Globally significant oceanic source of organic carbon aerosol

Significant concentrations of organic carbon (OC) aerosol are observed at three oceanic surface sites (Amsterdam Island, Azores and Mace Head). Two global chemical transport models (CTMs) underpredict OC concentrations at these sites (normalised mean bias of -67% and -58%). During periods of high bi...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Spracklen, Dominick V., Arnold, Steve R., Sciare, Jean, Carslaw, Kenneth S., Pio, Casimiro
Format: Article in Journal/Newspaper
Language:English
Published: Amer Geophysical Union 2008
Subjects:
Online Access:https://archimer.ifremer.fr/doc/00237/34831/33290.pdf
https://doi.org/10.1029/2008GL033359
https://archimer.ifremer.fr/doc/00237/34831/
Description
Summary:Significant concentrations of organic carbon (OC) aerosol are observed at three oceanic surface sites (Amsterdam Island, Azores and Mace Head). Two global chemical transport models (CTMs) underpredict OC concentrations at these sites (normalised mean bias of -67% and -58%). During periods of high biological activity monthly mean concentrations are underpredicted by a factor of 5-20. At Amsterdam Island and Mace Head, observed OC correlates well (R-2 = 0.61-0.77) with back-trajectory weighted chlorophyll-a, suggesting an oceanic OC source driven by biological activity. We use a combination of remote sensed chlorophyll-a, back trajectories and observed OC to derive an empirical relation between chlorophyll-a and the total oceanic OC emission flux. Using the GEOS-chem CTM we show a global oceanic OC emission, from primary and secondary sources, of similar to 8 Tg/year matches observations. This emission is comparable in magnitude to the fossil fuel OC source and increases the simulated global OC burden by 20%.