Seasonal and mesoscale variability of oceanic transport of anthropogenic CO 2
Estimates of the ocean's large-scale transport of anthropogenic CO 2 are based on one-time hydrographic sections, but the temporal variability of this transport has not been investigated. The aim of this study is to evaluate how the seasonal and mesoscale variability affect data-based estimates...
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ftdoajarticles:oai:doaj.org/article:3e1741c4dadc4834ad617d1487056f75 2023-05-15T17:32:00+02:00 Seasonal and mesoscale variability of oceanic transport of anthropogenic CO 2 J.-C. Dutay Z. Lachkar J. C. Orr 2009-11-01T00:00:00Z https://doaj.org/article/3e1741c4dadc4834ad617d1487056f75 EN eng Copernicus Publications http://www.biogeosciences.net/6/2509/2009/bg-6-2509-2009.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 1726-4170 1726-4189 https://doaj.org/article/3e1741c4dadc4834ad617d1487056f75 Biogeosciences, Vol 6, Iss 11, Pp 2509-2523 (2009) Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 article 2009 ftdoajarticles 2022-12-31T07:13:47Z Estimates of the ocean's large-scale transport of anthropogenic CO 2 are based on one-time hydrographic sections, but the temporal variability of this transport has not been investigated. The aim of this study is to evaluate how the seasonal and mesoscale variability affect data-based estimates of anthropogenic CO 2 transport. To diagnose this variability, we made a global anthropogenic CO 2 simulation using an eddy-permitting version of the coupled ocean sea-ice model ORCA-LIM. As for heat transport, the seasonally varying transport of anthropogenic CO 2 is largest within 20° of the equator and shows secondary maxima in the subtropics. Ekman transport generally drives most of the seasonal variability, but the contribution of the vertical shear becomes important near the equator and in the Southern Ocean. Mesoscale variabilty contributes to the annual-mean transport of both heat and anthropogenic CO 2 with strong poleward transport in the Southern Ocean and equatorward transport in the tropics. This "rectified" eddy transport is largely baroclinic in the tropics and barotropic in the Southern Ocean due to a larger contribution from standing eddies. Our analysis revealed that most previous hydrographic estimates of meridional transport of anthropogenic CO 2 are severely biased because they neglect temporal fluctuations due to non-Ekman velocity variations. In each of the three major ocean basins, this bias is largest near the equator and in the high southern latitudes. In the subtropical North Atlantic, where most of the hydrographic-based estimates have been focused, this uncertainty represents up to 20% and 30% of total meridional transport of heat and CO 2 . Generally though, outside the tropics and Southern Ocean, there are only small variations in meridional transport due to seasonal variations in tracer fields and time variations in eddy transport. For the North Atlantic, eddy variability accounts for up to 10% and 15% of the total transport of heat and CO 2 . This component is not accounted for in ... Article in Journal/Newspaper North Atlantic Orca Sea ice Southern Ocean Directory of Open Access Journals: DOAJ Articles Southern Ocean |
institution |
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Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
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language |
English |
topic |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 |
spellingShingle |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 J.-C. Dutay Z. Lachkar J. C. Orr Seasonal and mesoscale variability of oceanic transport of anthropogenic CO 2 |
topic_facet |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 |
description |
Estimates of the ocean's large-scale transport of anthropogenic CO 2 are based on one-time hydrographic sections, but the temporal variability of this transport has not been investigated. The aim of this study is to evaluate how the seasonal and mesoscale variability affect data-based estimates of anthropogenic CO 2 transport. To diagnose this variability, we made a global anthropogenic CO 2 simulation using an eddy-permitting version of the coupled ocean sea-ice model ORCA-LIM. As for heat transport, the seasonally varying transport of anthropogenic CO 2 is largest within 20° of the equator and shows secondary maxima in the subtropics. Ekman transport generally drives most of the seasonal variability, but the contribution of the vertical shear becomes important near the equator and in the Southern Ocean. Mesoscale variabilty contributes to the annual-mean transport of both heat and anthropogenic CO 2 with strong poleward transport in the Southern Ocean and equatorward transport in the tropics. This "rectified" eddy transport is largely baroclinic in the tropics and barotropic in the Southern Ocean due to a larger contribution from standing eddies. Our analysis revealed that most previous hydrographic estimates of meridional transport of anthropogenic CO 2 are severely biased because they neglect temporal fluctuations due to non-Ekman velocity variations. In each of the three major ocean basins, this bias is largest near the equator and in the high southern latitudes. In the subtropical North Atlantic, where most of the hydrographic-based estimates have been focused, this uncertainty represents up to 20% and 30% of total meridional transport of heat and CO 2 . Generally though, outside the tropics and Southern Ocean, there are only small variations in meridional transport due to seasonal variations in tracer fields and time variations in eddy transport. For the North Atlantic, eddy variability accounts for up to 10% and 15% of the total transport of heat and CO 2 . This component is not accounted for in ... |
format |
Article in Journal/Newspaper |
author |
J.-C. Dutay Z. Lachkar J. C. Orr |
author_facet |
J.-C. Dutay Z. Lachkar J. C. Orr |
author_sort |
J.-C. Dutay |
title |
Seasonal and mesoscale variability of oceanic transport of anthropogenic CO 2 |
title_short |
Seasonal and mesoscale variability of oceanic transport of anthropogenic CO 2 |
title_full |
Seasonal and mesoscale variability of oceanic transport of anthropogenic CO 2 |
title_fullStr |
Seasonal and mesoscale variability of oceanic transport of anthropogenic CO 2 |
title_full_unstemmed |
Seasonal and mesoscale variability of oceanic transport of anthropogenic CO 2 |
title_sort |
seasonal and mesoscale variability of oceanic transport of anthropogenic co 2 |
publisher |
Copernicus Publications |
publishDate |
2009 |
url |
https://doaj.org/article/3e1741c4dadc4834ad617d1487056f75 |
geographic |
Southern Ocean |
geographic_facet |
Southern Ocean |
genre |
North Atlantic Orca Sea ice Southern Ocean |
genre_facet |
North Atlantic Orca Sea ice Southern Ocean |
op_source |
Biogeosciences, Vol 6, Iss 11, Pp 2509-2523 (2009) |
op_relation |
http://www.biogeosciences.net/6/2509/2009/bg-6-2509-2009.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 1726-4170 1726-4189 https://doaj.org/article/3e1741c4dadc4834ad617d1487056f75 |
_version_ |
1766129897993928704 |