Spatiotemporal variability of barium in Arctic sea-ice and seawater

Freshwater export from the Arctic is critical in determining the density of water at sites of North Atlantic deep water formation, which in turn influences the global flux of oceanic heat and nutrients. We need geochemical tracers and high-resolution observations to refine our freshwater budgets and...

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Main Authors: Hendry, Katharine R., Pyle, Kimberley M., Butler, G. Barney, Cooper, Adam, Fransson, Agneta, Chierici, Melissa, Leng, Melanie J., Meyer, Amelie, Dodd, Paul A.
Format: Article
Language:English
Published: American Geophysical Union 2018
Online Access:https://eprints.nottingham.ac.uk/51688/
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author Hendry, Katharine R.
Pyle, Kimberley M.
Butler, G. Barney
Cooper, Adam
Fransson, Agneta
Chierici, Melissa
Leng, Melanie J.
Meyer, Amelie
Dodd, Paul A.
author_facet Hendry, Katharine R.
Pyle, Kimberley M.
Butler, G. Barney
Cooper, Adam
Fransson, Agneta
Chierici, Melissa
Leng, Melanie J.
Meyer, Amelie
Dodd, Paul A.
author_sort Hendry, Katharine R.
building Nottingham Research Data Repository
collection Online Access
description Freshwater export from the Arctic is critical in determining the density of water at sites of North Atlantic deep water formation, which in turn influences the global flux of oceanic heat and nutrients. We need geochemical tracers and high-resolution observations to refine our freshwater budgets and constrain models for future change. The use of seawater barium concentrations in the Arctic Ocean as a freshwater tracer relies on the conservative behaviour of barium in seawater; whilst this has been shown to be an unreliable assumption in Arctic summers, there are a lack of studies observing seasonal progressions. Here, we present barium concentrations from seawater and sea-ice collected during the Norwegian Young Sea ICE expedition from boreal winter into summer. We use other tracers (salinity, oxygen isotopes and alkalinity) to reconstruct freshwater inputs and calculate a barium “deficit” that can be attributed to non-conservative processes. We locate a deficit in winter when biological production is low, which we attribute to uptake by barite formation associated with old organic matter or by internal sea-ice processes. We also find a significant barium deficit during the early spring bloom, consistent with uptake into organic-matter associated microenvironments. However, in summer there no strong barium deficit near the surface, despite high biological production and organic carbon standing stocks, perhaps reflecting phytoplankton assemblage changes, and/or rapid internal cycling. Our findings challenge the assumptions surrounding the use of barium as an Arctic freshwater tracer, and highlight the need to improve our understanding of barium in sea-ice environments.
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spelling nottingham-516882018-05-22T14:40:17Z https://eprints.nottingham.ac.uk/51688/ Spatiotemporal variability of barium in Arctic sea-ice and seawater Hendry, Katharine R. Pyle, Kimberley M. Butler, G. Barney Cooper, Adam Fransson, Agneta Chierici, Melissa Leng, Melanie J. Meyer, Amelie Dodd, Paul A. Freshwater export from the Arctic is critical in determining the density of water at sites of North Atlantic deep water formation, which in turn influences the global flux of oceanic heat and nutrients. We need geochemical tracers and high-resolution observations to refine our freshwater budgets and constrain models for future change. The use of seawater barium concentrations in the Arctic Ocean as a freshwater tracer relies on the conservative behaviour of barium in seawater; whilst this has been shown to be an unreliable assumption in Arctic summers, there are a lack of studies observing seasonal progressions. Here, we present barium concentrations from seawater and sea-ice collected during the Norwegian Young Sea ICE expedition from boreal winter into summer. We use other tracers (salinity, oxygen isotopes and alkalinity) to reconstruct freshwater inputs and calculate a barium “deficit” that can be attributed to non-conservative processes. We locate a deficit in winter when biological production is low, which we attribute to uptake by barite formation associated with old organic matter or by internal sea-ice processes. We also find a significant barium deficit during the early spring bloom, consistent with uptake into organic-matter associated microenvironments. However, in summer there no strong barium deficit near the surface, despite high biological production and organic carbon standing stocks, perhaps reflecting phytoplankton assemblage changes, and/or rapid internal cycling. Our findings challenge the assumptions surrounding the use of barium as an Arctic freshwater tracer, and highlight the need to improve our understanding of barium in sea-ice environments. American Geophysical Union 2018-04-06 Article PeerReviewed application/pdf en cc_by https://eprints.nottingham.ac.uk/51688/8/Hendry_et_al-2017-Journal_of_Geophysical_Research%253A_Oceans.pdf Hendry, Katharine R., Pyle, Kimberley M., Butler, G. Barney, Cooper, Adam, Fransson, Agneta, Chierici, Melissa, Leng, Melanie J., Meyer, Amelie and Dodd, Paul A. (2018) Spatiotemporal variability of barium in Arctic sea-ice and seawater. Journal of Geophysical Research: Oceans . ISSN 2169-9275 https://agupubs.onlinelibrary.wiley.com/doi/epdf/10.1029/2017JC013668 doi:10.1029/2017JC013668 doi:10.1029/2017JC013668
spellingShingle Hendry, Katharine R.
Pyle, Kimberley M.
Butler, G. Barney
Cooper, Adam
Fransson, Agneta
Chierici, Melissa
Leng, Melanie J.
Meyer, Amelie
Dodd, Paul A.
Spatiotemporal variability of barium in Arctic sea-ice and seawater
title Spatiotemporal variability of barium in Arctic sea-ice and seawater
title_full Spatiotemporal variability of barium in Arctic sea-ice and seawater
title_fullStr Spatiotemporal variability of barium in Arctic sea-ice and seawater
title_full_unstemmed Spatiotemporal variability of barium in Arctic sea-ice and seawater
title_short Spatiotemporal variability of barium in Arctic sea-ice and seawater
title_sort spatiotemporal variability of barium in arctic sea-ice and seawater
url https://eprints.nottingham.ac.uk/51688/
https://eprints.nottingham.ac.uk/51688/
https://eprints.nottingham.ac.uk/51688/