High‐frequency variability of small‐particle carbon export flux in the Northeast Atlantic

The biological carbon pump exports carbon fixed by photosynthesis out of the surface ocean and transfers it to the deep, mostly in the form of sinking particles. Despite the importance of the pump in regulating the air‐sea CO2 balance, the magnitude of global carbon export remains unclear, as do its...

Full description

Bibliographic Details
Published in:Global Biogeochemical Cycles
Main Authors: Bol, Roséanne, Henson, Stephanie, Anne, Rumyantseva, Anna, Briggs, Nathan
Format: Article in Journal/Newspaper
Language:English
Published: 2018
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/522078/
https://nora.nerc.ac.uk/id/eprint/522078/1/Bol_et_al-2018-Global_Biogeochemical_Cycles.pdf
https://doi.org/10.1029/2018GB005963
id ftnerc:oai:nora.nerc.ac.uk:522078
record_format openpolar
spelling ftnerc:oai:nora.nerc.ac.uk:522078 2023-05-15T17:41:17+02:00 High‐frequency variability of small‐particle carbon export flux in the Northeast Atlantic Bol, Roséanne Henson, Stephanie, Anne Rumyantseva, Anna Briggs, Nathan 2018 text http://nora.nerc.ac.uk/id/eprint/522078/ https://nora.nerc.ac.uk/id/eprint/522078/1/Bol_et_al-2018-Global_Biogeochemical_Cycles.pdf https://doi.org/10.1029/2018GB005963 en eng https://nora.nerc.ac.uk/id/eprint/522078/1/Bol_et_al-2018-Global_Biogeochemical_Cycles.pdf Bol, Roséanne; Henson, Stephanie, Anne orcid:0000-0002-3875-6802 Rumyantseva, Anna; Briggs, Nathan orcid:0000-0003-1549-1386 . 2018 High‐frequency variability of small‐particle carbon export flux in the Northeast Atlantic. Global Biogeochemical Cycles, 32 (12). 1803-1814. https://doi.org/10.1029/2018GB005963 <https://doi.org/10.1029/2018GB005963> cc_by_4 CC-BY Publication - Article PeerReviewed 2018 ftnerc https://doi.org/10.1029/2018GB005963 2023-02-04T19:47:42Z The biological carbon pump exports carbon fixed by photosynthesis out of the surface ocean and transfers it to the deep, mostly in the form of sinking particles. Despite the importance of the pump in regulating the air‐sea CO2 balance, the magnitude of global carbon export remains unclear, as do its controlling mechanisms. A possible sinking flux of carbon to the mesopelagic zone may be via the mixed‐layer pump: a seasonal net detrainment of particulate organic carbon (POC)‐rich surface waters, caused by sequential deepening and shoaling of the mixed layer. In this study, we present a full year of daily small‐particle POC concentrations derived from glider optical backscatter data, to study export variability at the Porcupine Abyssal Plain (PAP) sustained observatory in the Northeast Atlantic. We observe a strong seasonality in small‐particle transfer efficiency, with a maximum in winter and early spring. By calculating daily POC export driven by mixed‐layer variations, we find that the mixed‐layer pump supplies an annual flux of at least 3.0 ± 0.9 g POC·m−2·year−1 to the mesopelagic zone, contributing between 5% and 25% of the total annual export flux and likely contributing to closing a gap in the mesopelagic carbon budget found by other studies. These are, to our best knowledge, the first high‐frequency observations of export variability over the course of a full year. Our results support the deployment of bio‐optical sensors on gliders to improve our understanding of the ocean carbon cycle on temporal scales from daily to annual. Article in Journal/Newspaper Northeast Atlantic Natural Environment Research Council: NERC Open Research Archive Global Biogeochemical Cycles 32 12 1803 1814
institution Open Polar
collection Natural Environment Research Council: NERC Open Research Archive
op_collection_id ftnerc
language English
description The biological carbon pump exports carbon fixed by photosynthesis out of the surface ocean and transfers it to the deep, mostly in the form of sinking particles. Despite the importance of the pump in regulating the air‐sea CO2 balance, the magnitude of global carbon export remains unclear, as do its controlling mechanisms. A possible sinking flux of carbon to the mesopelagic zone may be via the mixed‐layer pump: a seasonal net detrainment of particulate organic carbon (POC)‐rich surface waters, caused by sequential deepening and shoaling of the mixed layer. In this study, we present a full year of daily small‐particle POC concentrations derived from glider optical backscatter data, to study export variability at the Porcupine Abyssal Plain (PAP) sustained observatory in the Northeast Atlantic. We observe a strong seasonality in small‐particle transfer efficiency, with a maximum in winter and early spring. By calculating daily POC export driven by mixed‐layer variations, we find that the mixed‐layer pump supplies an annual flux of at least 3.0 ± 0.9 g POC·m−2·year−1 to the mesopelagic zone, contributing between 5% and 25% of the total annual export flux and likely contributing to closing a gap in the mesopelagic carbon budget found by other studies. These are, to our best knowledge, the first high‐frequency observations of export variability over the course of a full year. Our results support the deployment of bio‐optical sensors on gliders to improve our understanding of the ocean carbon cycle on temporal scales from daily to annual.
format Article in Journal/Newspaper
author Bol, Roséanne
Henson, Stephanie, Anne
Rumyantseva, Anna
Briggs, Nathan
spellingShingle Bol, Roséanne
Henson, Stephanie, Anne
Rumyantseva, Anna
Briggs, Nathan
High‐frequency variability of small‐particle carbon export flux in the Northeast Atlantic
author_facet Bol, Roséanne
Henson, Stephanie, Anne
Rumyantseva, Anna
Briggs, Nathan
author_sort Bol, Roséanne
title High‐frequency variability of small‐particle carbon export flux in the Northeast Atlantic
title_short High‐frequency variability of small‐particle carbon export flux in the Northeast Atlantic
title_full High‐frequency variability of small‐particle carbon export flux in the Northeast Atlantic
title_fullStr High‐frequency variability of small‐particle carbon export flux in the Northeast Atlantic
title_full_unstemmed High‐frequency variability of small‐particle carbon export flux in the Northeast Atlantic
title_sort high‐frequency variability of small‐particle carbon export flux in the northeast atlantic
publishDate 2018
url http://nora.nerc.ac.uk/id/eprint/522078/
https://nora.nerc.ac.uk/id/eprint/522078/1/Bol_et_al-2018-Global_Biogeochemical_Cycles.pdf
https://doi.org/10.1029/2018GB005963
genre Northeast Atlantic
genre_facet Northeast Atlantic
op_relation https://nora.nerc.ac.uk/id/eprint/522078/1/Bol_et_al-2018-Global_Biogeochemical_Cycles.pdf
Bol, Roséanne; Henson, Stephanie, Anne orcid:0000-0002-3875-6802
Rumyantseva, Anna; Briggs, Nathan orcid:0000-0003-1549-1386 . 2018 High‐frequency variability of small‐particle carbon export flux in the Northeast Atlantic. Global Biogeochemical Cycles, 32 (12). 1803-1814. https://doi.org/10.1029/2018GB005963 <https://doi.org/10.1029/2018GB005963>
op_rights cc_by_4
op_rightsnorm CC-BY
op_doi https://doi.org/10.1029/2018GB005963
container_title Global Biogeochemical Cycles
container_volume 32
container_issue 12
container_start_page 1803
op_container_end_page 1814
_version_ 1766142766411153408