Seasonal and mesoscale variability of oceanic transport of anthropogenic CO2

Metadata Label Value
Author(s) Lachkar, Z., Orr, J. C., Dutay, J.-C.
Publication Type Journal Items, Publication Status: Published
Full Text Search SFX for a Full-Text version of this document
Import to Mendeley

Detailed Information

Metadata Field Content
Title Seasonal and mesoscale variability of oceanic transport of anthropogenic CO2
Author(s) Lachkar, Z.
Orr, J. C.
Dutay, J.-C.
Journal or Series Title Biogeosciences
Volume Number 6
Issue Number 11
Start Page 2509
End Page 2523
ISSN 1726-4170
Publisher Copernicus
Publication Place Katlenburg-Lindau
Publication Date 2009-11-09
Abstract Estimates of the ocean's large-scale transport of anthropogenic CO2 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 CO2 transport. To diagnose this variability, we made a global anthropogenic CO2 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 CO2 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 CO2 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 CO2 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 CO2. 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 CO2. This component is not accounted for in coarse-resolution hydrographic surveys.
DOI 10.5194/bg-6-2509-2009
Additional Notes Received 13 March 2009, Published in Biogeosciences Discuss. 17 April 2009, Revised 20 August 2009, Accepted 29 October 2009
Document Type Article
Publication Status Published
Language English
Assigned Organisational Unit(s) 03731
Organisational Unit(s)
Source Database ID PP-51446
Description File Name MIME Type Size
No details could be found
There are no links available for this record.
This record has not been viewed during this period

  author = "Lachkar, Z. and Orr, J. C. and Dutay, J.-C.",
  title = "{S}easonal and mesoscale variability of oceanic transport of anthropogenic {C}{O}2",
  journal = "Biogeosciences",
  year = 2009,
  volume = "6",
  number = "11",
  pages = "2509--2523",
  month = nov,

E-Citations record created: Wed, 23 Jun 2010, 20:47:32 CET