Ocean acidification in the subpolar North Atlantic: rates and mechanisms controlling pH changes
Repeated hydrographic sections provide critically needed data on and understanding of changes in basin-wide ocean CO2 chemistry over multi-decadal timescales. Here, high-quality measurements collected at twelve cruises carried out along the same track between 1991 and 2015 have been used to determin...
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ftunivbergen:oai:bora.uib.no:1956/16362 2023-05-15T16:48:32+02:00 Ocean acidification in the subpolar North Atlantic: rates and mechanisms controlling pH changes García-Ibáñez, Maribel I. Zunino, Patricia Fröb, Friederike Carracedo, Lidia I. Ríos, Aida F. Mercier, Herlé Olsen, Are Pérez, Fiz F. 2016-06-23 application/pdf https://hdl.handle.net/1956/16362 https://doi.org/10.5194/bg-13-3701-2016 eng eng European Geosciences Union Climate controlled mechanisms of subpolar North Atlantic carbon uptake urn:issn:1726-4189 urn:issn:1726-4170 https://hdl.handle.net/1956/16362 https://doi.org/10.5194/bg-13-3701-2016 This work is distributed under the Creative Commons Attribution 3.0 License. https://creativecommons.org/licenses/by/3.0/ Copyright the authors. Biogeosciences 13 VDP::Matematikk og Naturvitenskap: 400::Geofag: 450 Peer reviewed Journal article 2016 ftunivbergen https://doi.org/10.5194/bg-13-3701-2016 2023-03-14T17:41:21Z Repeated hydrographic sections provide critically needed data on and understanding of changes in basin-wide ocean CO2 chemistry over multi-decadal timescales. Here, high-quality measurements collected at twelve cruises carried out along the same track between 1991 and 2015 have been used to determine long-term changes in ocean CO2 chemistry and ocean acidification in the Irminger and Iceland basins of the North Atlantic Ocean. Trends were determined for each of the main water masses present and are discussed in the context of the basin-wide circulation. The pH has decreased in all water masses of the Irminger and Iceland basins over the past 25 years with the greatest changes in surface and intermediate waters (between −0.0010 ± 0.0001 and −0.0018 ± 0.0001 pH units yr−1). In order to disentangle the drivers of the pH changes, we decomposed the trends into their principal drivers: changes in temperature, salinity, total alkalinity (AT) and total dissolved inorganic carbon (both its natural and anthropogenic components). The increase in anthropogenic CO2 (Cant) was identified as the main agent of the pH decline, partially offset by AT increases. The acidification of intermediate waters caused by Cant uptake has been reinforced by the aging of the water masses over the period of our analysis. The pH decrease of the deep overflow waters in the Irminger basin was similar to that observed in the upper ocean and was mainly linked to the Cant increase, thus reflecting the recent contact of these deep waters with the atmosphere. publishedVersion Article in Journal/Newspaper Iceland North Atlantic Ocean acidification University of Bergen: Bergen Open Research Archive (BORA-UiB) Irminger Basin ENVELOPE(-36.000,-36.000,61.000,61.000) Biogeosciences 13 12 3701 3715 |
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::Geofag: 450 |
spellingShingle |
VDP::Matematikk og Naturvitenskap: 400::Geofag: 450 García-Ibáñez, Maribel I. Zunino, Patricia Fröb, Friederike Carracedo, Lidia I. Ríos, Aida F. Mercier, Herlé Olsen, Are Pérez, Fiz F. Ocean acidification in the subpolar North Atlantic: rates and mechanisms controlling pH changes |
topic_facet |
VDP::Matematikk og Naturvitenskap: 400::Geofag: 450 |
description |
Repeated hydrographic sections provide critically needed data on and understanding of changes in basin-wide ocean CO2 chemistry over multi-decadal timescales. Here, high-quality measurements collected at twelve cruises carried out along the same track between 1991 and 2015 have been used to determine long-term changes in ocean CO2 chemistry and ocean acidification in the Irminger and Iceland basins of the North Atlantic Ocean. Trends were determined for each of the main water masses present and are discussed in the context of the basin-wide circulation. The pH has decreased in all water masses of the Irminger and Iceland basins over the past 25 years with the greatest changes in surface and intermediate waters (between −0.0010 ± 0.0001 and −0.0018 ± 0.0001 pH units yr−1). In order to disentangle the drivers of the pH changes, we decomposed the trends into their principal drivers: changes in temperature, salinity, total alkalinity (AT) and total dissolved inorganic carbon (both its natural and anthropogenic components). The increase in anthropogenic CO2 (Cant) was identified as the main agent of the pH decline, partially offset by AT increases. The acidification of intermediate waters caused by Cant uptake has been reinforced by the aging of the water masses over the period of our analysis. The pH decrease of the deep overflow waters in the Irminger basin was similar to that observed in the upper ocean and was mainly linked to the Cant increase, thus reflecting the recent contact of these deep waters with the atmosphere. publishedVersion |
format |
Article in Journal/Newspaper |
author |
García-Ibáñez, Maribel I. Zunino, Patricia Fröb, Friederike Carracedo, Lidia I. Ríos, Aida F. Mercier, Herlé Olsen, Are Pérez, Fiz F. |
author_facet |
García-Ibáñez, Maribel I. Zunino, Patricia Fröb, Friederike Carracedo, Lidia I. Ríos, Aida F. Mercier, Herlé Olsen, Are Pérez, Fiz F. |
author_sort |
García-Ibáñez, Maribel I. |
title |
Ocean acidification in the subpolar North Atlantic: rates and mechanisms controlling pH changes |
title_short |
Ocean acidification in the subpolar North Atlantic: rates and mechanisms controlling pH changes |
title_full |
Ocean acidification in the subpolar North Atlantic: rates and mechanisms controlling pH changes |
title_fullStr |
Ocean acidification in the subpolar North Atlantic: rates and mechanisms controlling pH changes |
title_full_unstemmed |
Ocean acidification in the subpolar North Atlantic: rates and mechanisms controlling pH changes |
title_sort |
ocean acidification in the subpolar north atlantic: rates and mechanisms controlling ph changes |
publisher |
European Geosciences Union |
publishDate |
2016 |
url |
https://hdl.handle.net/1956/16362 https://doi.org/10.5194/bg-13-3701-2016 |
long_lat |
ENVELOPE(-36.000,-36.000,61.000,61.000) |
geographic |
Irminger Basin |
geographic_facet |
Irminger Basin |
genre |
Iceland North Atlantic Ocean acidification |
genre_facet |
Iceland North Atlantic Ocean acidification |
op_source |
Biogeosciences 13 |
op_relation |
Climate controlled mechanisms of subpolar North Atlantic carbon uptake urn:issn:1726-4189 urn:issn:1726-4170 https://hdl.handle.net/1956/16362 https://doi.org/10.5194/bg-13-3701-2016 |
op_rights |
This work is distributed under the Creative Commons Attribution 3.0 License. https://creativecommons.org/licenses/by/3.0/ Copyright the authors. |
op_doi |
https://doi.org/10.5194/bg-13-3701-2016 |
container_title |
Biogeosciences |
container_volume |
13 |
container_issue |
12 |
container_start_page |
3701 |
op_container_end_page |
3715 |
_version_ |
1766038608140042240 |