the Archipelago, rising sea surface temperature may not be
as great a problem as it could be for more tropical reefs.
Although effects due to increasing ocean acidification are
not well understood, large carbonate deposits that exist
throughout the Archipelago may buffer the potential
impacts of slightly lower pH. Increased storminess is also
hard to predict depending on frequency, magnitude, and
location, but if larger wave events are produced, then intermediate disturbance may become more limiting to coral
development and abundance. Overall, while it may be premature to predict dire consequences for the health of coral
reefs globally, the coming century clearly contains as many
challenges as it does uncertainties.
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