi 22.4 -1.3 Extremely low
Fiji Nausori 21.8 -1.1 Extremely low
Fiji Penang Mill 22.4 -1.7 Extremely low
French Polynesia Rapa Island 19.3 +1.3 Extremely high
French Polynesia Tahiti-Faaa 25.9 +1.1 Extremely high
Outgoing Long-wave Radiation (OLR) anomalies, in Wm-2 are represented by shaded areas, and rainfall percentage of average, shown by numbers. High radiation levels (yellow) are typically associated with clearer skies and lower rainfall, while cloudy conditions lower the OLR (blue) and typically mean higher rainfalls. The August 2003 position of the South Pacific Convergence Zone (SPCZ), as identified from total rainfall, is indicated by the solid green line. The average position of the SPCZ is identified by the dashed green line. Data source: NOAA-CIRES Climate Diagnostics Center.