The carbonic system distribution and fluxes in the NE Atlantic during Spring 1991
20 páginas, 3 tablas, 12 figuras The potential of the North Atlantic as a sink for atmospheric CO, was investigated hystudyinatbecarbonicsystemusingdamobtzinedduringthespnngof 1991.Tbeti.seafluxofC0, was related to chlorophyll and other enviromuental variables, and tbe regeneration of carbon in the...
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Language: | English |
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1995
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ftcsic:oai:digital.csic.es:10261/59975 2024-02-11T10:06:25+01:00 The carbonic system distribution and fluxes in the NE Atlantic during Spring 1991 Ríos, Aida F. Anderson, Thomas R. Pérez, Fiz F. 1995 http://hdl.handle.net/10261/59975 https://doi.org/10.1016/0079-6611(95)80001-A en eng Elsevier http://dx.doi.org/10.1016/0079-6611(95)80001-A Progress in Oceanography 35(4): 295-314 (1995) 0079-6611 http://hdl.handle.net/10261/59975 doi:10.1016/0079-6611(95)80001-A open artículo http://purl.org/coar/resource_type/c_6501 1995 ftcsic https://doi.org/10.1016/0079-6611(95)80001-A 2024-01-16T09:42:22Z 20 páginas, 3 tablas, 12 figuras The potential of the North Atlantic as a sink for atmospheric CO, was investigated hystudyinatbecarbonicsystemusingdamobtzinedduringthespnngof 1991.Tbeti.seafluxofC0, was related to chlorophyll and other enviromuental variables, and tbe regeneration of carbon in the mid-ocemr studied by examining vertical sections representative of the study area. Poor ccmelations were found between pC0, and cbloropbylf throughout much of the study area, aIthougb agood correlation wa? found along 1 VW. Tbe highest air-sea fluxes ofC0, were cakulatcd for areas where cbloropbyll was highest (45”13’N, 16”04’W), and where the greatest wind speeds occuned(4705l’N,280l8’W~.ThemeanCO,fluxfromIheaunospberetotheoce;loduringthestudy period (May) was calculated as 0.65mmol m-*d-l,w hich compares well with other studies. Regression equations were developed to predict total inorganic carbon from nutrients; errors were typically less tbau Ipmol kg’. Kegeneradonofcarbon in tbemld-oceauoccurredin two principal stages: O-IOCQm and>2300m.Reeeuera~onintheupperzonewasdominatedbysofttissuecarbon(86~), witbskeletal carbon(calcite)conCributingonly 14%.Tbefractionofregeneratedcafbonofskeletalorigb1increased to 5 I Qn in the >23OOm zone. EC MAST CTPO-0017 and MAR&245 projects supported by EEC and CICYT Peer reviewed Article in Journal/Newspaper North Atlantic Digital.CSIC (Spanish National Research Council) Progress in Oceanography 35 4 295 314 |
institution |
Open Polar |
collection |
Digital.CSIC (Spanish National Research Council) |
op_collection_id |
ftcsic |
language |
English |
description |
20 páginas, 3 tablas, 12 figuras The potential of the North Atlantic as a sink for atmospheric CO, was investigated hystudyinatbecarbonicsystemusingdamobtzinedduringthespnngof 1991.Tbeti.seafluxofC0, was related to chlorophyll and other enviromuental variables, and tbe regeneration of carbon in the mid-ocemr studied by examining vertical sections representative of the study area. Poor ccmelations were found between pC0, and cbloropbylf throughout much of the study area, aIthougb agood correlation wa? found along 1 VW. Tbe highest air-sea fluxes ofC0, were cakulatcd for areas where cbloropbyll was highest (45”13’N, 16”04’W), and where the greatest wind speeds occuned(4705l’N,280l8’W~.ThemeanCO,fluxfromIheaunospberetotheoce;loduringthestudy period (May) was calculated as 0.65mmol m-*d-l,w hich compares well with other studies. Regression equations were developed to predict total inorganic carbon from nutrients; errors were typically less tbau Ipmol kg’. Kegeneradonofcarbon in tbemld-oceauoccurredin two principal stages: O-IOCQm and>2300m.Reeeuera~onintheupperzonewasdominatedbysofttissuecarbon(86~), witbskeletal carbon(calcite)conCributingonly 14%.Tbefractionofregeneratedcafbonofskeletalorigb1increased to 5 I Qn in the >23OOm zone. EC MAST CTPO-0017 and MAR&245 projects supported by EEC and CICYT Peer reviewed |
format |
Article in Journal/Newspaper |
author |
Ríos, Aida F. Anderson, Thomas R. Pérez, Fiz F. |
spellingShingle |
Ríos, Aida F. Anderson, Thomas R. Pérez, Fiz F. The carbonic system distribution and fluxes in the NE Atlantic during Spring 1991 |
author_facet |
Ríos, Aida F. Anderson, Thomas R. Pérez, Fiz F. |
author_sort |
Ríos, Aida F. |
title |
The carbonic system distribution and fluxes in the NE Atlantic during Spring 1991 |
title_short |
The carbonic system distribution and fluxes in the NE Atlantic during Spring 1991 |
title_full |
The carbonic system distribution and fluxes in the NE Atlantic during Spring 1991 |
title_fullStr |
The carbonic system distribution and fluxes in the NE Atlantic during Spring 1991 |
title_full_unstemmed |
The carbonic system distribution and fluxes in the NE Atlantic during Spring 1991 |
title_sort |
carbonic system distribution and fluxes in the ne atlantic during spring 1991 |
publisher |
Elsevier |
publishDate |
1995 |
url |
http://hdl.handle.net/10261/59975 https://doi.org/10.1016/0079-6611(95)80001-A |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
http://dx.doi.org/10.1016/0079-6611(95)80001-A Progress in Oceanography 35(4): 295-314 (1995) 0079-6611 http://hdl.handle.net/10261/59975 doi:10.1016/0079-6611(95)80001-A |
op_rights |
open |
op_doi |
https://doi.org/10.1016/0079-6611(95)80001-A |
container_title |
Progress in Oceanography |
container_volume |
35 |
container_issue |
4 |
container_start_page |
295 |
op_container_end_page |
314 |
_version_ |
1790604136829419520 |