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pacific islands report_NU.indd - Whale and Dolphin Conservation ...

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identified as marine <strong>and</strong> coastal ecosystems,tourism assets, human settlements <strong>and</strong>infrastructure (IPCC 1998). Coupled withEl Niño, the impacts have included watershortages <strong>and</strong> drought in Papua New Guinea,the Marshall Isl<strong>and</strong>s, Federated States ofMicronesia, American Samoa, Samoa <strong>and</strong>Fiji. Current risks are likely to persist (Joneset al. 1999). Sea-level rise is obviously amajor concern for the low-lying atoll <strong>isl<strong>and</strong>s</strong>as repercussions of encroachment are alreadybeing felt (Govt of Samoa 1999, Hsu 1999,Govt of the Republic of the Marshall Isl<strong>and</strong>s2000, WWF 2003, Hunt 2002, Thaman 2002).Additional potential impacts of climate changeon the marine environment include: seatemperature rise, changes in ocean circulation,changes in salinity, ocean acidification,changes in rainfall patterns, <strong>and</strong> an increasein storm frequency (Hansen et al. 2001, IPCC2001, Sear et al. 2001, Hulme et al. 2002,ICES 2004, Bass et al. 2006). Althoughthe biological consequences of a changingclimate upon the ocean are far from beingunderstood, it is plausible there could bestrong implications in terms of nutrientavailability, biological productivity, <strong>and</strong> thestructure <strong>and</strong> functions of marine ecosystems(Gillespie 2002). In the Pacific Isl<strong>and</strong>s Regionthere have already been noted ramificationson coral reefs, tuna distribution, <strong>and</strong> mangrovesystems (Hoegh-Guldberg et al. 2000, Lehodey2001, Crosby et al. 2002, Hunt 2002, Thaman2002, UNEP 2006). These marine ecosystemimplications will be exp<strong>and</strong>ed on in the nextchapter.

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