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Monthly climate

Climate developments in June 2003

SPCZ active with extremely high rainfall over French Polynesia
Reduced convection persists along the equator
Record low rainfall in parts of Tonga and Niue

The SPCZ was displaced further south than average east of the Date Line. As a result enhanced convection occurred over much of French Polynesia and at least 200% of average rainfall throughout much of the Society and northern Austral Islands. Rainfall totals were also enhanced, being 125% or more than average in most areas from the Solomon Islands to Tuvalu and east to the Cook Islands, as well as Pitcairn Island and much of Vanuatu. The high rainfall recorded in northern Vanuatu was largely due to tropical cyclone Gina.

An elongated region of suppressed convection persisted along the equator extending from Indonesia across to Eastern Kiribati (with rainfall totals generally less than 50% of average there) and further east. Another region of suppressed convection, with rainfall generally less than 50% of average with low totals in places, affected Fiji, Tonga and Niue. June was Niue’s third consecutive month with below average rainfall.

Air temperatures were above average over New Caledonia, Vanuatu, and the Marquesas Islands, average or below average over Fiji, and near average elsewhere.

Climate extremes in June 2003

Country Location Rainfall (mm) % of average Comments
Australia Willis Island 121 243 Well above average
French Polynesia Tahiti-Faaa 271 444 Record high
French Polynesia Tuamotu, Hereheretue 248 241 Well above average
French Polynesia Tubuai 275 267 Record High
Vanuatu Pekoa 532 338 Record high
Fiji Labasa Airport 14 21 Well below average
Fiji Savusavu Airport 25 21 Well below average
Fiji Nadi 29 45 Well below average
Fiji Penang Mill 19 19 Well below average
Niue Hanan Airport 15 20 Well below average
Tonga Lupepau’u 12 10 Record low
Tonga Fua’amotu Airport 19 18 Extremenly low
Country Location Min Air Temp (°C) Date Comments
Fiji Savusavu 25.5 4th New 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 June 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.