Island Climate Update 19 - April 2002

April

Monthly climate

ENSO & SST

Forecast validation

Three-month outlook

Feature article

Data sources

In this issue

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    April

    An overview of the present climate in the tropical South Pacific Islands, with an outlook for the coming months, to assist in dissemination of climate information in the Pacific region.
    Number 19 – 10 April 2002
    March’s Climate: An extensive area of enhanced convection occurred over equatorial waters about and west of the date line, from Papua-New Guinea to Western Kiribati, with another convective band associated with a southward displacement of the South Pacific Convergence Zone (SPCZ) extending from the northern Coral Sea southeast to affect Vanuatu and New Caledonia.
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    Feature article

    Tropical cyclones
    Summary of the year 2001/02 tropical cyclone season
    The number of Southwest Pacific tropical cyclones 2001/02 season compared to frequencies during the past 20 years - Click to enlarge
    Southwest Pacific tropical cyclone tracks: November 2001 through 31 March 2002 - Click to enlarge
    Five tropical cyclones have occurred so far this season, which is the same number as for the whole of last season and well below average (see graph below).
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    Forecast validation

    Forecast validation
    Forecast period: January to March 2002
    The SPCZ was expected to be more active than usual and also further north than average of its normal location. Rainfall was expected to be average to above average in equatorial latitudes from Western Kiribati southeast to Tonga and Niue, including Tuvalu, Wallis and Futuna, and Samoa.Average to below average rainfall was expected in Vanuatu, Eastern Kiribati, the Society Islands, and the Southern Cooks, with below average rainfall in the Marquesas.
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    ENSO & SST

    ENSO and Sea Surface TEmperatures
    Conditions are set for the development of an El Niño
    Warmer than average seas across the whole of the tropical Southwest Pacific
    The likelihood of an El Niño developing this year, based on recent observations in the equatorial Pacific, has increased. The equatorial Pacific Ocean temperatures are becoming warmer than average especially near South America where anomalies now exceed +1.0°C, The Southern Oscillation Index showed a substantial fall (to -0.8) in March, from weakly positive values over the previous two months.
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    Monthly climate

    Climate developments in March 2002
    Active convection over equatorial waters about and west of the date line
    High rainfall in parts of New Caledonia and southern French Polynesia
    Low rainfall from Tuvalu to northern French Polynesia
    An extensive area of enhanced convection occurred over equatorial waters about and west of the date line, from Papua-New Guinea to Western Kiribati, with another convective band associated with a southward displacement of the SPCZ extending from the northern Coral Sea southeast to affect Vanuatu and New Caledonia.
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    Three-month outlook

    Rainfall outlook for April to June 2002
    Above average rainfall in Kiribati and Vanuatu
    Average to below average rainfall from the Solomon Islands to the Marquesas, including the Northern Cook Islands and central French Polynesia
    The South Pacific Convergence Zone moved south in March, lying over Fiji, Tonga and the Southern Cook Islands: displaced further to the southwest than usual in areas west of the dateline. Rainfall is projected to be above average in Western and Eastern Kiribati and Vanuatu, and average to above average in New Caledonia, Fiji, Niue and Pitcairn Island.
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    Data sources

    Sources of South Pacific rainfall data
    This bulletin is a multi-national project with important collaboration from the following Pacific nations:
    American Samoa
    Australia
    Cook Islands
    Fiji
    French Polynesia
    Kiribati
    New Caledonia
    New Zealand
    Niue
    Papua New Guinea
    Pitcairn Island
    Samoa
    Solomon Islands
    Tokelau
    Tonga
    Tuvalu
    Vanuatu
    Requests for Pacific island climate data should be directed to the Meteorological Services concerned.
    Acknowledgements
    This bulletin is made possible with financial support from the New Zealand Agency for International Development (NZAID), Wellington, New Zealand, wi