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The Occurrence and Predictability of Extreme Events over the Southwest Pacific with Particular Reference to ENSO

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Natural Disasters and Extreme Events in Agriculture

Abstract

Extreme events in the Southwest Pacific (SWP) are widespread and largely centre on tropical cyclones, droughts and floods. These events are directly influenced by the state of the El Niño Southern Oscillation (ENSO). The impacts of climate extremes are dramatic, particularly on Small Island Developing States (SIDS) of the SWP region. They cause destruction and widespread damage to human, socio, economic and development well being of local communities, examples being tropical cyclones Ofa, Val and more recently Heta, Olaf and Percy that devastated Samoa, Niue, Tonga and the Cook Islands and the severe impacts of the 1997–1998 El Niño event on Papua New Guinea and Fiji. Although warming in the SWP region is decreasing, extremes of low temperature, the trend of more El Niño episodes in the 20th century, based on observations, has increased both dry periods and extreme rainfalls in significant parts of the region, especially near the Date Line. The phase of ENSO also significantly affects temperature and rainfall anomalies and extreme across the region, with sharp gradients between contrasting areas of above and below average departures. ENSO also changes tropical cyclone track, density and occurrence, with El Niño events increasing the frequency and displacing tropical cyclones more towards the central South Pacific, and La Niña episodes decreasing the frequency and confining tracks to the west of the Date Line.

Seasonal to Inter-annual (SI) prediction has become a major research area and application tool that offers much promise for early warning and disaster preparedness to extreme events. In the SIDS of the SWP region, the Island Climate Update (ICU), a multinational virtual type regional climate prediction tool, with success hit rates (percentage of prediction being correct after comparing it with what actually happened) greater than 70 percent being achieved in some parts of the region since it was launched in September 1999, provides an extremely useful regional mechanism for preparing and predicting seasonal rainfall departures and other extreme events associated with ENSO for SIDS. The ICU could be used as a model in other regions.

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References

  • Basher RE (1998) The 1997/98 El Niño event: impacts, responses and outlook for New Zealand: a review prepared for the Ministry of Research, Science and Technology. Wellington, 28 pp.

    Google Scholar 

  • Folland CK, Renwick JA, Salinger MJ, Mullan AB (2002) Relative influences of the Interdecadal Pacific Oscillation and ENSO on the South Pacific Convergence Zone. Geophysical Research Letters 29(13): 10.1029/2001GL014201, 21-1–21-4.

    Article  Google Scholar 

  • Folland CK, Salinger, MJ, Jiang N, Rayner N (2003) Trends and variations in South Pacific island and ocean surface temperatures. Journal of Climate 16(17): 2859–2874.

    Article  Google Scholar 

  • Glantz MH, Katz RW, Nicholls N (1991) Teleconnections linking worldwide climate anomalies, Cambridge University Press, Cambridge, 535 pp.

    Google Scholar 

  • Goddard L, Mason SJ, Zebiak SE, Ropelewski CF, Basher R, Cane MA (2001). Current approaches to seasonal to inter-annual climate predictions, International Journal of Climatology 21: 1111–1152.

    Article  Google Scholar 

  • Griffiths GM, Salinger MJ, Leleu I (2003) Trends in extreme daily rainfall across the South Pacific and relationships to the SPCZ. International Journal of Climatology 23: 847–869.

    Article  Google Scholar 

  • Hamnett M, Anderson CL, Gosai, A (2002) Pacific Islands Summary. Pages 38–42 in Preparing for El Niño: Advancing regional plans and interregional communication. International Research Institute for Climate Prediction, New York, USA.

    Google Scholar 

  • Kidson JW, Renwick JA (2002) The Southern Hemisphere evolution of ENSO during 1981–1999. Journal of Climate 15: 847–863.

    Google Scholar 

  • Krishna R, Lefale PF, Sullivan M, Young E, Pilon JC, Schulz C, Clarke G, Hassett M, Power S, Prasad R, Veitch T, Turner K, Shea E, Taiki H, Brook R (2001) A needs analysis for the strengthening of Pacific Island Meteorological Services, Australian Agency for International Development (AusAID), Published by the South Pacific Regional Environment Programme (SPREP).

    Google Scholar 

  • Lefale PF, Lehodey P, Salinger MJ (2003) Impacts of ENSO on Tuna stocks and coral reefs of the Pacific Islands. NIWA Report AKL 2003-16.

    Google Scholar 

  • Lehodey P, Bertignac M, Hampton J,. Lewis, J. (1997) El Niño/Southern Oscillation and tuna in the western Pacific, Nature 389, 715–718.

    Article  Google Scholar 

  • Lightfoot C. (1999) Regional El Niño social and economic drought impact assessment and mitigation. Disaster Management Unit, South Pacific Geoscience Commission, Suva, Fiji, 39 pp.

    Google Scholar 

  • Philander SGH (1990) El Niño, La Niña, and the Southern Oscillation. Academic Press, 289 pp.

    Google Scholar 

  • Salinger MJ, Griffiths G (2001) Trends in annual New Zealand daily temperature and rainfall extremes. International Journal of Climatology 21: 1437–1452.

    Google Scholar 

  • Salinger MJ, Basher RE, Fitzharris BB, Hay JE, Jones PD, MacVeigh JP, Schmidelly-Leleu I (1995) Climate trends in the South West Pacific. International Journal of Climatology 15: 285–302.

    Google Scholar 

  • Shea EL, Dolcemascolo G, Anderson CL, Barnston A, Guard CP, Hamnett MP, Kubota ST, Lewis N, Loschnigg J, Meehl G (2001) Preparing for a changing climate: The potential consequences of climate variability and change. A report of the Pacific Islands Regional Assessment Team for the U.S. Global Change Research Program. East-West Center, 102 pp.

    Google Scholar 

  • Trenberth KE, Hoar TJ (1996) The 1990–1995 El Niño-Southern Oscillation event: longest on record, Geophysical Research Letters 23: 57–60.

    Article  Google Scholar 

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Salinger, M.J., Lefale, P. (2005). The Occurrence and Predictability of Extreme Events over the Southwest Pacific with Particular Reference to ENSO. In: Sivakumar, M.V., Motha, R.P., Das, H.P. (eds) Natural Disasters and Extreme Events in Agriculture. Springer, Berlin, Heidelberg. https://doi.org/10.1007/3-540-28307-2_3

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