A modelling study of temporal and spatial p CO 2 variability on the biologically active and temperature-dominated Scotian Shelf
Continental shelves are thought to be affected disproportionately by climate change and are a large contributor to global air–sea carbon dioxide (CO 2 ) fluxes. It is often reported that low-latitude shelves tend to act as net sources of CO 2 , whereas mid- and high-latitude shelves act as net sinks...
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Copernicus Publications
2021
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Online Access: | https://doi.org/10.5194/bg-18-6271-2021 https://doaj.org/article/4fbfb3f0a9034adfaa061f9884c12dbf |
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ftdoajarticles:oai:doaj.org/article:4fbfb3f0a9034adfaa061f9884c12dbf 2023-05-15T17:36:51+02:00 A modelling study of temporal and spatial p CO 2 variability on the biologically active and temperature-dominated Scotian Shelf K. Rutherford K. Fennel D. Atamanchuk D. Wallace H. Thomas 2021-12-01T00:00:00Z https://doi.org/10.5194/bg-18-6271-2021 https://doaj.org/article/4fbfb3f0a9034adfaa061f9884c12dbf EN eng Copernicus Publications https://bg.copernicus.org/articles/18/6271/2021/bg-18-6271-2021.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 doi:10.5194/bg-18-6271-2021 1726-4170 1726-4189 https://doaj.org/article/4fbfb3f0a9034adfaa061f9884c12dbf Biogeosciences, Vol 18, Pp 6271-6286 (2021) Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 article 2021 ftdoajarticles https://doi.org/10.5194/bg-18-6271-2021 2022-12-31T08:05:03Z Continental shelves are thought to be affected disproportionately by climate change and are a large contributor to global air–sea carbon dioxide (CO 2 ) fluxes. It is often reported that low-latitude shelves tend to act as net sources of CO 2 , whereas mid- and high-latitude shelves act as net sinks. Here, we combine a high-resolution regional model with surface water time series and repeat transect observations from the Scotian Shelf, a mid-latitude region in the northwest North Atlantic, to determine what processes are driving the temporal and spatial variability of partial pressure of CO 2 ( p CO 2 ) on a seasonal scale. In contrast to the global trend, the Scotian Shelf acts as a net source. Surface p CO 2 undergoes a strong seasonal cycle with an amplitude of ∼ 200–250 µ atm. These changes are associated with both a strong biological drawdown of dissolved inorganic carbon (DIC) in spring (corresponding to a decrease in p CO 2 of 100–200 µ atm) and pronounced effects of temperature, which ranges from 0 ∘ C in the winter to near 20 ∘ C in the summer, resulting in an increase in p CO 2 of ∼ 200–250 µ atm. Throughout the summer, events with low surface water p CO 2 occur associated with coastal upwelling. This effect of upwelling on p CO 2 is also in contrast to the general assumption that upwelling increases surface p CO 2 by delivering DIC-enriched water to the surface. Aside from these localized events, p CO 2 is relatively uniform across the shelf. Our model agrees with regional observations, reproduces seasonal patterns of p CO 2 , and simulates annual outgassing of CO 2 from the ocean of <math xmlns="http://www.w3.org/1998/Math/MathML" id="M34" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>+</mo><mn mathvariant="normal">1.7</mn><mspace linebreak="nobreak" width="0.125em"/><mo>±</mo><mspace width="0.125em" linebreak="nobreak"/><mn mathvariant="normal">0.2</mn></mrow></math> <svg:svg ... Article in Journal/Newspaper North Atlantic Directory of Open Access Journals: DOAJ Articles Biogeosciences 18 23 6271 6286 |
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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 K. Rutherford K. Fennel D. Atamanchuk D. Wallace H. Thomas A modelling study of temporal and spatial p CO 2 variability on the biologically active and temperature-dominated Scotian Shelf |
topic_facet |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 |
description |
Continental shelves are thought to be affected disproportionately by climate change and are a large contributor to global air–sea carbon dioxide (CO 2 ) fluxes. It is often reported that low-latitude shelves tend to act as net sources of CO 2 , whereas mid- and high-latitude shelves act as net sinks. Here, we combine a high-resolution regional model with surface water time series and repeat transect observations from the Scotian Shelf, a mid-latitude region in the northwest North Atlantic, to determine what processes are driving the temporal and spatial variability of partial pressure of CO 2 ( p CO 2 ) on a seasonal scale. In contrast to the global trend, the Scotian Shelf acts as a net source. Surface p CO 2 undergoes a strong seasonal cycle with an amplitude of ∼ 200–250 µ atm. These changes are associated with both a strong biological drawdown of dissolved inorganic carbon (DIC) in spring (corresponding to a decrease in p CO 2 of 100–200 µ atm) and pronounced effects of temperature, which ranges from 0 ∘ C in the winter to near 20 ∘ C in the summer, resulting in an increase in p CO 2 of ∼ 200–250 µ atm. Throughout the summer, events with low surface water p CO 2 occur associated with coastal upwelling. This effect of upwelling on p CO 2 is also in contrast to the general assumption that upwelling increases surface p CO 2 by delivering DIC-enriched water to the surface. Aside from these localized events, p CO 2 is relatively uniform across the shelf. Our model agrees with regional observations, reproduces seasonal patterns of p CO 2 , and simulates annual outgassing of CO 2 from the ocean of <math xmlns="http://www.w3.org/1998/Math/MathML" id="M34" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>+</mo><mn mathvariant="normal">1.7</mn><mspace linebreak="nobreak" width="0.125em"/><mo>±</mo><mspace width="0.125em" linebreak="nobreak"/><mn mathvariant="normal">0.2</mn></mrow></math> <svg:svg ... |
format |
Article in Journal/Newspaper |
author |
K. Rutherford K. Fennel D. Atamanchuk D. Wallace H. Thomas |
author_facet |
K. Rutherford K. Fennel D. Atamanchuk D. Wallace H. Thomas |
author_sort |
K. Rutherford |
title |
A modelling study of temporal and spatial p CO 2 variability on the biologically active and temperature-dominated Scotian Shelf |
title_short |
A modelling study of temporal and spatial p CO 2 variability on the biologically active and temperature-dominated Scotian Shelf |
title_full |
A modelling study of temporal and spatial p CO 2 variability on the biologically active and temperature-dominated Scotian Shelf |
title_fullStr |
A modelling study of temporal and spatial p CO 2 variability on the biologically active and temperature-dominated Scotian Shelf |
title_full_unstemmed |
A modelling study of temporal and spatial p CO 2 variability on the biologically active and temperature-dominated Scotian Shelf |
title_sort |
modelling study of temporal and spatial p co 2 variability on the biologically active and temperature-dominated scotian shelf |
publisher |
Copernicus Publications |
publishDate |
2021 |
url |
https://doi.org/10.5194/bg-18-6271-2021 https://doaj.org/article/4fbfb3f0a9034adfaa061f9884c12dbf |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Biogeosciences, Vol 18, Pp 6271-6286 (2021) |
op_relation |
https://bg.copernicus.org/articles/18/6271/2021/bg-18-6271-2021.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 doi:10.5194/bg-18-6271-2021 1726-4170 1726-4189 https://doaj.org/article/4fbfb3f0a9034adfaa061f9884c12dbf |
op_doi |
https://doi.org/10.5194/bg-18-6271-2021 |
container_title |
Biogeosciences |
container_volume |
18 |
container_issue |
23 |
container_start_page |
6271 |
op_container_end_page |
6286 |
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1766136468568276992 |