Island Climate Update 40 - January 2004

January

Monthly climate

ENSO & SST

Forecast validation

Three-month outlook

Feature article

Data sources

Cyclone

In this issue

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    Feature article

    Pacific Island Training Institute on Climate and Extreme Events
    The University of the South Pacific (USP), the East-West Center (EWC) and the National Institute of Water and Atmospheric Research (NIWA) will convene a two-week Pacific Island Training Institute on Climate and Extreme Events from 15–28 June 2004 at the Suva campus of the University of the South Pacific. The Asia-Pacific Network for Global Change Research (APN) and the U.S.
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    Forecast validation

    Forecast validation
    Forecast period: October to December 2003
    Average or above average rainfall was expected in Samoa. A large area of suppressed convection in the equatorial region was expected to extend south, to affect areas west of the Date Line, with below average rainfall in Western and Eastern Kiribati, and average or below average rainfall in New Caledonia, and Vanuatu, as well as the Marquesas Islands. Average rainfall was expected elsewhere in the region.
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    Cyclone

    Tropical Cyclone Update
    ‘Heta’, the first severe tropical cyclone (category 5 – most severe) of the season, originated from a disturbance north of Fiji on 28 December. It moved to develop into a tropical cyclone just west of Atafu, the northernmost part of the Tokelau Islands on 2 January.
    Heta continued to track south, passing west of Samoa on 5 January, and then southeast, with sustained winds near its centre exceeding 220 km/h.
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    ENSO & SST

    ENSO and Sea Surface Temperatures
    Pacific in a neutral ENSO state
    Westerly surface wind anomalies
    The Equatorial Pacific continues in a neutral state. Positive equatorial SSTs have eased
    recently, but are still higher than normal, especially in the west. The mean SOI for December was +0.9, and 0.0 for October–December. The NINO3 SST anomaly for December was about +0.6°C and NINO4 is around +0.9°C (3-month means are +0.7°C and +1.0°C, respectively).
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    January

    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 40 – 8 January 2004
    December’s climate: Enhanced convection was associated with the monsoon over Indonesia, northern Australia, and Papua New Guinea, which merged with the Inter-tropical convergence zone (ITCZ) north of the equator and the South Pacific Convergence Zone (SPCZ) to the southeast.
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    Monthly climate

    Climate developments in December 2003
    Active SPCZ further south than usual
    Below average rainfall persists over much of the equatorial southwest Pacific
    A large region of enhanced convection was associated with the monsoon over Indonesia, northern Australia, and Papua New Guinea. This extended east to merge with the ITCZ north of the equator and the SPCZ to the southeast.
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    Three-month outlook

    Rainfall outlook for January to March 2004
    Average or above average rainfall likely from the Solomon Islands east southeast to the Austral Islands
    Below average rainfall likely in the Marquesas Islands
    Near average rainfall elsewhere in the region
    Enhanced convection is expected in parts of the tropical Southwest Pacific resulting in average or above average rainfall from the Solomon Islands trending east to the Austral Islands, including Samoa, the Northern Cook Islands and the Society and Austral Islands.
    However, below average rainfall is expected for the Marquesas Islands.
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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