Vertical fluxes of nitrate in the seasonal nitracline of the Atlantic sector of the Arctic Ocean

This study compiles colocated oceanic observations of high-resolution vertical profiles of nitrate concentration and turbulent microstructure around the Svalbard shelf slope, covering both the permanently ice-free Fram Strait and the pack ice north of Svalbard. The authors present an overview over t...

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Published in:Journal of Geophysical Research: Oceans
Main Authors: Randelhoff, Achim, Fer, Ilker, Sundfjord, Arild, Tremblay, Jean-Éric, Reigstad, Marit
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2017
Subjects:
Online Access:https://hdl.handle.net/1956/16267
https://doi.org/10.1002/2016jc011779
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spelling ftunivbergen:oai:bora.uib.no:1956/16267 2023-05-15T14:56:14+02:00 Vertical fluxes of nitrate in the seasonal nitracline of the Atlantic sector of the Arctic Ocean Randelhoff, Achim Fer, Ilker Sundfjord, Arild Tremblay, Jean-Éric Reigstad, Marit 2017-07-24T08:25:45Z application/pdf https://hdl.handle.net/1956/16267 https://doi.org/10.1002/2016jc011779 eng eng Wiley Norges forskningsråd: 229786 Norges forskningsråd: 226415 urn:issn:2169-9275 https://hdl.handle.net/1956/16267 https://doi.org/10.1002/2016jc011779 cristin:1380742 Copyright 2016 American Geophysical Union. All Rights Reserved Journal of Geophysical Research - Oceans Peer reviewed Journal article 2017 ftunivbergen https://doi.org/10.1002/2016jc011779 2023-03-14T17:44:04Z This study compiles colocated oceanic observations of high-resolution vertical profiles of nitrate concentration and turbulent microstructure around the Svalbard shelf slope, covering both the permanently ice-free Fram Strait and the pack ice north of Svalbard. The authors present an overview over the seasonal evolution of the distribution of nitrate and its relation to upper ocean stratification. The average upward turbulent diffusive nitrate flux across the seasonal nitracline during the Arctic summer season is derived, with average values of 0.3 and 0.7 mmol m−2 d−1 for stations with and without ice cover, respectively. The increase under ice-free conditions is attributed to different patterns of stratification under sea ice versus open water. The nitrate flux obtained from microstructure measurements lacked a seasonal signal. However, bottle incubations indicate that August nitrate uptake was reduced by more than an order of magnitude relative to the May values. It remains inconclusive whether the new production was limited by an unidentified factor other than math formula supply in late summer, or the uptake was underestimated by the incubation method. publishedVersion Article in Journal/Newspaper Arctic Arctic Ocean Fram Strait Sea ice Svalbard University of Bergen: Bergen Open Research Archive (BORA-UiB) Arctic Arctic Ocean Svalbard Journal of Geophysical Research: Oceans 121 7 5282 5295
institution Open Polar
collection University of Bergen: Bergen Open Research Archive (BORA-UiB)
op_collection_id ftunivbergen
language English
description This study compiles colocated oceanic observations of high-resolution vertical profiles of nitrate concentration and turbulent microstructure around the Svalbard shelf slope, covering both the permanently ice-free Fram Strait and the pack ice north of Svalbard. The authors present an overview over the seasonal evolution of the distribution of nitrate and its relation to upper ocean stratification. The average upward turbulent diffusive nitrate flux across the seasonal nitracline during the Arctic summer season is derived, with average values of 0.3 and 0.7 mmol m−2 d−1 for stations with and without ice cover, respectively. The increase under ice-free conditions is attributed to different patterns of stratification under sea ice versus open water. The nitrate flux obtained from microstructure measurements lacked a seasonal signal. However, bottle incubations indicate that August nitrate uptake was reduced by more than an order of magnitude relative to the May values. It remains inconclusive whether the new production was limited by an unidentified factor other than math formula supply in late summer, or the uptake was underestimated by the incubation method. publishedVersion
format Article in Journal/Newspaper
author Randelhoff, Achim
Fer, Ilker
Sundfjord, Arild
Tremblay, Jean-Éric
Reigstad, Marit
spellingShingle Randelhoff, Achim
Fer, Ilker
Sundfjord, Arild
Tremblay, Jean-Éric
Reigstad, Marit
Vertical fluxes of nitrate in the seasonal nitracline of the Atlantic sector of the Arctic Ocean
author_facet Randelhoff, Achim
Fer, Ilker
Sundfjord, Arild
Tremblay, Jean-Éric
Reigstad, Marit
author_sort Randelhoff, Achim
title Vertical fluxes of nitrate in the seasonal nitracline of the Atlantic sector of the Arctic Ocean
title_short Vertical fluxes of nitrate in the seasonal nitracline of the Atlantic sector of the Arctic Ocean
title_full Vertical fluxes of nitrate in the seasonal nitracline of the Atlantic sector of the Arctic Ocean
title_fullStr Vertical fluxes of nitrate in the seasonal nitracline of the Atlantic sector of the Arctic Ocean
title_full_unstemmed Vertical fluxes of nitrate in the seasonal nitracline of the Atlantic sector of the Arctic Ocean
title_sort vertical fluxes of nitrate in the seasonal nitracline of the atlantic sector of the arctic ocean
publisher Wiley
publishDate 2017
url https://hdl.handle.net/1956/16267
https://doi.org/10.1002/2016jc011779
geographic Arctic
Arctic Ocean
Svalbard
geographic_facet Arctic
Arctic Ocean
Svalbard
genre Arctic
Arctic Ocean
Fram Strait
Sea ice
Svalbard
genre_facet Arctic
Arctic Ocean
Fram Strait
Sea ice
Svalbard
op_source Journal of Geophysical Research - Oceans
op_relation Norges forskningsråd: 229786
Norges forskningsråd: 226415
urn:issn:2169-9275
https://hdl.handle.net/1956/16267
https://doi.org/10.1002/2016jc011779
cristin:1380742
op_rights Copyright 2016 American Geophysical Union. All Rights Reserved
op_doi https://doi.org/10.1002/2016jc011779
container_title Journal of Geophysical Research: Oceans
container_volume 121
container_issue 7
container_start_page 5282
op_container_end_page 5295
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