Ocean acidification from 1997 to 2011 in the subarctic western North Pacific Ocean
Rising atmospheric CO 2 contents have led to greater CO 2 uptake by the oceans, lowering both pH due to increasing hydrogen ions and CaCO 3 saturation states due to declining carbonate ion (CO 3 2− ). Here we used previously compiled data sets and new data collected in 2010 and 2011 to investigate o...
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ftdoajarticles:oai:doaj.org/article:f276143a29ff4986a39d74231229ebd9 2023-05-15T17:50:48+02:00 Ocean acidification from 1997 to 2011 in the subarctic western North Pacific Ocean M. Wakita S. Watanabe M. Honda A. Nagano K. Kimoto K. Matsumoto M. Kitamura K. Sasaki H. Kawakami T. Fujiki K. Sasaoka Y. Nakano A. Murata 2013-12-01T00:00:00Z https://doi.org/10.5194/bg-10-7817-2013 https://doaj.org/article/f276143a29ff4986a39d74231229ebd9 EN eng Copernicus Publications http://www.biogeosciences.net/10/7817/2013/bg-10-7817-2013.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 1726-4170 1726-4189 doi:10.5194/bg-10-7817-2013 https://doaj.org/article/f276143a29ff4986a39d74231229ebd9 Biogeosciences, Vol 10, Iss 12, Pp 7817-7827 (2013) Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 article 2013 ftdoajarticles https://doi.org/10.5194/bg-10-7817-2013 2022-12-31T09:03:51Z Rising atmospheric CO 2 contents have led to greater CO 2 uptake by the oceans, lowering both pH due to increasing hydrogen ions and CaCO 3 saturation states due to declining carbonate ion (CO 3 2− ). Here we used previously compiled data sets and new data collected in 2010 and 2011 to investigate ocean acidification of the North Pacific western subarctic gyre. In winter, the western subarctic gyre is a source of CO 2 to the atmosphere because of convective mixing of deep waters rich in dissolved inorganic carbon (DIC). We calculated pH in winter mixed layer from DIC and total alkalinity (TA), and found that it decreased at the rate of −0.0011 ± 0.0004 yr −1 from 1997 to 2011. This decrease rate is slower than that expected under the condition of seawater/atmosphere equilibration, and it is also slower than the rate in the subtropical regions (−0.002 yr −1 ). The slow rate is caused by a reduction of CO 2 emission in winter due to an increase in TA. Below the mixed layer, the calcite saturation horizon (~ 185 m depth) shoaled at the rate of 2.9 ± 0.9 m yr −1 as the result of the declining CO 3 2− concentration (−0.03 ± 0.01 μmol kg −1 yr −1 ). Between 200 m and 300 m depth, pH decline during the study period (−0.0051 ± 0.0010 yr −1 ) was larger than ever reported in the open North Pacific. This enhanced acidification rate below the calcite saturation horizon reflected not only the uptake of anthropogenic CO 2 but also the increase in the decomposition of organic matter evaluated from the increase in AOU, which suggests that the dissolution of CaCO 3 particles increased. Article in Journal/Newspaper Ocean acidification Subarctic Directory of Open Access Journals: DOAJ Articles Pacific Biogeosciences 10 12 7817 7827 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 |
spellingShingle |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 M. Wakita S. Watanabe M. Honda A. Nagano K. Kimoto K. Matsumoto M. Kitamura K. Sasaki H. Kawakami T. Fujiki K. Sasaoka Y. Nakano A. Murata Ocean acidification from 1997 to 2011 in the subarctic western North Pacific Ocean |
topic_facet |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 |
description |
Rising atmospheric CO 2 contents have led to greater CO 2 uptake by the oceans, lowering both pH due to increasing hydrogen ions and CaCO 3 saturation states due to declining carbonate ion (CO 3 2− ). Here we used previously compiled data sets and new data collected in 2010 and 2011 to investigate ocean acidification of the North Pacific western subarctic gyre. In winter, the western subarctic gyre is a source of CO 2 to the atmosphere because of convective mixing of deep waters rich in dissolved inorganic carbon (DIC). We calculated pH in winter mixed layer from DIC and total alkalinity (TA), and found that it decreased at the rate of −0.0011 ± 0.0004 yr −1 from 1997 to 2011. This decrease rate is slower than that expected under the condition of seawater/atmosphere equilibration, and it is also slower than the rate in the subtropical regions (−0.002 yr −1 ). The slow rate is caused by a reduction of CO 2 emission in winter due to an increase in TA. Below the mixed layer, the calcite saturation horizon (~ 185 m depth) shoaled at the rate of 2.9 ± 0.9 m yr −1 as the result of the declining CO 3 2− concentration (−0.03 ± 0.01 μmol kg −1 yr −1 ). Between 200 m and 300 m depth, pH decline during the study period (−0.0051 ± 0.0010 yr −1 ) was larger than ever reported in the open North Pacific. This enhanced acidification rate below the calcite saturation horizon reflected not only the uptake of anthropogenic CO 2 but also the increase in the decomposition of organic matter evaluated from the increase in AOU, which suggests that the dissolution of CaCO 3 particles increased. |
format |
Article in Journal/Newspaper |
author |
M. Wakita S. Watanabe M. Honda A. Nagano K. Kimoto K. Matsumoto M. Kitamura K. Sasaki H. Kawakami T. Fujiki K. Sasaoka Y. Nakano A. Murata |
author_facet |
M. Wakita S. Watanabe M. Honda A. Nagano K. Kimoto K. Matsumoto M. Kitamura K. Sasaki H. Kawakami T. Fujiki K. Sasaoka Y. Nakano A. Murata |
author_sort |
M. Wakita |
title |
Ocean acidification from 1997 to 2011 in the subarctic western North Pacific Ocean |
title_short |
Ocean acidification from 1997 to 2011 in the subarctic western North Pacific Ocean |
title_full |
Ocean acidification from 1997 to 2011 in the subarctic western North Pacific Ocean |
title_fullStr |
Ocean acidification from 1997 to 2011 in the subarctic western North Pacific Ocean |
title_full_unstemmed |
Ocean acidification from 1997 to 2011 in the subarctic western North Pacific Ocean |
title_sort |
ocean acidification from 1997 to 2011 in the subarctic western north pacific ocean |
publisher |
Copernicus Publications |
publishDate |
2013 |
url |
https://doi.org/10.5194/bg-10-7817-2013 https://doaj.org/article/f276143a29ff4986a39d74231229ebd9 |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
Ocean acidification Subarctic |
genre_facet |
Ocean acidification Subarctic |
op_source |
Biogeosciences, Vol 10, Iss 12, Pp 7817-7827 (2013) |
op_relation |
http://www.biogeosciences.net/10/7817/2013/bg-10-7817-2013.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 1726-4170 1726-4189 doi:10.5194/bg-10-7817-2013 https://doaj.org/article/f276143a29ff4986a39d74231229ebd9 |
op_doi |
https://doi.org/10.5194/bg-10-7817-2013 |
container_title |
Biogeosciences |
container_volume |
10 |
container_issue |
12 |
container_start_page |
7817 |
op_container_end_page |
7827 |
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1766157696694747136 |