Oceanic CO2 uptake and biogeochemical variability during the formation of the Eastern North Atlantic Central water under two contrasting NAO scenarios
10 páginas, 8 figuras Long-term variability of the biogeochemical properties during the formation of central waters in the Eastern North Atlantic were analyzed between 42–47°N and 10–20°W from the dataset gathered during the Galicia VII (GVII) and C. Darwin 58/59 (CD58/59) cruises. These cruises tha...
Published in: | Journal of Marine Systems |
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Language: | English |
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Online Access: | http://hdl.handle.net/10261/54385 https://doi.org/10.1016/j.jmarsys.2010.10.002 |
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ftcsic:oai:digital.csic.es:10261/54385 2024-02-11T10:06:07+01:00 Oceanic CO2 uptake and biogeochemical variability during the formation of the Eastern North Atlantic Central water under two contrasting NAO scenarios Padín, X. A. Castro, Carmen G. Ríos, Aida F. Pérez, Fiz F. 2011 http://hdl.handle.net/10261/54385 https://doi.org/10.1016/j.jmarsys.2010.10.002 en eng Elsevier http://dx.doi.org/10.1016/j.jmarsys.2010.10.002 Journal of Marine Systems 84(3-4): 96-105 (2011) 0924-7963 http://hdl.handle.net/10261/54385 doi:10.1016/j.jmarsys.2010.10.002 none Air–sea CO2 fluxes NAO Climate variability ENACW formation Biogeochemical variability Northeast Atlantic artículo http://purl.org/coar/resource_type/c_6501 2011 ftcsic https://doi.org/10.1016/j.jmarsys.2010.10.002 2024-01-16T09:39:52Z 10 páginas, 8 figuras Long-term variability of the biogeochemical properties during the formation of central waters in the Eastern North Atlantic were analyzed between 42–47°N and 10–20°W from the dataset gathered during the Galicia VII (GVII) and C. Darwin 58/59 (CD58/59) cruises. These cruises that showed important changes in the thermohaline properties and the nutrient abundance of the upper layers were carried out under contrasting conditions of the North Atlantic Oscillation (NAO) index. The different climate forcing led ameridional shift of the transition zone between the formation regions of subpolar and subtropical Eastern North Atlantic CentralWater (ENACWp and ENACWt, respectively). This displacement conditioned the presence of each ENACW in the study region and so the thermohaline and biogeochemical properties. The effect of the observed variability at decadal scale on the air– sea CO2 gradient (ΔfCO2) and exchange (FCO2) was analyzed using 1D model approach throughout 11 weeklysteps that simulated the development of a spring bloomduring the shoaling of the mixed layer. The outputs of the model showed an intensification of the ocean CO2 uptake due to higher biological CO2 drawdown, during positive NAO conditions and its weakening under negative NAO influence. Processing work was supported by the European Commission within the 6th Framework Programme (EU FP6 CARBOOCEAN Integrated Project, contract no. 511176) and the ECO project (MCyT REN2002-00503/MAR). Peer reviewed Article in Journal/Newspaper North Atlantic North Atlantic oscillation Northeast Atlantic Digital.CSIC (Spanish National Research Council) Journal of Marine Systems 84 3-4 96 105 |
institution |
Open Polar |
collection |
Digital.CSIC (Spanish National Research Council) |
op_collection_id |
ftcsic |
language |
English |
topic |
Air–sea CO2 fluxes NAO Climate variability ENACW formation Biogeochemical variability Northeast Atlantic |
spellingShingle |
Air–sea CO2 fluxes NAO Climate variability ENACW formation Biogeochemical variability Northeast Atlantic Padín, X. A. Castro, Carmen G. Ríos, Aida F. Pérez, Fiz F. Oceanic CO2 uptake and biogeochemical variability during the formation of the Eastern North Atlantic Central water under two contrasting NAO scenarios |
topic_facet |
Air–sea CO2 fluxes NAO Climate variability ENACW formation Biogeochemical variability Northeast Atlantic |
description |
10 páginas, 8 figuras Long-term variability of the biogeochemical properties during the formation of central waters in the Eastern North Atlantic were analyzed between 42–47°N and 10–20°W from the dataset gathered during the Galicia VII (GVII) and C. Darwin 58/59 (CD58/59) cruises. These cruises that showed important changes in the thermohaline properties and the nutrient abundance of the upper layers were carried out under contrasting conditions of the North Atlantic Oscillation (NAO) index. The different climate forcing led ameridional shift of the transition zone between the formation regions of subpolar and subtropical Eastern North Atlantic CentralWater (ENACWp and ENACWt, respectively). This displacement conditioned the presence of each ENACW in the study region and so the thermohaline and biogeochemical properties. The effect of the observed variability at decadal scale on the air– sea CO2 gradient (ΔfCO2) and exchange (FCO2) was analyzed using 1D model approach throughout 11 weeklysteps that simulated the development of a spring bloomduring the shoaling of the mixed layer. The outputs of the model showed an intensification of the ocean CO2 uptake due to higher biological CO2 drawdown, during positive NAO conditions and its weakening under negative NAO influence. Processing work was supported by the European Commission within the 6th Framework Programme (EU FP6 CARBOOCEAN Integrated Project, contract no. 511176) and the ECO project (MCyT REN2002-00503/MAR). Peer reviewed |
format |
Article in Journal/Newspaper |
author |
Padín, X. A. Castro, Carmen G. Ríos, Aida F. Pérez, Fiz F. |
author_facet |
Padín, X. A. Castro, Carmen G. Ríos, Aida F. Pérez, Fiz F. |
author_sort |
Padín, X. A. |
title |
Oceanic CO2 uptake and biogeochemical variability during the formation of the Eastern North Atlantic Central water under two contrasting NAO scenarios |
title_short |
Oceanic CO2 uptake and biogeochemical variability during the formation of the Eastern North Atlantic Central water under two contrasting NAO scenarios |
title_full |
Oceanic CO2 uptake and biogeochemical variability during the formation of the Eastern North Atlantic Central water under two contrasting NAO scenarios |
title_fullStr |
Oceanic CO2 uptake and biogeochemical variability during the formation of the Eastern North Atlantic Central water under two contrasting NAO scenarios |
title_full_unstemmed |
Oceanic CO2 uptake and biogeochemical variability during the formation of the Eastern North Atlantic Central water under two contrasting NAO scenarios |
title_sort |
oceanic co2 uptake and biogeochemical variability during the formation of the eastern north atlantic central water under two contrasting nao scenarios |
publisher |
Elsevier |
publishDate |
2011 |
url |
http://hdl.handle.net/10261/54385 https://doi.org/10.1016/j.jmarsys.2010.10.002 |
genre |
North Atlantic North Atlantic oscillation Northeast Atlantic |
genre_facet |
North Atlantic North Atlantic oscillation Northeast Atlantic |
op_relation |
http://dx.doi.org/10.1016/j.jmarsys.2010.10.002 Journal of Marine Systems 84(3-4): 96-105 (2011) 0924-7963 http://hdl.handle.net/10261/54385 doi:10.1016/j.jmarsys.2010.10.002 |
op_rights |
none |
op_doi |
https://doi.org/10.1016/j.jmarsys.2010.10.002 |
container_title |
Journal of Marine Systems |
container_volume |
84 |
container_issue |
3-4 |
container_start_page |
96 |
op_container_end_page |
105 |
_version_ |
1790603605853601792 |