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Projected changes to growth and mortality of Hawaiian corals over the next 100 years. | LitMetric

Projected changes to growth and mortality of Hawaiian corals over the next 100 years.

PLoS One

Joint Institute for Marine and Atmospheric Research (JIMAR), University of Hawaii, Honolulu, Hawaii, United States of America.

Published: March 2011

AI Article Synopsis

  • Recent reviews indicate that warming and acidification of ocean waters will likely cause mass mortality and decreased calcification in reef-building corals.
  • The study models changes in coral cover in the Hawaiian Archipelago from 2000 to 2099, utilizing a growth and mortality model that incorporates factors like sea surface temperature and carbon dioxide levels.
  • Highlights from the model suggest a significant decline in coral cover is probable this century, but outcomes will vary greatly in different locations and over time, influenced by uncertainties in climate predictions and coral adaptation.

Article Abstract

Background: Recent reviews suggest that the warming and acidification of ocean surface waters predicated by most accepted climate projections will lead to mass mortality and declining calcification rates of reef-building corals. This study investigates the use of modeling techniques to quantitatively examine rates of coral cover change due to these effects.

Methodology/principal Findings: Broad-scale probabilities of change in shallow-water scleractinian coral cover in the Hawaiian Archipelago for years 2000-2099 A.D. were calculated assuming a single middle-of-the-road greenhouse gas emissions scenario. These projections were based on ensemble calculations of a growth and mortality model that used sea surface temperature (SST), atmospheric carbon dioxide (CO(2)), observed coral growth (calcification) rates, and observed mortality linked to mass coral bleaching episodes as inputs. SST and CO(2) predictions were derived from the World Climate Research Programme (WCRP) multi-model dataset, statistically downscaled with historical data.

Conclusions/significance: The model calculations illustrate a practical approach to systematic evaluation of climate change effects on corals, and also show the effect of uncertainties in current climate predictions and in coral adaptation capabilities on estimated changes in coral cover. Despite these large uncertainties, this analysis quantitatively illustrates that a large decline in coral cover is highly likely in the 21(st) Century, but that there are significant spatial and temporal variances in outcomes, even under a single climate change scenario.

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Source
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC3066221PMC
http://journals.plos.org/plosone/article?id=10.1371/journal.pone.0018038PLOS

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