[1] We apply to Classical Labrador Sea Water (CLSW) the
transit-time distribution (TTD) method to estimate the inventory and uptake of anthropogenic carbon dioxide (Cant). A model of TTDs representing bulk-advection and diffusive mixing is constrained with CFC11 data. The constrained TTDs are used to propagate Cant into CLSW, allowing the air-sea disequi...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.524.6069 2023-05-15T17:06:02+02:00 [1] We apply to Classical Labrador Sea Water (CLSW) the C. B. Rodehacke D. A. Lebel Uptake Of Natural The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.524.6069 http://www.ldeo.columbia.edu/~spk/Papers/TerenzietalLabSeaCarbonGRL07.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.524.6069 http://www.ldeo.columbia.edu/~spk/Papers/TerenzietalLabSeaCarbonGRL07.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.ldeo.columbia.edu/~spk/Papers/TerenzietalLabSeaCarbonGRL07.pdf text ftciteseerx 2016-01-08T10:18:04Z transit-time distribution (TTD) method to estimate the inventory and uptake of anthropogenic carbon dioxide (Cant). A model of TTDs representing bulk-advection and diffusive mixing is constrained with CFC11 data. The constrained TTDs are used to propagate Cant into CLSW, allowing the air-sea disequilibrium to evolve consistently. Cant in the Labrador Sea (LS) surface waters cannot keep pace with increasing atmospheric CO2 and is highly undersaturated. Our best estimate for 2001 is an anthropogenic inventory of 1.0 Gt C and an uptake of 0.02 Gt C/year. By additionally using the constraint of present-day CO2 measurements, we estimate that the preindustrial LS was neutral or a weak source of CO2 to the atmosphere. Our estimates are subject to possible error due to the assumption of steady-state transport and carbon Text Labrador Sea Unknown |
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ftciteseerx |
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English |
description |
transit-time distribution (TTD) method to estimate the inventory and uptake of anthropogenic carbon dioxide (Cant). A model of TTDs representing bulk-advection and diffusive mixing is constrained with CFC11 data. The constrained TTDs are used to propagate Cant into CLSW, allowing the air-sea disequilibrium to evolve consistently. Cant in the Labrador Sea (LS) surface waters cannot keep pace with increasing atmospheric CO2 and is highly undersaturated. Our best estimate for 2001 is an anthropogenic inventory of 1.0 Gt C and an uptake of 0.02 Gt C/year. By additionally using the constraint of present-day CO2 measurements, we estimate that the preindustrial LS was neutral or a weak source of CO2 to the atmosphere. Our estimates are subject to possible error due to the assumption of steady-state transport and carbon |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
C. B. Rodehacke D. A. Lebel Uptake Of Natural |
spellingShingle |
C. B. Rodehacke D. A. Lebel Uptake Of Natural [1] We apply to Classical Labrador Sea Water (CLSW) the |
author_facet |
C. B. Rodehacke D. A. Lebel Uptake Of Natural |
author_sort |
C. B. Rodehacke |
title |
[1] We apply to Classical Labrador Sea Water (CLSW) the |
title_short |
[1] We apply to Classical Labrador Sea Water (CLSW) the |
title_full |
[1] We apply to Classical Labrador Sea Water (CLSW) the |
title_fullStr |
[1] We apply to Classical Labrador Sea Water (CLSW) the |
title_full_unstemmed |
[1] We apply to Classical Labrador Sea Water (CLSW) the |
title_sort |
[1] we apply to classical labrador sea water (clsw) the |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.524.6069 http://www.ldeo.columbia.edu/~spk/Papers/TerenzietalLabSeaCarbonGRL07.pdf |
genre |
Labrador Sea |
genre_facet |
Labrador Sea |
op_source |
http://www.ldeo.columbia.edu/~spk/Papers/TerenzietalLabSeaCarbonGRL07.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.524.6069 http://www.ldeo.columbia.edu/~spk/Papers/TerenzietalLabSeaCarbonGRL07.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766060943476785152 |