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Monthly climate

Climate developments in January 2003

El Niño related convection continues in the equatorial region

Suppressed convection in eastern Pacific, southeast from Papua New Guinea to New Caledonia

The SPCZ was close to its average position during January, extending southeast from Solomon Islands to Society Islands. This region merged with the Inter-Tropical Convergence Zone (ITCZ) resulting in enhanced convection over Western Kiribati and in the central equatorial Pacific just north and east of the dateline.

January rainfall was at least 180% of average (and approximately 500 mm or more at Tarawa) over the central equatorial Pacific region. Three tropical cyclones brought high rainfall events to countries which were experiencing dry conditions, i.e. New Caledonia, parts of Fiji and Tonga.

The large region of suppressed convection continues in the Indonesian region, extending to affect Papua New Guinea, northern Australia, Vanuatu and New Caledonia, where rainfall is less than 60% of average in many areas. Rainfall was also below average in parts of Fiji, Cook Island, Society Islands and Marquesas Islands.

Temperatures were generally warmer than usual with Fiji recording three new high maximum temperature records during January.

Climate extremes in January 2003

Country Location Rainfall (mm) % of average Comments
Australia Brisbane 10.0 6 Record Low
Australia Sydney 12.2 12 Extremely Low
Australia Willis Island 27.0 13 Extremely Low
New Caledonia Koumac 22.6 13 Extremely Low
Niue Hanan Airport 433.3 167 Record High
Kiribati Tarawa 501.2 179 Well above average
Fiji Ono-i-Lau 367.0 221 Extremely High
Tonga Fua’amotu Airport 413.1 203 Extremely High
French Polynesia Hereheretue 526.2 199 Extremely High
Country Location Max Air Temp (°C) Date Comments
Fiji Ono-I-Lau 33.2 10th Record High
Fiji Labasa 34.9 11th Record High
Fiji Vatukoula 37.4 12th Record High

Outgoing Long-wave Radiation (OLR) anomalies, in Wm-2 , for January 2003 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 January 2003 position of the South Pacific Convergence Zone (SPCZ), as identified from total rainfall, is indicated by the solid green line. The average climatological position of the SPCZ is identified by the dashed green line. Data source: NOAA-CIRES Climate Diagnostics Center.