Ocean Acidification trends and Carbonate System dynamics in the North Atlantic Subpolar Gyre during 2009–2019
The CO 2 -carbonate system dynamics in the North Atlantic Subpolar Gyre (NASPG) were evaluated between 2009 and 2019. Data was collected aboard eight summer cruises through the CLIVAR 59.5º N section. The Ocean Acidification (OA) patterns and the reduction in the saturation state of calcite...
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ftcopernicus:oai:publications.copernicus.org:egusphere120068 2024-09-15T18:13:41+00:00 Ocean Acidification trends and Carbonate System dynamics in the North Atlantic Subpolar Gyre during 2009–2019 Curbelo-Hernández, David Pérez, Fiz F. González-Dávila, Melchor Gladyshev, Sergey V. González, Aridane G. González-Santana, David Velo, Antón Sokov, Alexey Santana-Casiano, J. Magdalena 2024-06-11 application/pdf https://doi.org/10.5194/egusphere-2024-1388 https://egusphere.copernicus.org/preprints/2024/egusphere-2024-1388/ eng eng doi:10.5194/egusphere-2024-1388 https://egusphere.copernicus.org/preprints/2024/egusphere-2024-1388/ eISSN: Text 2024 ftcopernicus https://doi.org/10.5194/egusphere-2024-1388 2024-08-28T05:24:22Z The CO 2 -carbonate system dynamics in the North Atlantic Subpolar Gyre (NASPG) were evaluated between 2009 and 2019. Data was collected aboard eight summer cruises through the CLIVAR 59.5º N section. The Ocean Acidification (OA) patterns and the reduction in the saturation state of calcite ( Ω Ca ) and aragonite ( Ω Arag ) in response to the increasing anthropogenic CO 2 ( C ant ) were assessed within the Irminger, Iceland and Rockall basins during a poorly-assessed decade in which the physical patterns reversed in comparison with previous well-known periods. The observed cooling, freshening and enhanced ventilation increased the interannual rate of accumulation of C ant in the interior ocean by 50–86 % and the OA rates by close to 10 %. The OA trends were 0.0013–0.0032 units yr -1 in the Irminger and Iceland basin and 0.0006–0.0024 units yr -1 in the Rockall Trough, causing a decline in Ω Ca and Ω Arag of 0.004–0.021 and 0.003–0.0013 units yr -1 , respectively. The C ant -driven rise in total inorganic carbon ( C T ) was the main driver of the OA (contributed by 53–68 % in upper layers and >82 % toward the interior ocean) and the reduction in Ω Ca and Ω Arag (>64 %). The transient decrease in temperature, salinity and A T collectively counteracts the C T -driven acidification by 45–85 % in the upper layers and in the shallow Rockall Trough and by <10 % in the interior ocean. The present investigation reports the acceleration of the OA within the NASPG and expands knowledge about the future state of the ocean. Text Iceland North Atlantic Ocean acidification Copernicus Publications: E-Journals |
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English |
description |
The CO 2 -carbonate system dynamics in the North Atlantic Subpolar Gyre (NASPG) were evaluated between 2009 and 2019. Data was collected aboard eight summer cruises through the CLIVAR 59.5º N section. The Ocean Acidification (OA) patterns and the reduction in the saturation state of calcite ( Ω Ca ) and aragonite ( Ω Arag ) in response to the increasing anthropogenic CO 2 ( C ant ) were assessed within the Irminger, Iceland and Rockall basins during a poorly-assessed decade in which the physical patterns reversed in comparison with previous well-known periods. The observed cooling, freshening and enhanced ventilation increased the interannual rate of accumulation of C ant in the interior ocean by 50–86 % and the OA rates by close to 10 %. The OA trends were 0.0013–0.0032 units yr -1 in the Irminger and Iceland basin and 0.0006–0.0024 units yr -1 in the Rockall Trough, causing a decline in Ω Ca and Ω Arag of 0.004–0.021 and 0.003–0.0013 units yr -1 , respectively. The C ant -driven rise in total inorganic carbon ( C T ) was the main driver of the OA (contributed by 53–68 % in upper layers and >82 % toward the interior ocean) and the reduction in Ω Ca and Ω Arag (>64 %). The transient decrease in temperature, salinity and A T collectively counteracts the C T -driven acidification by 45–85 % in the upper layers and in the shallow Rockall Trough and by <10 % in the interior ocean. The present investigation reports the acceleration of the OA within the NASPG and expands knowledge about the future state of the ocean. |
format |
Text |
author |
Curbelo-Hernández, David Pérez, Fiz F. González-Dávila, Melchor Gladyshev, Sergey V. González, Aridane G. González-Santana, David Velo, Antón Sokov, Alexey Santana-Casiano, J. Magdalena |
spellingShingle |
Curbelo-Hernández, David Pérez, Fiz F. González-Dávila, Melchor Gladyshev, Sergey V. González, Aridane G. González-Santana, David Velo, Antón Sokov, Alexey Santana-Casiano, J. Magdalena Ocean Acidification trends and Carbonate System dynamics in the North Atlantic Subpolar Gyre during 2009–2019 |
author_facet |
Curbelo-Hernández, David Pérez, Fiz F. González-Dávila, Melchor Gladyshev, Sergey V. González, Aridane G. González-Santana, David Velo, Antón Sokov, Alexey Santana-Casiano, J. Magdalena |
author_sort |
Curbelo-Hernández, David |
title |
Ocean Acidification trends and Carbonate System dynamics in the North Atlantic Subpolar Gyre during 2009–2019 |
title_short |
Ocean Acidification trends and Carbonate System dynamics in the North Atlantic Subpolar Gyre during 2009–2019 |
title_full |
Ocean Acidification trends and Carbonate System dynamics in the North Atlantic Subpolar Gyre during 2009–2019 |
title_fullStr |
Ocean Acidification trends and Carbonate System dynamics in the North Atlantic Subpolar Gyre during 2009–2019 |
title_full_unstemmed |
Ocean Acidification trends and Carbonate System dynamics in the North Atlantic Subpolar Gyre during 2009–2019 |
title_sort |
ocean acidification trends and carbonate system dynamics in the north atlantic subpolar gyre during 2009–2019 |
publishDate |
2024 |
url |
https://doi.org/10.5194/egusphere-2024-1388 https://egusphere.copernicus.org/preprints/2024/egusphere-2024-1388/ |
genre |
Iceland North Atlantic Ocean acidification |
genre_facet |
Iceland North Atlantic Ocean acidification |
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doi:10.5194/egusphere-2024-1388 https://egusphere.copernicus.org/preprints/2024/egusphere-2024-1388/ |
op_doi |
https://doi.org/10.5194/egusphere-2024-1388 |
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1810451443648299008 |