Spatial variability in surface-water p CO 2 and gas exchange in the world's largest semi-enclosed estuarine system: St. Lawrence Estuary (Canada)
The incomplete spatial coverage of CO 2 partial pressure ( p CO 2 ) measurements across estuary types represents a significant knowledge gap in current regional- and global-scale estimates of estuarine CO 2 emissions. Given the limited research on CO 2 dynamics in large estuaries and bay systems, as...
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ftdoajarticles:oai:doaj.org/article:cf1f62ba498148e3b04402926a3dab86 2023-05-15T15:53:02+02:00 Spatial variability in surface-water p CO 2 and gas exchange in the world's largest semi-enclosed estuarine system: St. Lawrence Estuary (Canada) A. Dinauer A. Mucci 2017-07-01T00:00:00Z https://doi.org/10.5194/bg-14-3221-2017 https://doaj.org/article/cf1f62ba498148e3b04402926a3dab86 EN eng Copernicus Publications https://www.biogeosciences.net/14/3221/2017/bg-14-3221-2017.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 doi:10.5194/bg-14-3221-2017 1726-4170 1726-4189 https://doaj.org/article/cf1f62ba498148e3b04402926a3dab86 Biogeosciences, Vol 14, Pp 3221-3237 (2017) Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 article 2017 ftdoajarticles https://doi.org/10.5194/bg-14-3221-2017 2022-12-31T15:02:28Z The incomplete spatial coverage of CO 2 partial pressure ( p CO 2 ) measurements across estuary types represents a significant knowledge gap in current regional- and global-scale estimates of estuarine CO 2 emissions. Given the limited research on CO 2 dynamics in large estuaries and bay systems, as well as the sources of error in the calculation of p CO 2 (carbonic acid dissociation constants, organic alkalinity), estimates of air–sea CO 2 fluxes in estuaries are subject to large uncertainties. The Estuary and Gulf of St. Lawrence (EGSL) at the lower limit of the subarctic region in eastern Canada is the world's largest estuarine system, and is characterized by an exceptional richness in environmental diversity. It is among the world's most intensively studied estuaries, yet there are no published data on its surface-water p CO 2 distribution. To fill this data gap, a comprehensive dataset was compiled from direct and indirect measurements of carbonate system parameters in the surface waters of the EGSL during the spring or summer of 2003–2016. The calculated surface-water p CO 2 ranged from 435 to 765 µatm in the shallow partially mixed upper estuary, 139–578 µatm in the deep stratified lower estuary, and 207–478 µatm along the Laurentian Channel in the Gulf of St. Lawrence. Overall, at the time of sampling, the St. Lawrence Estuary served as a very weak source of CO 2 to the atmosphere, with an area-averaged CO 2 degassing flux of 0.98 to 2.02 mmol C m −2 d −1 (0.36 to 0.74 mol C m −2 yr −1 ). A preliminary analysis revealed that respiration (upper estuary), photosynthesis (lower estuary), and temperature (Gulf of St. Lawrence) controlled the spatial variability in surface-water p CO 2 . Whereas we used the dissociation constants of Cai and Wang (1998) to calculate estuarine p CO 2 , formulations recommended for best practices in open ocean environments may underestimate p CO 2 at low salinities, while those of Millero (2010) may result in overestimates. Article in Journal/Newspaper Carbonic acid Subarctic Directory of Open Access Journals: DOAJ Articles Canada Biogeosciences 14 13 3221 3237 |
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Open Polar |
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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 A. Dinauer A. Mucci Spatial variability in surface-water p CO 2 and gas exchange in the world's largest semi-enclosed estuarine system: St. Lawrence Estuary (Canada) |
topic_facet |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 |
description |
The incomplete spatial coverage of CO 2 partial pressure ( p CO 2 ) measurements across estuary types represents a significant knowledge gap in current regional- and global-scale estimates of estuarine CO 2 emissions. Given the limited research on CO 2 dynamics in large estuaries and bay systems, as well as the sources of error in the calculation of p CO 2 (carbonic acid dissociation constants, organic alkalinity), estimates of air–sea CO 2 fluxes in estuaries are subject to large uncertainties. The Estuary and Gulf of St. Lawrence (EGSL) at the lower limit of the subarctic region in eastern Canada is the world's largest estuarine system, and is characterized by an exceptional richness in environmental diversity. It is among the world's most intensively studied estuaries, yet there are no published data on its surface-water p CO 2 distribution. To fill this data gap, a comprehensive dataset was compiled from direct and indirect measurements of carbonate system parameters in the surface waters of the EGSL during the spring or summer of 2003–2016. The calculated surface-water p CO 2 ranged from 435 to 765 µatm in the shallow partially mixed upper estuary, 139–578 µatm in the deep stratified lower estuary, and 207–478 µatm along the Laurentian Channel in the Gulf of St. Lawrence. Overall, at the time of sampling, the St. Lawrence Estuary served as a very weak source of CO 2 to the atmosphere, with an area-averaged CO 2 degassing flux of 0.98 to 2.02 mmol C m −2 d −1 (0.36 to 0.74 mol C m −2 yr −1 ). A preliminary analysis revealed that respiration (upper estuary), photosynthesis (lower estuary), and temperature (Gulf of St. Lawrence) controlled the spatial variability in surface-water p CO 2 . Whereas we used the dissociation constants of Cai and Wang (1998) to calculate estuarine p CO 2 , formulations recommended for best practices in open ocean environments may underestimate p CO 2 at low salinities, while those of Millero (2010) may result in overestimates. |
format |
Article in Journal/Newspaper |
author |
A. Dinauer A. Mucci |
author_facet |
A. Dinauer A. Mucci |
author_sort |
A. Dinauer |
title |
Spatial variability in surface-water p CO 2 and gas exchange in the world's largest semi-enclosed estuarine system: St. Lawrence Estuary (Canada) |
title_short |
Spatial variability in surface-water p CO 2 and gas exchange in the world's largest semi-enclosed estuarine system: St. Lawrence Estuary (Canada) |
title_full |
Spatial variability in surface-water p CO 2 and gas exchange in the world's largest semi-enclosed estuarine system: St. Lawrence Estuary (Canada) |
title_fullStr |
Spatial variability in surface-water p CO 2 and gas exchange in the world's largest semi-enclosed estuarine system: St. Lawrence Estuary (Canada) |
title_full_unstemmed |
Spatial variability in surface-water p CO 2 and gas exchange in the world's largest semi-enclosed estuarine system: St. Lawrence Estuary (Canada) |
title_sort |
spatial variability in surface-water p co 2 and gas exchange in the world's largest semi-enclosed estuarine system: st. lawrence estuary (canada) |
publisher |
Copernicus Publications |
publishDate |
2017 |
url |
https://doi.org/10.5194/bg-14-3221-2017 https://doaj.org/article/cf1f62ba498148e3b04402926a3dab86 |
geographic |
Canada |
geographic_facet |
Canada |
genre |
Carbonic acid Subarctic |
genre_facet |
Carbonic acid Subarctic |
op_source |
Biogeosciences, Vol 14, Pp 3221-3237 (2017) |
op_relation |
https://www.biogeosciences.net/14/3221/2017/bg-14-3221-2017.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 doi:10.5194/bg-14-3221-2017 1726-4170 1726-4189 https://doaj.org/article/cf1f62ba498148e3b04402926a3dab86 |
op_doi |
https://doi.org/10.5194/bg-14-3221-2017 |
container_title |
Biogeosciences |
container_volume |
14 |
container_issue |
13 |
container_start_page |
3221 |
op_container_end_page |
3237 |
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1766388099485532160 |