Anthropogenic carbon and water masses in the Bay of Biscay

As part of the VACLAN (Climate Variability in the North Atlantic) project, a section covering the Bay of Biscay was sampled in September 2005. This work estimates the distribution of the different water masses in the region using an extended optimum multiparametric method and analyzes water mass dis...

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Autores principales: Castaño-Carrera, M, Pardo, PC, Álvarez, M, Lavín, A, Rodríguez, C, Carballo, R, Ríos, AF, Pérez, FF
Format: info:eu-repo/semantics/article
Jezik:eng
Izdano: Iniversidad Autónoma de Baja California 2011
Teme:
OMP
Online dostop:https://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/1820
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spelling repositorioinstitucional-20.500.12930-74432023-05-09T14:30:30Z Anthropogenic carbon and water masses in the Bay of Biscay Carbono antropogénico y masas de agua en el golfo de Vizcaya Castaño-Carrera, M Pardo, PC Álvarez, M Lavín, A Rodríguez, C Carballo, R Ríos, AF Pérez, FF anthropogenic carbon water masses Bay of Biscay OMP ENACW carbono antropogénico masas de agua golfo de Vizcaya OMP ENACW As part of the VACLAN (Climate Variability in the North Atlantic) project, a section covering the Bay of Biscay was sampled in September 2005. This work estimates the distribution of the different water masses in the region using an extended optimum multiparametric method and analyzes water mass distribution of anthropogenic carbon as calculated using two different approaches. The Eastern North Atlantic Central Water layer is mainly constituted by its subpolar component and Mediterranean Water appears very diluted, its dilution increasing northeastward. In relation to the anthropogenic carbon inventory, small differences were found between the two different methods used, 95 vs 87 mol C m–2, though both show the same distribution pattern, the concentration decreasing with depth. Eastern North Atlantic Central Water presents the highest anthropogenic carbon inventory, supporting more than 50% of the total column (52%). This work confirms the relevant role of the Bay of Biscay as a sink zone in the oceanic circulation.  En septiembre de 2005, como parte del proyecto VACLAN (Variabilidad Climática en el Atlántico Norte) se muestreó una sección a través del golfo de Vizcaya. En este trabajo se estimó la distribución de las diferentes masas de agua usando un método óptimo multiparamétrico extendido y se estudió la distribución del carbono antropogénico calculado en las mismas usando dos métodos distintos. Con respecto a las masas de agua presentes en la región, la capa de Agua Central del Este del Atlántico Norte está principalmente constituida por su componente subpolar y el agua Mediterránea aparece muy diluida, aumentando su dilución hacia el noreste. En relación al inventario de carbono antropogénico hay pequeñas diferencias entre los dos métodos utilizados, 95 vs 87 mol C m–2, aunque en ambos se observa el mismo patrón de distribución vertical, la concentración decrece con la profundidad. El Agua Central del Atlántico Nororiental presenta el mayor inventario de carbono antropogénico, que corresponde a más del 50% de la columna total (52%). Este trabajo confirma el papel relevante del golfo de Vizcaya como un sumidero de carbono antropogénico en la circulación oceánica. 2011-03-17 2021-06-03T03:55:19Z 2021-06-03T03:55:19Z info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Peer-reviewed Article Artículo Arbitrado https://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/1820 10.7773/cm.v38i1B.1820 https://hdl.handle.net/20.500.12930/7443 eng https://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/1820/1665 application/pdf Iniversidad Autónoma de Baja California Ciencias Marinas; Vol. 38 No. 1B (2012); 191-207 Ciencias Marinas; Vol. 38 Núm. 1B (2012); 191-207 2395-9053 0185-3880
institution Repositorio Institucional
collection DSpace
language eng
topic anthropogenic carbon
water masses
Bay of Biscay
OMP
ENACW
carbono antropogénico
masas de agua
golfo de Vizcaya
OMP
ENACW
spellingShingle anthropogenic carbon
water masses
Bay of Biscay
OMP
ENACW
carbono antropogénico
masas de agua
golfo de Vizcaya
OMP
ENACW
Castaño-Carrera, M
Pardo, PC
Álvarez, M
Lavín, A
Rodríguez, C
Carballo, R
Ríos, AF
Pérez, FF
Anthropogenic carbon and water masses in the Bay of Biscay
description As part of the VACLAN (Climate Variability in the North Atlantic) project, a section covering the Bay of Biscay was sampled in September 2005. This work estimates the distribution of the different water masses in the region using an extended optimum multiparametric method and analyzes water mass distribution of anthropogenic carbon as calculated using two different approaches. The Eastern North Atlantic Central Water layer is mainly constituted by its subpolar component and Mediterranean Water appears very diluted, its dilution increasing northeastward. In relation to the anthropogenic carbon inventory, small differences were found between the two different methods used, 95 vs 87 mol C m–2, though both show the same distribution pattern, the concentration decreasing with depth. Eastern North Atlantic Central Water presents the highest anthropogenic carbon inventory, supporting more than 50% of the total column (52%). This work confirms the relevant role of the Bay of Biscay as a sink zone in the oceanic circulation. 
format info:eu-repo/semantics/article
author Castaño-Carrera, M
Pardo, PC
Álvarez, M
Lavín, A
Rodríguez, C
Carballo, R
Ríos, AF
Pérez, FF
author_facet Castaño-Carrera, M
Pardo, PC
Álvarez, M
Lavín, A
Rodríguez, C
Carballo, R
Ríos, AF
Pérez, FF
author_sort Castaño-Carrera, M
title Anthropogenic carbon and water masses in the Bay of Biscay
title_short Anthropogenic carbon and water masses in the Bay of Biscay
title_full Anthropogenic carbon and water masses in the Bay of Biscay
title_fullStr Anthropogenic carbon and water masses in the Bay of Biscay
title_full_unstemmed Anthropogenic carbon and water masses in the Bay of Biscay
title_sort anthropogenic carbon and water masses in the bay of biscay
publisher Iniversidad Autónoma de Baja California
publishDate 2011
url https://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/1820
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