Fluxes of carbon and nutrients to the Iceland Sea surface layer and inferred primary productivity and stoichiometry
This study evaluates long-term mean fluxes of carbon and nutrients to the upper 100 m of the Iceland Sea. The study utilises hydro-chemical data from the Iceland Sea time series station (68.00° N, 12.67° W), for the years between 1993 and 2006. By comparing data of dissolved inorganic carbon (DIC) a...
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2018
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Online Access: | https://hdl.handle.net/1956/18199 https://doi.org/10.5194/bg-12-875-2015 |
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ftunivbergen:oai:bora.uib.no:1956/18199 2023-05-15T16:47:31+02:00 Fluxes of carbon and nutrients to the Iceland Sea surface layer and inferred primary productivity and stoichiometry Jeansson, Emil Bellerby, Richard Skjelvan, Ingunn Frigstad, Helene Ólafsdóttir, Sólveig R. Ólafsson, Jón Hjaltalín 2018-07-02T14:29:33Z application/pdf https://hdl.handle.net/1956/18199 https://doi.org/10.5194/bg-12-875-2015 eng eng Copernicus Publications EU: 264879 EU: 264933 EU: 265294 urn:issn:1726-4170 urn:issn:1726-4189 https://hdl.handle.net/1956/18199 https://doi.org/10.5194/bg-12-875-2015 cristin:1221986 Attribution CC BY http://creativecommons.org/licenses/by/4.0 Copyright 2015 The Author(s) Biogeosciences VDP::Matematikk og naturvitenskap: 400::Zoologiske og botaniske fag: 480::Marinbiologi: 497 VDP::Mathematics and natural scienses: 400::Zoology and botany: 480::Marine biology: 497 VDP::Matematikk og naturvitenskap: 400::Geofag: 450::Oseanografi: 452 VDP::Mathematics and natural scienses: 400::Geosciences: 450::Oceanography: 452 Peer reviewed Journal article 2018 ftunivbergen https://doi.org/10.5194/bg-12-875-2015 2023-03-14T17:44:53Z This study evaluates long-term mean fluxes of carbon and nutrients to the upper 100 m of the Iceland Sea. The study utilises hydro-chemical data from the Iceland Sea time series station (68.00° N, 12.67° W), for the years between 1993 and 2006. By comparing data of dissolved inorganic carbon (DIC) and nutrients in the surface layer (upper 100 m), and a sub-surface layer (100–200 m), we calculate monthly deficits in the surface, and use these to deduce the long-term mean surface layer fluxes that affect the deficits: vertical mixing, horizontal advection, air–sea exchange, and biological activity. The deficits show a clear seasonality with a minimum in winter, when the mixed layer is at the deepest, and a maximum in early autumn, when biological uptake has removed much of the nutrients. The annual vertical fluxes of DIC and nitrate amounts to 2.9 ± 0.5 and 0.45 ± 0.09 mol m−2 yr−1, respectively, and the annual air–sea uptake of atmospheric CO2 is 4.4 ± 1.1 mol C m−2 yr−1. The biologically driven changes in DIC during the year relates to net community production (NCP), and the net annual NCP corresponds to export production, and is here calculated as 7.3 ± 1.0 mol C m−2 yr−1. The typical, median C : N ratio during the period of net community uptake is 9.0, and clearly higher than the Redfield ratio, but is varying during the season. publishedVersion Article in Journal/Newspaper Iceland University of Bergen: Bergen Open Research Archive (BORA-UiB) Biogeosciences 12 3 875 885 |
institution |
Open Polar |
collection |
University of Bergen: Bergen Open Research Archive (BORA-UiB) |
op_collection_id |
ftunivbergen |
language |
English |
topic |
VDP::Matematikk og naturvitenskap: 400::Zoologiske og botaniske fag: 480::Marinbiologi: 497 VDP::Mathematics and natural scienses: 400::Zoology and botany: 480::Marine biology: 497 VDP::Matematikk og naturvitenskap: 400::Geofag: 450::Oseanografi: 452 VDP::Mathematics and natural scienses: 400::Geosciences: 450::Oceanography: 452 |
spellingShingle |
