Inorganic carbon and pH levels in the Rockall Trough 1991-2010
NOTICE: this is the author’s version of a work that was accepted for publication in Deep Sea Research Part I: Oceanographic Research Papers. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not b...
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Online Access: | http://hdl.handle.net/10793/820 https://doi.org/10.1016/j.dsr.2012.05.011 |
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ftmarineinst:oai:oar.marine.ie:10793/820 2023-05-15T17:36:03+02:00 Inorganic carbon and pH levels in the Rockall Trough 1991-2010 McGrath, Triona Kivimäe, Caroline Tanhua, Toste Cave, Rachel R. McGovern, Evin 2012 http://hdl.handle.net/10793/820 https://doi.org/10.1016/j.dsr.2012.05.011 en eng Elsevier Oceanographic Research Papers;68 McGrath, T., Kivimäe, C., Tanhua, T., Cave, R. & McGovern, E. (2012). Inorganic carbon and pH levels in the Rockall Trough 1991-2010. Deep Sea Research Part I: Oceanographic Research Papers, 68(2012), 79-91. doi:10.1016/j.dsr.2012.05.011 0967-0637 http://hdl.handle.net/10793/820 http://dx.doi.org/10.1016/j.dsr.2012.05.011 Anthropogenic carbon Acidification Inorganic carbon Water masses Rockall Trough North Atlantic Article 2012 ftmarineinst https://doi.org/10.1016/j.dsr.2012.05.011 2022-07-27T09:39:09Z NOTICE: this is the author’s version of a work that was accepted for publication in Deep Sea Research Part I: Oceanographic Research Papers. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Deep Sea Research Part I: Oceanographic Research Papers, [Volume 68, (June 2012)] doi:10.1016/j.dsr.2012.05.011, http://www.sciencedirect.com/science/article/pii/S0967063712001185 peer-reviewed The accumulation of anthropogenic CO2 in the oceans is altering seawater carbonate chemistry. Investigation and monitoring of the carbonate parameters is therefore necessary to understand potential impacts on ocean ecosystems. Total alkalinity (AT) and dissolved inorganic carbon (CT) were sampled across the Rockall Trough in Feb 2009 (CE0903) and Feb 2010 (CE10002) as part of a baseline study of inorganic carbon chemistry in Irish shelf waters. The results have been compared with data from WOCE surveys A01E (Sept 1991), A01 (Dec 1994), AR24 (Nov 1996) and A24 (June 1997). The 2009 and 2010 datasets provide a snapshot of the biogeochemical parameters which can act as a baseline of inorganic carbon and acidity levels in surface waters of the Rockall Trough in late winter for future comparison since previous surveys in the area have been affected by biological activity. The dataset also offers the possibility to compare decadal changes in subsurface waters. The temporal evolution of anthropogenic carbon (D Cant) between the 1990s and 2010 was evaluated using two separate methods; (i) a comparison of the concentrations of CT between surveys, after correcting it for remineralisation of organic material and formation and dissolution of calcium carbonate (D CT-abio) and (ii) an extended Multiple Linear Regression was used to calculate the D Cant (D Cant eMLR). There was an ... Article in Journal/Newspaper North Atlantic Marine Institute Open Access Repository Rockall Trough ENVELOPE(-15.036,-15.036,53.825,53.825) Deep Sea Research Part I: Oceanographic Research Papers 68 79 91 |
institution |
Open Polar |
collection |
Marine Institute Open Access Repository |
op_collection_id |
ftmarineinst |
language |
English |
topic |
Anthropogenic carbon Acidification Inorganic carbon Water masses Rockall Trough North Atlantic |
spellingShingle |
Anthropogenic carbon Acidification Inorganic carbon Water masses Rockall Trough North Atlantic McGrath, Triona Kivimäe, Caroline Tanhua, Toste Cave, Rachel R. McGovern, Evin Inorganic carbon and pH levels in the Rockall Trough 1991-2010 |
topic_facet |
Anthropogenic carbon Acidification Inorganic carbon Water masses Rockall Trough North Atlantic |
description |
NOTICE: this is the author’s version of a work that was accepted for publication in Deep Sea Research Part I: Oceanographic Research Papers. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Deep Sea Research Part I: Oceanographic Research Papers, [Volume 68, (June 2012)] doi:10.1016/j.dsr.2012.05.011, http://www.sciencedirect.com/science/article/pii/S0967063712001185 peer-reviewed The accumulation of anthropogenic CO2 in the oceans is altering seawater carbonate chemistry. Investigation and monitoring of the carbonate parameters is therefore necessary to understand potential impacts on ocean ecosystems. Total alkalinity (AT) and dissolved inorganic carbon (CT) were sampled across the Rockall Trough in Feb 2009 (CE0903) and Feb 2010 (CE10002) as part of a baseline study of inorganic carbon chemistry in Irish shelf waters. The results have been compared with data from WOCE surveys A01E (Sept 1991), A01 (Dec 1994), AR24 (Nov 1996) and A24 (June 1997). The 2009 and 2010 datasets provide a snapshot of the biogeochemical parameters which can act as a baseline of inorganic carbon and acidity levels in surface waters of the Rockall Trough in late winter for future comparison since previous surveys in the area have been affected by biological activity. The dataset also offers the possibility to compare decadal changes in subsurface waters. The temporal evolution of anthropogenic carbon (D Cant) between the 1990s and 2010 was evaluated using two separate methods; (i) a comparison of the concentrations of CT between surveys, after correcting it for remineralisation of organic material and formation and dissolution of calcium carbonate (D CT-abio) and (ii) an extended Multiple Linear Regression was used to calculate the D Cant (D Cant eMLR). There was an ... |
format |
Article in Journal/Newspaper |
author |
McGrath, Triona Kivimäe, Caroline Tanhua, Toste Cave, Rachel R. McGovern, Evin |
author_facet |
McGrath, Triona Kivimäe, Caroline Tanhua, Toste Cave, Rachel R. McGovern, Evin |
author_sort |
McGrath, Triona |
title |
Inorganic carbon and pH levels in the Rockall Trough 1991-2010 |
title_short |
Inorganic carbon and pH levels in the Rockall Trough 1991-2010 |
title_full |
Inorganic carbon and pH levels in the Rockall Trough 1991-2010 |
title_fullStr |
Inorganic carbon and pH levels in the Rockall Trough 1991-2010 |
title_full_unstemmed |
Inorganic carbon and pH levels in the Rockall Trough 1991-2010 |
title_sort |
inorganic carbon and ph levels in the rockall trough 1991-2010 |
publisher |
Elsevier |
publishDate |
2012 |
url |
http://hdl.handle.net/10793/820 https://doi.org/10.1016/j.dsr.2012.05.011 |
long_lat |
ENVELOPE(-15.036,-15.036,53.825,53.825) |
geographic |
Rockall Trough |
geographic_facet |
Rockall Trough |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
Oceanographic Research Papers;68 McGrath, T., Kivimäe, C., Tanhua, T., Cave, R. & McGovern, E. (2012). Inorganic carbon and pH levels in the Rockall Trough 1991-2010. Deep Sea Research Part I: Oceanographic Research Papers, 68(2012), 79-91. doi:10.1016/j.dsr.2012.05.011 0967-0637 http://hdl.handle.net/10793/820 http://dx.doi.org/10.1016/j.dsr.2012.05.011 |
op_doi |
https://doi.org/10.1016/j.dsr.2012.05.011 |
container_title |
Deep Sea Research Part I: Oceanographic Research Papers |
container_volume |
68 |
container_start_page |
79 |
op_container_end_page |
91 |
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1766135403561091072 |