Feedbacks of CaCO3 dissolution effect on ocean carbon sink and seawater acidification: a model study
The oceanic absorption of atmospheric CO _2 acidifies seawater, which accelerates CaCO _3 dissolution of calcifying organisms, a process termed dissolution effect. Promoted CaCO _3 dissolution increases seawater ALK (alkalinity), enhancing ocean carbon sink and mitigating ocean acidification. We inc...
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ftdoajarticles:oai:doaj.org/article:24e82bfd31c44af984acc75a843a23c6 2023-06-11T04:15:34+02:00 Feedbacks of CaCO3 dissolution effect on ocean carbon sink and seawater acidification: a model study Han Zhang Kuo Wang Gaofeng Fan Zhengquan Li Zhenyan Yu Jiu Jiang Tao Lian Guolin Feng 2023-01-01T00:00:00Z https://doi.org/10.1088/2515-7620/aca9ac https://doaj.org/article/24e82bfd31c44af984acc75a843a23c6 EN eng IOP Publishing https://doi.org/10.1088/2515-7620/aca9ac https://doaj.org/toc/2515-7620 doi:10.1088/2515-7620/aca9ac 2515-7620 https://doaj.org/article/24e82bfd31c44af984acc75a843a23c6 Environmental Research Communications, Vol 5, Iss 2, p 021004 (2023) CaCO3 dissolution effect ocean carbon sink ocean acidification carbon cycle modelling carbon cycle-climate feedback Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2023 ftdoajarticles https://doi.org/10.1088/2515-7620/aca9ac 2023-04-23T00:34:27Z The oceanic absorption of atmospheric CO _2 acidifies seawater, which accelerates CaCO _3 dissolution of calcifying organisms, a process termed dissolution effect. Promoted CaCO _3 dissolution increases seawater ALK (alkalinity), enhancing ocean carbon sink and mitigating ocean acidification. We incorporate different parameterizations of the link between CaCO _3 dissolution and ocean acidification into an Earth System Model, to quantify the feedback of the dissolution effect on the global carbon cycle. Under SRES A2 CO _2 emission scenario and its extension with emissions of 5,000 PgC in ∼400 years, in the absence of the dissolution effect, accumulated ocean CO _2 uptake between year 1800 and 3500 is 2,041 PgC. The consideration of the dissolution effect increases ocean carbon sink by 195–858 PgC (10%–42%), and mitigates the decrease in surface pH by 0.04–0.17 (a decrease of 10%–48% in [H ^+ ] (hydrogen ion concentration)), depending on the prescribed parameterization scheme. In the epipelagic zone, relative to the Arc-Atlantic Ocean, the Pacific-Indian Ocean experiences greater acidification, leading to greater dissolution effects and the resultant stronger feedbacks on ocean carbon sink and acidification in the Pacific-Indian Ocean. Noteworthy, the feedback of dissolution effect on ocean carbon sink can be comparable with or stronger than the feedback from CO _2 -induced radiative warming. Our study highlights the potentially critical role played by CaCO _3 dissolution effect in the ocean carbon sink, global carbon cycle and climate system. Article in Journal/Newspaper Ocean acidification Directory of Open Access Journals: DOAJ Articles Indian Pacific Environmental Research Communications 5 2 021004 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
CaCO3 dissolution effect ocean carbon sink ocean acidification carbon cycle modelling carbon cycle-climate feedback Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
spellingShingle |
CaCO3 dissolution effect ocean carbon sink ocean acidification carbon cycle modelling carbon cycle-climate feedback Environmental sciences GE1-350 Meteorology. Climatology QC851-999 Han Zhang Kuo Wang Gaofeng Fan Zhengquan Li Zhenyan Yu Jiu Jiang Tao Lian Guolin Feng Feedbacks of CaCO3 dissolution effect on ocean carbon sink and seawater acidification: a model study |
topic_facet |
CaCO3 dissolution effect ocean carbon sink ocean acidification carbon cycle modelling carbon cycle-climate feedback Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
description |
The oceanic absorption of atmospheric CO _2 acidifies seawater, which accelerates CaCO _3 dissolution of calcifying organisms, a process termed dissolution effect. Promoted CaCO _3 dissolution increases seawater ALK (alkalinity), enhancing ocean carbon sink and mitigating ocean acidification. We incorporate different parameterizations of the link between CaCO _3 dissolution and ocean acidification into an Earth System Model, to quantify the feedback of the dissolution effect on the global carbon cycle. Under SRES A2 CO _2 emission scenario and its extension with emissions of 5,000 PgC in ∼400 years, in the absence of the dissolution effect, accumulated ocean CO _2 uptake between year 1800 and 3500 is 2,041 PgC. The consideration of the dissolution effect increases ocean carbon sink by 195–858 PgC (10%–42%), and mitigates the decrease in surface pH by 0.04–0.17 (a decrease of 10%–48% in [H ^+ ] (hydrogen ion concentration)), depending on the prescribed parameterization scheme. In the epipelagic zone, relative to the Arc-Atlantic Ocean, the Pacific-Indian Ocean experiences greater acidification, leading to greater dissolution effects and the resultant stronger feedbacks on ocean carbon sink and acidification in the Pacific-Indian Ocean. Noteworthy, the feedback of dissolution effect on ocean carbon sink can be comparable with or stronger than the feedback from CO _2 -induced radiative warming. Our study highlights the potentially critical role played by CaCO _3 dissolution effect in the ocean carbon sink, global carbon cycle and climate system. |
format |
Article in Journal/Newspaper |
author |
Han Zhang Kuo Wang Gaofeng Fan Zhengquan Li Zhenyan Yu Jiu Jiang Tao Lian Guolin Feng |
author_facet |
Han Zhang Kuo Wang Gaofeng Fan Zhengquan Li Zhenyan Yu Jiu Jiang Tao Lian Guolin Feng |
author_sort |
Han Zhang |
title |
Feedbacks of CaCO3 dissolution effect on ocean carbon sink and seawater acidification: a model study |
title_short |
Feedbacks of CaCO3 dissolution effect on ocean carbon sink and seawater acidification: a model study |
title_full |
Feedbacks of CaCO3 dissolution effect on ocean carbon sink and seawater acidification: a model study |
title_fullStr |
Feedbacks of CaCO3 dissolution effect on ocean carbon sink and seawater acidification: a model study |
title_full_unstemmed |
Feedbacks of CaCO3 dissolution effect on ocean carbon sink and seawater acidification: a model study |
title_sort |
feedbacks of caco3 dissolution effect on ocean carbon sink and seawater acidification: a model study |
publisher |
IOP Publishing |
publishDate |
2023 |
url |
https://doi.org/10.1088/2515-7620/aca9ac https://doaj.org/article/24e82bfd31c44af984acc75a843a23c6 |
geographic |
Indian Pacific |
geographic_facet |
Indian Pacific |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_source |
Environmental Research Communications, Vol 5, Iss 2, p 021004 (2023) |
op_relation |
https://doi.org/10.1088/2515-7620/aca9ac https://doaj.org/toc/2515-7620 doi:10.1088/2515-7620/aca9ac 2515-7620 https://doaj.org/article/24e82bfd31c44af984acc75a843a23c6 |
op_doi |
https://doi.org/10.1088/2515-7620/aca9ac |
container_title |
Environmental Research Communications |
container_volume |
5 |
container_issue |
2 |
container_start_page |
021004 |
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1768372474859225088 |