Aerosol and Clouds
Airborne measurements of atmospheric carbonaceous aerosols during ACE-Asia
Article first published online: 11 DEC 2002
DOI: 10.1029/2002JD002221
Copyright 2002 by the American Geophysical Union.
Issue
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Journal of Geophysical Research: Atmospheres (1984–2012)
Volume 107, Issue D23, pages AAC 13-1–AAC 13-21, 16 December 2002
Additional Information
How to Cite
, , and , Airborne measurements of atmospheric carbonaceous aerosols during ACE-Asia, J. Geophys. Res., 107(D23), 4704, doi:10.1029/2002JD002221, 2002.
Publication History
- Issue published online: 11 DEC 2002
- Article first published online: 11 DEC 2002
- Manuscript Accepted: 28 APR 2002
- Manuscript Revised: 22 APR 2002
- Manuscript Received: 21 FEB 2002
- Abstract
- Article
- References
- Cited By
Keywords:
- Elemental carbon;
- black carbon;
- ACE-Asia;
- Carbonate carbon;
- mineral dust
[1] Airborne levels of carbonaceous aerosols were measured using the Twin Otter aircraft during the Aerosol Characterization Experiment (ACE)-Asia. Particles were collected using a newly developed honeycomb denuder sampler and organic carbon (OC), elemental carbon (EC), and carbonate (CC) carbon levels determined using a thermal–optical carbon analyzer. During some flights, atmospheric layers could be identified as marine boundary, pollution dominated, or mineral dust dominated. Ångstrom exponent (å) values, calculated based on data from an onboard three-wavelength nephelometer, were used to discern the nature of some individual layers. Values of å for individual layers ranged from 0.2 to 2, corresponding to dust- and pollution-dominated layers, respectively. OC and EC concentrations below 3 km ranged from 0.58 to 29 μg C m−3 and from 0.20 to 1.8 μg C m−3, respectively. In general, for a given type of atmospheric layer, higher levels of total carbon (TC) were observed during ACE-Asia than those observed during ACE-2, Tropospheric Aerosol Radiative Forcing Observational Experiment (TARFOX) and Indian Ocean Experiment (INDOEX). Mixed layers of dust and pollution were found on some occasions. CC was detected in samples taken from layers in which å = 1.6, indicating that significant amounts of dust can be present even though å > 0.2. A linear regression of light absorption coefficient σap (Mm−1) versus EC concentration had an r2 of only 0.50, indicating that parameters other than the mass of EC significantly affected the value of σap. The mass absorption coefficient Eabs (m2 g−1) varied by as much as a factor of 8 between sampling events, and the average value of 11 m2 g−1 (±5.0) agrees well with previous published values.

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