VDP::Matematikk og naturvitenskap: 400::Zoologiske og botaniske fag: 480::Marinbiologi: 497 VDP::Mathematics and natural scienses: 400::Zoology and botany: 480::Marine biology: 497 VDP::Matematikk og naturvitenskap: 400::Geofag: 450::Oseanografi: 452 VDP::Mathematics and natural scienses: 400::Geosciences: 450::Oceanography: 452 Jeansson, Emil Bellerby, Richard Skjelvan, Ingunn Frigstad, Helene Ólafsdóttir, Sólveig R. Ólafsson, Jón Hjaltalín Fluxes of carbon and nutrients to the Iceland Sea surface layer and inferred primary productivity and stoichiometry |
topic_facet |
VDP::Matematikk og naturvitenskap: 400::Zoologiske og botaniske fag: 480::Marinbiologi: 497 VDP::Mathematics and natural scienses: 400::Zoology and botany: 480::Marine biology: 497 VDP::Matematikk og naturvitenskap: 400::Geofag: 450::Oseanografi: 452 VDP::Mathematics and natural scienses: 400::Geosciences: 450::Oceanography: 452 |
description |
This study evaluates long-term mean fluxes of carbon and nutrients to the upper 100 m of the Iceland Sea. The study utilises hydro-chemical data from the Iceland Sea time series station (68.00° N, 12.67° W), for the years between 1993 and 2006. By comparing data of dissolved inorganic carbon (DIC) and nutrients in the surface layer (upper 100 m), and a sub-surface layer (100–200 m), we calculate monthly deficits in the surface, and use these to deduce the long-term mean surface layer fluxes that affect the deficits: vertical mixing, horizontal advection, air–sea exchange, and biological activity. The deficits show a clear seasonality with a minimum in winter, when the mixed layer is at the deepest, and a maximum in early autumn, when biological uptake has removed much of the nutrients. The annual vertical fluxes of DIC and nitrate amounts to 2.9 ± 0.5 and 0.45 ± 0.09 mol m−2 yr−1, respectively, and the annual air–sea uptake of atmospheric CO2 is 4.4 ± 1.1 mol C m−2 yr−1. The biologically driven changes in DIC during the year relates to net community production (NCP), and the net annual NCP corresponds to export production, and is here calculated as 7.3 ± 1.0 mol C m−2 yr−1. The typical, median C : N ratio during the period of net community uptake is 9.0, and clearly higher than the Redfield ratio, but is varying during the season. publishedVersion |
format |
Article in Journal/Newspaper |
author |
Jeansson, Emil Bellerby, Richard Skjelvan, Ingunn Frigstad, Helene Ólafsdóttir, Sólveig R. Ólafsson, Jón Hjaltalín |
author_facet |
Jeansson, Emil Bellerby, Richard Skjelvan, Ingunn Frigstad, Helene Ólafsdóttir, Sólveig R. Ólafsson, Jón Hjaltalín |
author_sort |
Jeansson, Emil |
title |
Fluxes of carbon and nutrients to the Iceland Sea surface layer and inferred primary productivity and stoichiometry |
title_short |
Fluxes of carbon and nutrients to the Iceland Sea surface layer and inferred primary productivity and stoichiometry |
title_full |
Fluxes of carbon and nutrients to the Iceland Sea surface layer and inferred primary productivity and stoichiometry |
title_fullStr |
Fluxes of carbon and nutrients to the Iceland Sea surface layer and inferred primary productivity and stoichiometry |
title_full_unstemmed |
Fluxes of carbon and nutrients to the Iceland Sea surface layer and inferred primary productivity and stoichiometry |
title_sort |
fluxes of carbon and nutrients to the iceland sea surface layer and inferred primary productivity and stoichiometry |
publisher |
Copernicus Publications |
publishDate |
2018 |
url |
https://hdl.handle.net/1956/18199 https://doi.org/10.5194/bg-12-875-2015 |
genre |
Iceland |
genre_facet |
Iceland |
op_source |
Biogeosciences |
op_relation |
EU: 264879 EU: 264933 EU: 265294 urn:issn:1726-4170 urn:issn:1726-4189 https://hdl.handle.net/1956/18199 https://doi.org/10.5194/bg-12-875-2015 cristin:1221986 |
op_rights |
Attribution CC BY http://creativecommons.org/licenses/by/4.0 Copyright 2015 The Author(s) |
op_doi |
https://doi.org/10.5194/bg-12-875-2015 |
container_title |
Biogeosciences |
container_volume |
12 |
container_issue |
3 |
container_start_page |
875 |
op_container_end_page |
885 |
_version_ |
1766037613665320960 |