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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Published in:Biogeosciences
Main Authors: Jeansson, Emil, Bellerby, Richard, Skjelvan, Ingunn, Frigstad, Helene, Ólafsdóttir, Sólveig R., Ólafsson, Jón Hjaltalín
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2018
Subjects:
Online Access:https://hdl.handle.net/1956/18199
https://doi.org/10.5194/bg-12-875-2015
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spelling 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
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