Journal cover Journal topic
Biogeosciences An interactive open-access journal of the European Geosciences Union
Journal topic
Volume 6, issue 6
Biogeosciences, 6, 1105–1114, 2009
https://doi.org/10.5194/bg-6-1105-2009
© Author(s) 2009. This work is distributed under
the Creative Commons Attribution 3.0 License.
Biogeosciences, 6, 1105–1114, 2009
https://doi.org/10.5194/bg-6-1105-2009
© Author(s) 2009. This work is distributed under
the Creative Commons Attribution 3.0 License.

  25 Jun 2009

25 Jun 2009

Evidence for surface organic matter modulation of air-sea CO2 gas exchange

M. Ll. Calleja1,2, C. M. Duarte1, Y. T. Prairie3, S. Agustí1, and G. J. Herndl4 M. Ll. Calleja et al.
  • 1IMEDEA (CSIC-UIB), Grup d' Oceanografía Interdisciplinar, C/ Miquel Marquès 21, 07190 Esporles, Mallorca, Spain
  • 2Department of Ocean Sciences, University of California, 1156 High Street, Santa Cruz, CA 95064, USA
  • 3Département des Sciences Biologiques, Université du Québec à Montréal. Box 8888, succ. Centre-Ville, Montreal, Qc, H3C 3P8 Canada
  • 4Department of Biological Oceanography, Royal Netherlands Institute for Sea Research, P.O. Box 59, 1790 AB Den Burg, The Netherlands

Abstract. Air-sea CO2 exchange depends on the air-sea CO2 gradient and the gas transfer velocity (k), computed as a function of wind speed. Large discrepancies among relationships predicting k from wind suggest that other processes also contribute significantly to modulate CO2 exchange. Here we report, on the basis of the relationship between the measured gas transfer velocity and the organic carbon concentration at the ocean surface, a significant role of surface organic matter in suppressing air-sea gas exchange, at low and intermediate winds, in the open ocean, confirming previous observations. The potential role of total surface organic matter concentration (TOC) on gas transfer velocity (k) was evaluated by direct measurements of air-sea CO2 fluxes at different wind speeds and locations in the open ocean. According to the results obtained, high surface organic matter contents may lead to lower air-sea CO2 fluxes, for a given air-sea CO2 partial pressure gradient and wind speed below 5 m s−1, compared to that observed at low organic matter contents. We found the bias in calculated gas fluxes resulting from neglecting TOC to co-vary geographically and seasonally with marine productivity. These results support previous evidences that consideration of the role of organic matter in modulating air-sea CO2 exchange may improve flux estimates and help avoid possible bias associated to variability in surface organic concentration across the ocean.

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