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Published September 28, 2005 | Published
Journal Article Open

A large organic aerosol source in the free troposphere missing from current models


Aircraft measurements of organic carbon (OC) aerosol by two independent methods over the NW Pacific during the ACE-Asia campaign reveal unexpectedly high concentrations in the free troposphere (FT). Concentrations average 4 μg sm⁻³ in the 2–6.5 km column with little vertical gradient. These values are 10–100 times higher than computed with a global chemical transport model (CTM) including a standard 2-product simulation of secondary organic aerosol (SOA) formation based on empirical fits to smog chamber data. The same CTM reproduces the observed vertical profiles of sulfate and elemental carbon aerosols, which indicate sharp decreases from the boundary layer to the FT due to wet scavenging. Our results suggest a large, sustained source of SOA in the FT from oxidation of long-lived volatile organic compounds. We find that this SOA is the dominant component of aerosol mass in the FT, with implications for intercontinental pollution transport and radiative forcing of climate.

Additional Information

This work was supported by NASA ACMAP and NSF-ATM. The authors thank Teresa Campos for the ACE-Asia CO data and Jordi Dachs, Dan Jaffe, Doug Worsnop and Steve Maria for useful discussions.

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