Seasonal dynamics of the marine CO2 system in Adventfjorden, a west Spitsbergen fjord
Time series of the marine CO2system and related parameters at the IsA Station, by Adventfjorden, Svalbard, were investigated between March 2015 and November 2017. The physical and biogeochemical processes that govern changes in total alkalinity (TA), total dissolved inorganic carbon (DIC) and the sa...
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Norwegian Polar Institute
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ftjpolarres:oai:journals.openacademia.net:article/3345 2024-09-09T18:55:28+00:00 Seasonal dynamics of the marine CO2 system in Adventfjorden, a west Spitsbergen fjord Ericson, Ylva Chierici, Melissa Falck, Eva Fransson, Agneta Jones, Elizabeth Kristiansen, Svein 2019-06-11 application/pdf text/html application/epub+zip text/xml https://polarresearch.net/index.php/polar/article/view/3345 https://doi.org/10.33265/polar.v38.3345 eng eng Norwegian Polar Institute https://polarresearch.net/index.php/polar/article/view/3345/9277 https://polarresearch.net/index.php/polar/article/view/3345/9279 https://polarresearch.net/index.php/polar/article/view/3345/9278 https://polarresearch.net/index.php/polar/article/view/3345/9280 https://polarresearch.net/index.php/polar/article/view/3345 doi:10.33265/polar.v38.3345 Polar Research; Vol 38 (2019) 1751-8369 marine carbonate system aragonite net community production Arctic fjord biogeochemistry Svalbard info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2019 ftjpolarres https://doi.org/10.33265/polar.v38.3345 2024-06-20T23:33:17Z Time series of the marine CO2system and related parameters at the IsA Station, by Adventfjorden, Svalbard, were investigated between March 2015 and November 2017. The physical and biogeochemical processes that govern changes in total alkalinity (TA), total dissolved inorganic carbon (DIC) and the saturation state of the calcium carbonate mineral aragonite (ΩAr) were assessed on a monthly timescale. The major driver for TA and DIC was changes in salinity, caused by river runoff, mixing and advection. This accounted for 77 and 45%, respectively, of the overall variability. It contributed minimally to the variability in ΩAr(5%); instead, biological activity was responsible for 60% of the monthly variations. For DIC, the biological activity was also important, contributing 44%. The monthly effect of air–sea CO2fluxes accounted for 11 and 15% of the total changes in DIC and ΩAr, respectively. Net community production (NCP) during the productive season ranged between 65 and 85 g C m−2, depending on the year and the presence of either Arctic water or transformed Atlantic water (TAW). The annual NCP as estimated from DIC consumption was 34 g C m−2yr−1in 2016, which was opposite in direction but similar in magnitude to the integrated annual air–sea CO2flux (i.e., uptake of carbon from the atmosphere) of −29 g C m−2yr−1for the same year. The results showed that increased intrusions of TAW into Adventfjorden in the future could possibly lower the NCP, with the potential to reduce the CO2buffer capacity and ΩArover the summer season. Article in Journal/Newspaper Adventfjorden Arctic Polar Research Svalbard Spitsbergen Polar Research Adventfjorden ENVELOPE(15.515,15.515,78.258,78.258) Arctic Svalbard Polar Research 38 0 |
institution |
Open Polar |
collection |
Polar Research |
op_collection_id |
ftjpolarres |
language |
English |
topic |
marine carbonate system aragonite net community production Arctic fjord biogeochemistry Svalbard |
spellingShingle |
marine carbonate system aragonite net community production Arctic fjord biogeochemistry Svalbard Ericson, Ylva Chierici, Melissa Falck, Eva Fransson, Agneta Jones, Elizabeth Kristiansen, Svein Seasonal dynamics of the marine CO2 system in Adventfjorden, a west Spitsbergen fjord |
topic_facet |
marine carbonate system aragonite net community production Arctic fjord biogeochemistry Svalbard |
description |
Time series of the marine CO2system and related parameters at the IsA Station, by Adventfjorden, Svalbard, were investigated between March 2015 and November 2017. The physical and biogeochemical processes that govern changes in total alkalinity (TA), total dissolved inorganic carbon (DIC) and the saturation state of the calcium carbonate mineral aragonite (ΩAr) were assessed on a monthly timescale. The major driver for TA and DIC was changes in salinity, caused by river runoff, mixing and advection. This accounted for 77 and 45%, respectively, of the overall variability. It contributed minimally to the variability in ΩAr(5%); instead, biological activity was responsible for 60% of the monthly variations. For DIC, the biological activity was also important, contributing 44%. The monthly effect of air–sea CO2fluxes accounted for 11 and 15% of the total changes in DIC and ΩAr, respectively. Net community production (NCP) during the productive season ranged between 65 and 85 g C m−2, depending on the year and the presence of either Arctic water or transformed Atlantic water (TAW). The annual NCP as estimated from DIC consumption was 34 g C m−2yr−1in 2016, which was opposite in direction but similar in magnitude to the integrated annual air–sea CO2flux (i.e., uptake of carbon from the atmosphere) of −29 g C m−2yr−1for the same year. The results showed that increased intrusions of TAW into Adventfjorden in the future could possibly lower the NCP, with the potential to reduce the CO2buffer capacity and ΩArover the summer season. |
format |
Article in Journal/Newspaper |
author |
Ericson, Ylva Chierici, Melissa Falck, Eva Fransson, Agneta Jones, Elizabeth Kristiansen, Svein |
author_facet |
Ericson, Ylva Chierici, Melissa Falck, Eva Fransson, Agneta Jones, Elizabeth Kristiansen, Svein |
author_sort |
Ericson, Ylva |
title |
Seasonal dynamics of the marine CO2 system in Adventfjorden, a west Spitsbergen fjord |
title_short |
Seasonal dynamics of the marine CO2 system in Adventfjorden, a west Spitsbergen fjord |
title_full |
Seasonal dynamics of the marine CO2 system in Adventfjorden, a west Spitsbergen fjord |
title_fullStr |
Seasonal dynamics of the marine CO2 system in Adventfjorden, a west Spitsbergen fjord |
title_full_unstemmed |
Seasonal dynamics of the marine CO2 system in Adventfjorden, a west Spitsbergen fjord |
title_sort |
seasonal dynamics of the marine co2 system in adventfjorden, a west spitsbergen fjord |
publisher |
Norwegian Polar Institute |
publishDate |
2019 |
url |
https://polarresearch.net/index.php/polar/article/view/3345 https://doi.org/10.33265/polar.v38.3345 |
long_lat |
ENVELOPE(15.515,15.515,78.258,78.258) |
geographic |
Adventfjorden Arctic Svalbard |
geographic_facet |
Adventfjorden Arctic Svalbard |
genre |
Adventfjorden Arctic Polar Research Svalbard Spitsbergen |
genre_facet |
Adventfjorden Arctic Polar Research Svalbard Spitsbergen |
op_source |
Polar Research; Vol 38 (2019) 1751-8369 |
op_relation |
https://polarresearch.net/index.php/polar/article/view/3345/9277 https://polarresearch.net/index.php/polar/article/view/3345/9279 https://polarresearch.net/index.php/polar/article/view/3345/9278 https://polarresearch.net/index.php/polar/article/view/3345/9280 https://polarresearch.net/index.php/polar/article/view/3345 doi:10.33265/polar.v38.3345 |
op_doi |
https://doi.org/10.33265/polar.v38.3345 |
container_title |
Polar Research |
container_volume |
38 |
container_issue |
0 |
_version_ |
1809902996580990976 |