Carbon-climate feedbacks accelerate ocean acidification

We show that simulated carbon–climate feedbacks can significantly impact theonset of undersaturated aragonite conditions in the Southern and Arcticoceans, the suitable habitat for tropical coral and the deepwater saturationstates. Under the high-emissions scenarios (RCP8.5 and RCP6), thecarbon–clima...

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Published in:Biogeosciences
Main Authors: Matear, RJ, Lenton, A
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus GmbH 2018
Subjects:
Online Access:https://eprints.utas.edu.au/29965/
https://eprints.utas.edu.au/29965/1/132050%20-%20Carbon-climate%20feedbacks%20accelerate%20ocean%20acidification.pdf
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spelling ftunivtasmania:oai:eprints.utas.edu.au:29965 2023-05-15T17:49:45+02:00 Carbon-climate feedbacks accelerate ocean acidification Matear, RJ Lenton, A 2018 application/pdf https://eprints.utas.edu.au/29965/ https://eprints.utas.edu.au/29965/1/132050%20-%20Carbon-climate%20feedbacks%20accelerate%20ocean%20acidification.pdf en eng Copernicus GmbH https://eprints.utas.edu.au/29965/1/132050%20-%20Carbon-climate%20feedbacks%20accelerate%20ocean%20acidification.pdf Matear, RJ and Lenton, A 2018 , 'Carbon-climate feedbacks accelerate ocean acidification' , Biogeosciences, vol. 15, no. 6 , pp. 1721-1732 , doi:10.5194/bg-15-1721-2018 <http://dx.doi.org/10.5194/bg-15-1721-2018>. climate feedback ocean acidification CO2 concentrations Article PeerReviewed 2018 ftunivtasmania https://doi.org/10.5194/bg-15-1721-2018 2021-09-13T22:19:30Z We show that simulated carbon–climate feedbacks can significantly impact theonset of undersaturated aragonite conditions in the Southern and Arcticoceans, the suitable habitat for tropical coral and the deepwater saturationstates. Under the high-emissions scenarios (RCP8.5 and RCP6), thecarbon–climate feedbacks advance the onset of surface water under saturationand the decline in suitable coral reef habitat by a decade or more. Theimpacts of the carbon–climate feedbacks are most significant for the medium-(RCP4.5) and low-emissions (RCP2.6) scenarios. For the RCP4.5 scenario, by2100 the carbon–climate feedbacks nearly double the area of surface waterundersaturated with respect to aragonite and reduce by 50 % the surfacewater suitable for coral reefs. For the RCP2.6 scenario, by 2100 thecarbon–climate feedbacks reduce the area suitable for coral reefs by 40 %and increase the area of undersaturated surface water by 20 %. Thesensitivity of ocean acidification to the carbon–climate feedbacks in the lowto medium emission scenarios is important because recent CO2 emissionreduction commitments are trying to transition emissions to such a scenario.Our study highlights the need to better characterise the carbon–climatefeedbacks and ensure we do not underestimate the projected oceanacidification. Article in Journal/Newspaper Ocean acidification University of Tasmania: UTas ePrints Biogeosciences 15 6 1721 1732
institution Open Polar
collection University of Tasmania: UTas ePrints
op_collection_id ftunivtasmania
language English
topic climate feedback
ocean acidification
CO2 concentrations
spellingShingle climate feedback
ocean acidification
CO2 concentrations
Matear, RJ
Lenton, A
Carbon-climate feedbacks accelerate ocean acidification
topic_facet climate feedback
ocean acidification
CO2 concentrations
description We show that simulated carbon–climate feedbacks can significantly impact theonset of undersaturated aragonite conditions in the Southern and Arcticoceans, the suitable habitat for tropical coral and the deepwater saturationstates. Under the high-emissions scenarios (RCP8.5 and RCP6), thecarbon–climate feedbacks advance the onset of surface water under saturationand the decline in suitable coral reef habitat by a decade or more. Theimpacts of the carbon–climate feedbacks are most significant for the medium-(RCP4.5) and low-emissions (RCP2.6) scenarios. For the RCP4.5 scenario, by2100 the carbon–climate feedbacks nearly double the area of surface waterundersaturated with respect to aragonite and reduce by 50 % the surfacewater suitable for coral reefs. For the RCP2.6 scenario, by 2100 thecarbon–climate feedbacks reduce the area suitable for coral reefs by 40 %and increase the area of undersaturated surface water by 20 %. Thesensitivity of ocean acidification to the carbon–climate feedbacks in the lowto medium emission scenarios is important because recent CO2 emissionreduction commitments are trying to transition emissions to such a scenario.Our study highlights the need to better characterise the carbon–climatefeedbacks and ensure we do not underestimate the projected oceanacidification.
format Article in Journal/Newspaper
author Matear, RJ
Lenton, A
author_facet Matear, RJ
Lenton, A
author_sort Matear, RJ
title Carbon-climate feedbacks accelerate ocean acidification
title_short Carbon-climate feedbacks accelerate ocean acidification
title_full Carbon-climate feedbacks accelerate ocean acidification
title_fullStr Carbon-climate feedbacks accelerate ocean acidification
title_full_unstemmed Carbon-climate feedbacks accelerate ocean acidification
title_sort carbon-climate feedbacks accelerate ocean acidification
publisher Copernicus GmbH
publishDate 2018
url https://eprints.utas.edu.au/29965/
https://eprints.utas.edu.au/29965/1/132050%20-%20Carbon-climate%20feedbacks%20accelerate%20ocean%20acidification.pdf
genre Ocean acidification
genre_facet Ocean acidification
op_relation https://eprints.utas.edu.au/29965/1/132050%20-%20Carbon-climate%20feedbacks%20accelerate%20ocean%20acidification.pdf
Matear, RJ and Lenton, A 2018 , 'Carbon-climate feedbacks accelerate ocean acidification' , Biogeosciences, vol. 15, no. 6 , pp. 1721-1732 , doi:10.5194/bg-15-1721-2018 <http://dx.doi.org/10.5194/bg-15-1721-2018>.
op_doi https://doi.org/10.5194/bg-15-1721-2018
container_title Biogeosciences
container_volume 15
container_issue 6
container_start_page 1721
op_container_end_page 1732
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