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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Copernicus GmbH
2018
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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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1766156211064930304 |