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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 2008temperature records for silver-lip <strong>pearl</strong> oyster farms <strong>in</strong> Western Australia ranged from ca 19– 30 °C, 21 – 31 °C and 25 – 32 °C. This implies that black <strong>pearl</strong> farms are either located <strong>in</strong>areas where the water temperature is outside the optimum temperature range or that theoptimum ranges of this species <strong>in</strong> other countries differs markedly from that <strong>in</strong> north-eastAustralia. Some of the Western Australian silver-lip <strong>pearl</strong> farms are located <strong>in</strong> areas wherethe m<strong>in</strong>imum water temperature is below the lower limit of the optimum temperature rangeor where the maximum water temperature is close to the upper limit of the optimum range.If global warm<strong>in</strong>g causes a 0.4-1.0º C <strong>in</strong>crease <strong>in</strong> the sea temperature off the north-west coastof Australia as is predicted, temperatures at some farm locations could exceed the optimaltemperature range of silver-lip oysters.Temperature probes have also been deployed at several other locations <strong>in</strong> northern Australiaand Fiji and from one location <strong>in</strong> Papua New Gu<strong>in</strong>ea. The long-term data set obta<strong>in</strong>ed froma probe deployed at one particular location <strong>in</strong> Fiji <strong>in</strong>dicates that there is considerable <strong>in</strong>terannualvariability <strong>in</strong> SST. This suggests that time series data would probably be more usefulthan average monthly SST estimates, for gaug<strong>in</strong>g prevail<strong>in</strong>g temperature regimes.The sea-level f<strong>in</strong>e resolution acoustic measur<strong>in</strong>g (SEAFRAME) gauges <strong>in</strong>stalled at s<strong>in</strong>glelocations <strong>in</strong> the Cook Islands, Fiji, Papua New Gu<strong>in</strong>ea, Solomon Islands and Vanuatu <strong>in</strong> theearly 1990s provide contemporaneous records of SST. These <strong>in</strong>dicate that the temperaturerange off Papua New Gu<strong>in</strong>ea (4.8 °C) and the Solomon Islands (5.4 °C) is narrower than thatoff the Cook Islands, Fiji and Vanuatu (8.2-8.5 °C). The records also show that mean watertemperatures off Papua New Gu<strong>in</strong>ea and the Solomon Islands were about 2° C cooler thannormal dur<strong>in</strong>g the 1997/1998 El Niño event.SST measurements derived from sensors carried on board polar-orbit<strong>in</strong>g satellites were alsoexam<strong>in</strong>ed. Comparable SST data for locations <strong>in</strong> the regions of <strong>in</strong>terest were obta<strong>in</strong>ed fromthe Modern Average Global SST Dataset produced by the US Geological Survey. These datawere derived from weekly measurements taken by an Advanced Very High ResolutionRadiometer sensor over the period October 1981 to December 1990. More recent monthlySST climatology data were obta<strong>in</strong>ed for locations around Australia by us<strong>in</strong>g the surfacetemperature search tool ma<strong>in</strong>ta<strong>in</strong>ed by the Australian Department of Defence. Time seriesdata for five locations on the north-east coast of Australia were obta<strong>in</strong>ed from the SST webatlas for the Great Barrier Reef region produced by the Australian Institute of Mar<strong>in</strong>e Scienceand CRC Reef Research Centre. Time series for five locations <strong>in</strong> Australia and two locations<strong>in</strong> the South Pacific were also obta<strong>in</strong>ed from the National Oceanic and AtmosphericAdm<strong>in</strong>istration’s Coral Reef Watch Program.The limited <strong>in</strong>formation that is available on sea temperatures <strong>in</strong> Solomon Islands <strong>in</strong>dicatesthat the prevail<strong>in</strong>g regimes are similar to those <strong>in</strong> some areas of the Cook Islands and FrenchPolynesia, where there are productive black-lip <strong>pearl</strong> farms. Similar temperature regimesalso prevail <strong>in</strong> some areas of Vanuatu, Fiji and Papua New Gu<strong>in</strong>ea. The fact that thetemperature of the water at locations <strong>in</strong> the Solomon Islands and Papua New Gu<strong>in</strong>earegularly exceeds 29 °C <strong>in</strong> summer, however, implies that these regions may be moresuitable for cultur<strong>in</strong>g silver-lip than black-lip <strong>pearl</strong> oysters. The temperature regimes atmost of the locations <strong>in</strong> Fiji and Vanuatu, <strong>in</strong> contrast, appear to be suitable for cultur<strong>in</strong>g bothspecies of <strong>pearl</strong> oysters, but silver-lip <strong>pearl</strong> oysters do not occur naturally <strong>in</strong> these waters.On the basis of our current knowledge, it is not possible to say whether the sea temperatureregime <strong>in</strong> Solomon Islands would be more advantageous for <strong>pearl</strong> farm<strong>in</strong>g than that <strong>in</strong> theother South Pacific nations considered.The Ecology Lab Pty Ltd – Mar<strong>in</strong>e and Freshwater StudiesPage ii

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