Improvements on the back-calculation technique for estimating anthropogenic CO2

17 páginas. 3 tablas, 5 figuras The back-calculation technique for evaluating the anthropogenic CO2 (CANT) input corrects total inorganic carbon for the remineralisation of organic matter and the dissolution of calcium carbonate, along with subtracting the pre-industrial equilibrium total inorganic...

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Published in:Deep Sea Research Part I: Oceanographic Research Papers
Main Authors: Pérez, Fiz F., Álvarez, Marta, Ríos, Aida F.
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2002
Subjects:
Online Access:http://hdl.handle.net/10261/52746
https://doi.org/10.1016/S0967-0637(02)00002-X
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spelling ftcsic:oai:digital.csic.es:10261/52746 2024-02-11T10:06:11+01:00 Improvements on the back-calculation technique for estimating anthropogenic CO2 Pérez, Fiz F. Álvarez, Marta Ríos, Aida F. 2002 http://hdl.handle.net/10261/52746 https://doi.org/10.1016/S0967-0637(02)00002-X en eng Elsevier http://dx.doi.org/10.1016/S0967-0637(02)00002-X Deep Sea Research - Part I - Oceanographic Research Papers 49(5): 869-875 (2002) 0967-0637 http://hdl.handle.net/10261/52746 doi:10.1016/S0967-0637(02)00002-X open Anthropogenic carbon Performed alkalinity North Atlantic ocean CO2 disequilibrium artículo http://purl.org/coar/resource_type/c_6501 2002 ftcsic https://doi.org/10.1016/S0967-0637(02)00002-X 2024-01-16T09:39:11Z 17 páginas. 3 tablas, 5 figuras The back-calculation technique for evaluating the anthropogenic CO2 (CANT) input corrects total inorganic carbon for the remineralisation of organic matter and the dissolution of calcium carbonate, along with subtracting the pre-industrial equilibrium total inorganic carbon. This technique is mainly dependent on the estimation of the preformed values of total alkalinity, oxygen and partial pressure of CO2 (pCO2). A new approach for estimating the preformed alkalinity (TA0) in the North Atlantic Ocean is suggested. TA0 is parameterised as a function of the inorganic to organic carbon decomposition ratio in the water column in agreement with sediment trap data and a recent review by Milliman et al. (Deep-Sea Res. I 46 (1999) 1653), which gives evidence for a considerable calcium carbonate dissolution in the upper 500–1000 m of the ocean, above the lysocline. We recalculated the CANT content in a section along the Eastern North Atlantic (OacesNAtlIIB-93) using this new TA0, the Mehrbach et al. (Limnol. Oceanogr. 8 (1973) 897) CO2 dissociation constants, and including the effect of water vapour pressure on estimation of the pre-industrial pCO2. Our findings lead us to conclude that the CO2 disequilibrium when water masses are formed is small and not significant. Direct and indirect evidence based on available high-quality CO2 data taken in formation areas in late winter conditions support this argument. M. Alvarez was financed by the ‘‘Xunta de Galicia’’ with a predoctoral grant. This work was supported by grant number CICYT-MAR97-0660. Peer reviewed Article in Journal/Newspaper North Atlantic Digital.CSIC (Spanish National Research Council) Alvarez ENVELOPE(-64.483,-64.483,-65.633,-65.633) Deep Sea Research Part I: Oceanographic Research Papers 49 5 859 875
institution Open Polar
collection Digital.CSIC (Spanish National Research Council)
op_collection_id ftcsic
language English
topic Anthropogenic carbon
Performed alkalinity
North Atlantic ocean
CO2 disequilibrium
spellingShingle Anthropogenic carbon
Performed alkalinity
North Atlantic ocean
CO2 disequilibrium
Pérez, Fiz F.
Álvarez, Marta
Ríos, Aida F.
Improvements on the back-calculation technique for estimating anthropogenic CO2
topic_facet Anthropogenic carbon
Performed alkalinity
North Atlantic ocean
CO2 disequilibrium
description 17 páginas. 3 tablas, 5 figuras The back-calculation technique for evaluating the anthropogenic CO2 (CANT) input corrects total inorganic carbon for the remineralisation of organic matter and the dissolution of calcium carbonate, along with subtracting the pre-industrial equilibrium total inorganic carbon. This technique is mainly dependent on the estimation of the preformed values of total alkalinity, oxygen and partial pressure of CO2 (pCO2). A new approach for estimating the preformed alkalinity (TA0) in the North Atlantic Ocean is suggested. TA0 is parameterised as a function of the inorganic to organic carbon decomposition ratio in the water column in agreement with sediment trap data and a recent review by Milliman et al. (Deep-Sea Res. I 46 (1999) 1653), which gives evidence for a considerable calcium carbonate dissolution in the upper 500–1000 m of the ocean, above the lysocline. We recalculated the CANT content in a section along the Eastern North Atlantic (OacesNAtlIIB-93) using this new TA0, the Mehrbach et al. (Limnol. Oceanogr. 8 (1973) 897) CO2 dissociation constants, and including the effect of water vapour pressure on estimation of the pre-industrial pCO2. Our findings lead us to conclude that the CO2 disequilibrium when water masses are formed is small and not significant. Direct and indirect evidence based on available high-quality CO2 data taken in formation areas in late winter conditions support this argument. M. Alvarez was financed by the ‘‘Xunta de Galicia’’ with a predoctoral grant. This work was supported by grant number CICYT-MAR97-0660. Peer reviewed
format Article in Journal/Newspaper
author Pérez, Fiz F.
Álvarez, Marta
Ríos, Aida F.
author_facet Pérez, Fiz F.
Álvarez, Marta
Ríos, Aida F.
author_sort Pérez, Fiz F.
title Improvements on the back-calculation technique for estimating anthropogenic CO2
title_short Improvements on the back-calculation technique for estimating anthropogenic CO2
title_full Improvements on the back-calculation technique for estimating anthropogenic CO2
title_fullStr Improvements on the back-calculation technique for estimating anthropogenic CO2
title_full_unstemmed Improvements on the back-calculation technique for estimating anthropogenic CO2
title_sort improvements on the back-calculation technique for estimating anthropogenic co2
publisher Elsevier
publishDate 2002
url http://hdl.handle.net/10261/52746
https://doi.org/10.1016/S0967-0637(02)00002-X
long_lat ENVELOPE(-64.483,-64.483,-65.633,-65.633)
geographic Alvarez
geographic_facet Alvarez
genre North Atlantic
genre_facet North Atlantic
op_relation http://dx.doi.org/10.1016/S0967-0637(02)00002-X
Deep Sea Research - Part I - Oceanographic Research Papers 49(5): 869-875 (2002)
0967-0637
http://hdl.handle.net/10261/52746
doi:10.1016/S0967-0637(02)00002-X
op_rights open
op_doi https://doi.org/10.1016/S0967-0637(02)00002-X
container_title Deep Sea Research Part I: Oceanographic Research Papers
container_volume 49
container_issue 5
container_start_page 859
op_container_end_page 875
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