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(PIRCA), this report - Climate Adaptation Knowledge Exchange

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Executive Summary<br />

xi<br />

• Rising ocean acidification and changing carbonate chemistry will have<br />

negative consequences for the insular and pelagic marine ecosystems; although<br />

potentially dramatic, the exact nature of the consequences is not yet clear.<br />

• Distribution patterns of coastal and ocean fisheries will be altered, with<br />

potential for increased catches in some areas and decreased catches in other<br />

areas, but open-ocean fisheries being affected negatively overall in the long<br />

term.<br />

• Increasing temperatures, and in some areas reduced rainfall, will stress<br />

native Pacific Island plant and animal populations and species, especially in<br />

high-elevation ecosystems, with increased exposure to non-native biological<br />

invasions and fire, and with extinctions a likely result.<br />

• Threats to traditional lifestyles of indigenous communities in the region<br />

(including destruction of coastal artifacts and structures, reduced availability<br />

of traditional food sources and subsistence fisheries, and the loss of the land<br />

base that supports Pacific Island cultures) will make it increasingly difficult for<br />

Pacific Island cultures to sustain their connection with a defined place and their<br />

unique set of customs, beliefs, and languages.<br />

• Mounting threats to food and water security, infrastructure, and public health<br />

and safety will lead increasingly to human migration from low islands to high<br />

islands and continental sites.<br />

This assessment also highlights the following:<br />

• The high interannual and interdecadal variability of the climate in the Pacific<br />

Islands region (e.g., ENSO, Pacific Decadal Oscillation) makes it difficult to<br />

discern long-term trends from short-term data.<br />

• Many Pacific Islands lack long-term, high-quality data on rainfall, streamflows,<br />

waves, and ecosystems, and continued monitoring is needed.<br />

• Global circulation models need to be downscaled to provide higher resolution<br />

projections for Pacific Islands to account for the influence of local topography<br />

on weather patterns and the potential impact of climate change on ecosystems.<br />

• Sea level in the Western North Pacific has risen dramatically starting in the<br />

1990s. This regional change appears to be largely wind-driven, is associated<br />

with climate variability, and is not expected to persist over time.<br />

• Some islands in the region have no human inhabitants and few human<br />

impacts, offering a relatively pristine setting in which to assess the impacts of<br />

climate change on natural settings.<br />

• Integrated biological, geochemical, and physical models are needed to improve<br />

understanding of the pressures on ecosystems and ecological responses to<br />

climate change in the Pacific Islands region.<br />

• A better understanding of how climate change affects invasive species and<br />

their interactions with native species is needed.

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