Bottom water acidification and warming on the western Eurasian Arctic shelves: Dynamical downscaling projections

This is an article published by American Geophysical Union in Journal of Geophysical Research: Oceans, available online: https://sites.agu.org/ The impacts of oceanic CO2 uptake and global warming on the surface ocean environment have received substantial attention, but few studies have focused on s...

Full description

Bibliographic Details
Published in:Journal of Geophysical Research: Oceans
Main Authors: Wallhead, Philip, Bellerby, Richard, Silyakova, Anna, Slagstad, Dag, Polukhin, Alexander A.
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 2017
Subjects:
Online Access:http://hdl.handle.net/11250/2494326
https://doi.org/10.1002/2017JC013231
id ftnorskinstvf:oai:niva.brage.unit.no:11250/2494326
record_format openpolar
spelling ftnorskinstvf:oai:niva.brage.unit.no:11250/2494326 2023-05-15T14:59:13+02:00 Bottom water acidification and warming on the western Eurasian Arctic shelves: Dynamical downscaling projections Wallhead, Philip Bellerby, Richard Silyakova, Anna Slagstad, Dag Polukhin, Alexander A. 2017 application/pdf http://hdl.handle.net/11250/2494326 https://doi.org/10.1002/2017JC013231 eng eng American Geophysical Union EC/FP7/212085 EC/FP7/26493 Norges forskningsråd: 225956 Norges forskningsråd: 184860 Journal of Geophysical Research - Oceans. 2017, 122 (10), 8126-8144. urn:issn:2169-9275 http://hdl.handle.net/11250/2494326 https://doi.org/10.1002/2017JC013231 cristin:1499879 © 2017. American Geophysical Union. All Rights Reserved. 8126-8144 122 Journal of Geophysical Research - Oceans 10 Journal article Peer reviewed 2017 ftnorskinstvf https://doi.org/10.1002/2017JC013231 2023-02-21T08:45:34Z This is an article published by American Geophysical Union in Journal of Geophysical Research: Oceans, available online: https://sites.agu.org/ The impacts of oceanic CO2 uptake and global warming on the surface ocean environment have received substantial attention, but few studies have focused on shelf bottom water, despite its importance as habitat for benthic organisms and demersal fisheries such as cod. We used a downscaling ocean biogeochemical model to project bottom water acidification and warming on the western Eurasian Arctic shelves. A model hindcast produced 14–18 year acidification trends that were largely consistent with observational estimates at stations in the Iceland and Irminger Seas. Projections under SRES A1B scenario revealed a rapid and spatially variable decline in bottom pH by 0.10–0.20 units over 50 years (2.5%–97.5% quantiles) at depths 50–500 m on the Norwegian, Barents, Kara, and East Greenland shelves. Bottom water undersaturation with respect to aragonite occurred over the entire Kara shelf by 2040 and over most of the Barents and East Greenland shelves by 2070. Shelf acidification was predominantly driven by the accumulation of anthropogenic CO2, and was concurrent with warming of 0.1–2.78C over 50 years. These combined perturbations will act as significant multistressors on the Barents and Kara shelves. Future studies should aim to improve the resolution of shelf bottom processes in models, and should consider the Kara Sea and Russian shelves as possible bellwethers of shelf acidification. publishedVersion Article in Journal/Newspaper Arctic East Greenland Global warming Greenland Iceland Kara Sea Norwegian Institute for Water research: NIVA Open Access Archive (Brage) Arctic Greenland Kara Sea Journal of Geophysical Research: Oceans 122 10 8126 8144
institution Open Polar
collection Norwegian Institute for Water research: NIVA Open Access Archive (Brage)
op_collection_id ftnorskinstvf
language English
description This is an article published by American Geophysical Union in Journal of Geophysical Research: Oceans, available online: https://sites.agu.org/ The impacts of oceanic CO2 uptake and global warming on the surface ocean environment have received substantial attention, but few studies have focused on shelf bottom water, despite its importance as habitat for benthic organisms and demersal fisheries such as cod. We used a downscaling ocean biogeochemical model to project bottom water acidification and warming on the western Eurasian Arctic shelves. A model hindcast produced 14–18 year acidification trends that were largely consistent with observational estimates at stations in the Iceland and Irminger Seas. Projections under SRES A1B scenario revealed a rapid and spatially variable decline in bottom pH by 0.10–0.20 units over 50 years (2.5%–97.5% quantiles) at depths 50–500 m on the Norwegian, Barents, Kara, and East Greenland shelves. Bottom water undersaturation with respect to aragonite occurred over the entire Kara shelf by 2040 and over most of the Barents and East Greenland shelves by 2070. Shelf acidification was predominantly driven by the accumulation of anthropogenic CO2, and was concurrent with warming of 0.1–2.78C over 50 years. These combined perturbations will act as significant multistressors on the Barents and Kara shelves. Future studies should aim to improve the resolution of shelf bottom processes in models, and should consider the Kara Sea and Russian shelves as possible bellwethers of shelf acidification. publishedVersion
format Article in Journal/Newspaper
author Wallhead, Philip
Bellerby, Richard
Silyakova, Anna
Slagstad, Dag
Polukhin, Alexander A.
spellingShingle Wallhead, Philip
Bellerby, Richard
Silyakova, Anna
Slagstad, Dag
Polukhin, Alexander A.
Bottom water acidification and warming on the western Eurasian Arctic shelves: Dynamical downscaling projections
author_facet Wallhead, Philip
Bellerby, Richard
Silyakova, Anna
Slagstad, Dag
Polukhin, Alexander A.
author_sort Wallhead, Philip
title Bottom water acidification and warming on the western Eurasian Arctic shelves: Dynamical downscaling projections
title_short Bottom water acidification and warming on the western Eurasian Arctic shelves: Dynamical downscaling projections
title_full Bottom water acidification and warming on the western Eurasian Arctic shelves: Dynamical downscaling projections
title_fullStr Bottom water acidification and warming on the western Eurasian Arctic shelves: Dynamical downscaling projections
title_full_unstemmed Bottom water acidification and warming on the western Eurasian Arctic shelves: Dynamical downscaling projections
title_sort bottom water acidification and warming on the western eurasian arctic shelves: dynamical downscaling projections
publisher American Geophysical Union
publishDate 2017
url http://hdl.handle.net/11250/2494326
https://doi.org/10.1002/2017JC013231
geographic Arctic
Greenland
Kara Sea
geographic_facet Arctic
Greenland
Kara Sea
genre Arctic
East Greenland
Global warming
Greenland
Iceland
Kara Sea
genre_facet Arctic
East Greenland
Global warming
Greenland
Iceland
Kara Sea
op_source 8126-8144
122
Journal of Geophysical Research - Oceans
10
op_relation EC/FP7/212085
EC/FP7/26493
Norges forskningsråd: 225956
Norges forskningsråd: 184860
Journal of Geophysical Research - Oceans. 2017, 122 (10), 8126-8144.
urn:issn:2169-9275
http://hdl.handle.net/11250/2494326
https://doi.org/10.1002/2017JC013231
cristin:1499879
op_rights © 2017. American Geophysical Union. All Rights Reserved.
op_doi https://doi.org/10.1002/2017JC013231
container_title Journal of Geophysical Research: Oceans
container_volume 122
container_issue 10
container_start_page 8126
op_container_end_page 8144
_version_ 1766331346667438080