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Stimulating investment in pearl farming in ... - World Fish Center

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Water Temperature and Cyclone Frequency <strong>in</strong> the Pacific: Implications for Pearl Farm<strong>in</strong>g F<strong>in</strong>al, June 20083.3 The Influence of Climate Change on Tropical CyclonesThe effects of global warm<strong>in</strong>g on the characteristics and behaviour of tropical cyclones alsoneed to be considered. On a global scale, there is considerable uncerta<strong>in</strong>ty about the<strong>in</strong>fluence of global warm<strong>in</strong>g on cyclone frequency, but a general acceptance that tropicalcyclone <strong>in</strong>tensities will <strong>in</strong>crease. The latest report on climate change <strong>in</strong> Australia <strong>in</strong>dicatesthat there is likely to be an <strong>in</strong>crease <strong>in</strong> the proportion of the tropical cyclones <strong>in</strong> the more<strong>in</strong>tense categories, but a possible decrease <strong>in</strong> the total number of cyclones (CSIRO 2007). Thecomputer modell<strong>in</strong>g studies undertaken by Walsh et al. (2004) and Leslie et al. (2007) suggestthat there will be no significant change <strong>in</strong> the number of tropical cyclones off the east coastof Australia to the middle of the 21 st Century. The simulations made by Abbs et al. (2006),however, <strong>in</strong>dicate that there will be a significant decrease <strong>in</strong> numbers of cyclones,particularly off the west coast. All three studies agree that there will be a marked <strong>in</strong>crease <strong>in</strong>the frequency of severe tropical cyclones. The projections made by Abbs et al. (2006) andLeslie et al. (2007) suggest that cyclones will be more long-lived on the east coast. Abbs et al.(2006) <strong>in</strong>dicate that there will also be a decl<strong>in</strong>e <strong>in</strong> long-lived cyclones off the west coast.In the South Pacific region, global warm<strong>in</strong>g is predicted to have some or all of the follow<strong>in</strong>geffects on tropical cyclone activity:• Change the orig<strong>in</strong> of cyclones so that there is less cluster<strong>in</strong>g and more spread<strong>in</strong>g to theeast than at present;• Little change <strong>in</strong> total cyclone numbers or frequencies, but more storm<strong>in</strong>ess east oflongitude 180°;• Increase <strong>in</strong> the <strong>in</strong>tensity of tropical cyclones, with lower central pressure and greatermaximum w<strong>in</strong>d speeds;• Greater precipitation;• Longer cyclone lifespans;• More southerly trend <strong>in</strong> cyclone tracks; and• Longer cyclone tracks with greater southward movement prior to decay (Terry 2007).3.4 Impact of Tropical Cyclones3.4.1 General ImpactsThe gale force w<strong>in</strong>ds accompany<strong>in</strong>g cyclones can cause extensive property damage, turnairborne debris <strong>in</strong>to potentially lethal missiles, and produce heavy seas which are dangerousto vessels at sea and <strong>in</strong> harbours and cause serious erosion of foreshores (Bureau ofMeteorology, Australia 2007a). The heavy ra<strong>in</strong>fall that occurs as the cyclone passes over canproduce extensive flood<strong>in</strong>g which can <strong>in</strong> turn cause damage. Heavy ra<strong>in</strong> can persist as thecyclone moves <strong>in</strong>to central and southern parts of Australia and cause flood<strong>in</strong>g <strong>in</strong>land. Themost potentially destructive phenomena associated with tropical cyclones are storm surges,raised domes of water about 60 to 80 km across and 2 to 5 m higher than the normal tidelevel. If the arrival of a storm surge co<strong>in</strong>cides with a high tide it can cause extensive<strong>in</strong>undation of the coast, particularly <strong>in</strong> low-ly<strong>in</strong>g areas.The Ecology Lab Pty Ltd – Mar<strong>in</strong>e and Freshwater Studies Page 14

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