Long-term variations in ocean acidification indices in the Northwest Pacific from 1993 to 2018
Abstract Long-term variations in ocean acidification indices in the Northwest Pacific were examined using observational data and a biogeochemical model with an operational ocean model product for the period 1993–2018. The model and observational data for the surface ocean (< 100-m depth) exhi...
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2021
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crspringernat:10.1007/s10584-021-03239-1 2023-05-15T17:49:25+02:00 Long-term variations in ocean acidification indices in the Northwest Pacific from 1993 to 2018 Ishizu, Miho Miyazawa, Yasumasa Guo, Xinyu Sasakawa Peace Foundation Japan Agency for Marine-Earth Science and Technology 2021 http://dx.doi.org/10.1007/s10584-021-03239-1 https://link.springer.com/content/pdf/10.1007/s10584-021-03239-1.pdf https://link.springer.com/article/10.1007/s10584-021-03239-1/fulltext.html en eng Springer Science and Business Media LLC https://creativecommons.org/licenses/by/4.0 https://creativecommons.org/licenses/by/4.0 CC-BY Climatic Change volume 168, issue 3-4 ISSN 0165-0009 1573-1480 Atmospheric Science Global and Planetary Change journal-article 2021 crspringernat https://doi.org/10.1007/s10584-021-03239-1 2022-01-04T16:11:44Z Abstract Long-term variations in ocean acidification indices in the Northwest Pacific were examined using observational data and a biogeochemical model with an operational ocean model product for the period 1993–2018. The model and observational data for the surface ocean (< 100-m depth) exhibit consistent patterns of ocean acidification in the subtropical and Kuroshio Extension regions and relative alkalinization (i.e., reduced acidification) in the subarctic region of the Northwest Pacific. Below 100-m depth, acidification dominated in the subtropical regions and alkalinization in the subarctic regions. We attribute the excess acidification in the subtropical and Kuroshio regions to the vertical mixing of dissolved inorganic carbon (DIC) exceeding the DIC release by air–sea exchange. These regional differences in acidification and alkalinization are attributed to spatially variable biological processes in the upper ocean and horizontal and vertical physical redistribution of DIC. Our model and observational results have implications for the spatial extent and pattern of ocean acidification, along with the strength of the ocean carbon sink, which are key aspects of global climate change. Article in Journal/Newspaper Ocean acidification Subarctic Springer Nature (via Crossref) Pacific Climatic Change 168 3-4 |
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Open Polar |
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Springer Nature (via Crossref) |
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crspringernat |
language |
English |
topic |
Atmospheric Science Global and Planetary Change |
spellingShingle |
Atmospheric Science Global and Planetary Change Ishizu, Miho Miyazawa, Yasumasa Guo, Xinyu Long-term variations in ocean acidification indices in the Northwest Pacific from 1993 to 2018 |
topic_facet |
Atmospheric Science Global and Planetary Change |
description |
Abstract Long-term variations in ocean acidification indices in the Northwest Pacific were examined using observational data and a biogeochemical model with an operational ocean model product for the period 1993–2018. The model and observational data for the surface ocean (< 100-m depth) exhibit consistent patterns of ocean acidification in the subtropical and Kuroshio Extension regions and relative alkalinization (i.e., reduced acidification) in the subarctic region of the Northwest Pacific. Below 100-m depth, acidification dominated in the subtropical regions and alkalinization in the subarctic regions. We attribute the excess acidification in the subtropical and Kuroshio regions to the vertical mixing of dissolved inorganic carbon (DIC) exceeding the DIC release by air–sea exchange. These regional differences in acidification and alkalinization are attributed to spatially variable biological processes in the upper ocean and horizontal and vertical physical redistribution of DIC. Our model and observational results have implications for the spatial extent and pattern of ocean acidification, along with the strength of the ocean carbon sink, which are key aspects of global climate change. |
author2 |
Sasakawa Peace Foundation Japan Agency for Marine-Earth Science and Technology |
format |
Article in Journal/Newspaper |
author |
Ishizu, Miho Miyazawa, Yasumasa Guo, Xinyu |
author_facet |
Ishizu, Miho Miyazawa, Yasumasa Guo, Xinyu |
author_sort |
Ishizu, Miho |
title |
Long-term variations in ocean acidification indices in the Northwest Pacific from 1993 to 2018 |
title_short |
Long-term variations in ocean acidification indices in the Northwest Pacific from 1993 to 2018 |
title_full |
Long-term variations in ocean acidification indices in the Northwest Pacific from 1993 to 2018 |
title_fullStr |
Long-term variations in ocean acidification indices in the Northwest Pacific from 1993 to 2018 |
title_full_unstemmed |
Long-term variations in ocean acidification indices in the Northwest Pacific from 1993 to 2018 |
title_sort |
long-term variations in ocean acidification indices in the northwest pacific from 1993 to 2018 |
publisher |
Springer Science and Business Media LLC |
publishDate |
2021 |
url |
http://dx.doi.org/10.1007/s10584-021-03239-1 https://link.springer.com/content/pdf/10.1007/s10584-021-03239-1.pdf https://link.springer.com/article/10.1007/s10584-021-03239-1/fulltext.html |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
Ocean acidification Subarctic |
genre_facet |
Ocean acidification Subarctic |
op_source |
Climatic Change volume 168, issue 3-4 ISSN 0165-0009 1573-1480 |
op_rights |
https://creativecommons.org/licenses/by/4.0 https://creativecommons.org/licenses/by/4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1007/s10584-021-03239-1 |
container_title |
Climatic Change |
container_volume |
168 |
container_issue |
3-4 |
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1766155750506233856 |