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

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 quantitativel...

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Main Authors: Ron K Hoeke, Paul L Jokiel, Robert W Buddemeier, Russell E Brainard
Format: Article
Language:English
Published: Public Library of Science (PLoS) 2011-01-01
Series:PLoS ONE
Online Access:http://europepmc.org/articles/PMC3066221?pdf=render
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spelling doaj-a9debd904aa444ef8aa21591c67981bf2020-11-25T01:48:43ZengPublic Library of Science (PLoS)PLoS ONE1932-62032011-01-0163e1803810.1371/journal.pone.0018038Projected changes to growth and mortality of Hawaiian corals over the next 100 years.Ron K HoekePaul L JokielRobert W BuddemeierRussell E BrainardBACKGROUND: 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.http://europepmc.org/articles/PMC3066221?pdf=render
collection DOAJ
language English
format Article
sources DOAJ
author Ron K Hoeke
Paul L Jokiel
Robert W Buddemeier
Russell E Brainard
spellingShingle Ron K Hoeke
Paul L Jokiel
Robert W Buddemeier
Russell E Brainard
Projected changes to growth and mortality of Hawaiian corals over the next 100 years.
PLoS ONE
author_facet Ron K Hoeke
Paul L Jokiel
Robert W Buddemeier
Russell E Brainard
author_sort Ron K Hoeke
title Projected changes to growth and mortality of Hawaiian corals over the next 100 years.
title_short Projected changes to growth and mortality of Hawaiian corals over the next 100 years.
title_full Projected changes to growth and mortality of Hawaiian corals over the next 100 years.
title_fullStr Projected changes to growth and mortality of Hawaiian corals over the next 100 years.
title_full_unstemmed Projected changes to growth and mortality of Hawaiian corals over the next 100 years.
title_sort projected changes to growth and mortality of hawaiian corals over the next 100 years.
publisher Public Library of Science (PLoS)
series PLoS ONE
issn 1932-6203
publishDate 2011-01-01
description 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.
url http://europepmc.org/articles/PMC3066221?pdf=render
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