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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 2008these waters. On the basis of our current knowledge, it is not possible to say whether the seatemperature regime <strong>in</strong> Solomon Islands would be more advantageous for <strong>pearl</strong> farm<strong>in</strong>g thanthat <strong>in</strong> the other South Pacific nations considered.4.2 Risk of Damage to Pearl Farms from Tropical CyclonesAs the South Pacific region (east of 160°) usually experiences fewer tropical cyclones thanthe Australian region, the risk of damage to <strong>pearl</strong> farms and associated <strong>in</strong>frastructure is alsolikely to be smaller. The risk of cyclone damage also differs across the South Pacific region,be<strong>in</strong>g 60%, 50%, 30%, 15% and 10% for Vanuatu, Fiji, southern Cook Islands, FrenchPolynesia and the Solomon Islands, respectively (NIWA 1997). It is, however, important tonote that <strong>in</strong> a widespread nation, such as French Polynesia, the risk of cyclones varies acrossthe archipelagos and that the risk of cyclones with<strong>in</strong> the Australian/South-West PacificBas<strong>in</strong> also depends on the ENSO phenomenon. For example, dur<strong>in</strong>g El Niño years, the riskof cyclones <strong>in</strong> the Southern Cook Islands and French Polynesia <strong>in</strong>creases to 75% and 50%,respectively, rema<strong>in</strong>s at 50% <strong>in</strong> Fiji, but decreases to 40% <strong>in</strong> Vanuatu and 10% <strong>in</strong> theSolomon Islands. The risk of tropical cyclones also decl<strong>in</strong>es <strong>in</strong> the Australian region(Nicholls 1984).If the strength or frequency of El Niño events <strong>in</strong>creases, as is predicted with global warm<strong>in</strong>g,the easterly shift <strong>in</strong> tropical cyclone activity <strong>in</strong> the South Pacific region is likely to becomethe norm rather than an occasional event. Tropical cyclones are also expected to persist forlonger and travel further south before they lose energy and decay. The low-ly<strong>in</strong>g nature ofmany of the islands <strong>in</strong> the Cook Islands and French Polynesia means that they arevulnerable not only to overtopp<strong>in</strong>g by storm surges and extreme wave action generated bycyclones, but also to sea-level rise associated with global warm<strong>in</strong>g. The <strong>pearl</strong> farm<strong>in</strong>dustries <strong>in</strong> the Cook Islands and French Polynesia are both known to have been adverselyimpacted by cyclones <strong>in</strong> recent decades (Ponia et al. 2000; UNESCAP 2000). In the future,they are likely to be impacted not only by cyclone activity, but also by sea-level rise.Although impacts from cyclones are periodic, it may be wise to establish new <strong>pearl</strong> farms <strong>in</strong>nations, where the risk of damage from natural disasters and climate change is smaller.Whilst cyclones are less frequent <strong>in</strong> Solomon Islands than <strong>in</strong> most <strong>pearl</strong> farm<strong>in</strong>g areas, it isnot possible, on the basis of our current knowledge, to determ<strong>in</strong>e whether <strong>pearl</strong> farm<strong>in</strong>gwould be more advantageous there than <strong>in</strong> other South Pacific nations.Due consideration should also be given to ways of avoid<strong>in</strong>g or m<strong>in</strong>imiz<strong>in</strong>g damage to <strong>pearl</strong>farms. The development of better advance cyclone warn<strong>in</strong>g systems, for example, couldenable farmers to move longl<strong>in</strong>es <strong>in</strong>to deeper water and br<strong>in</strong>g portable equipment ashorebefore weather and sea conditions deteriorate. It may also be possible to cyclone proof subsurfacefarm <strong>in</strong>frastructure by us<strong>in</strong>g better attachments or “bunch<strong>in</strong>g up” longl<strong>in</strong>es on thelagoon floor to reduce impacts from surges.4.3 Overall ConclusionsIn the South Pacific region, the identification of potential culture sites for black-lip andsilver-<strong>pearl</strong> <strong>pearl</strong> oysters is currently h<strong>in</strong>dered by the lack of <strong>in</strong>formation on latitud<strong>in</strong>aldifferences <strong>in</strong> their optimal temperature ranges and the general lack of easily-accessible<strong>in</strong>formation on prevail<strong>in</strong>g sea temperatures. Whilst sea temperature and cyclone frequencyare important, they are only two of a range of environmental factors that could <strong>in</strong>fluenceproduction of <strong>pearl</strong> oysters. The identification of potential culture sites should also be basedon a sound knowledge of fluctuations <strong>in</strong> a number of other environmental parameters,The Ecology Lab Pty Ltd – Mar<strong>in</strong>e and Freshwater Studies Page 17

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