Sorooshian, A. and Murphy, S. M. and Hersey, S. and Gates, H. and Padro, L. T. and Nenes, A. and Brechtel, F. J. and Jonsson, H. and Flagan, R. C. and Seinfeld, J. H. (2008) Comprehensive airborne characterization of aerosol from a major bovine source. Atmospheric Chemistry and Physics, 8 (17). pp. 5489-5520. ISSN 1680-7316 http://resolver.caltech.edu/CaltechAUTHORS:SORacp08
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We report an extensive airborne characterization of aerosol downwind of a massive bovine source in the San Joaquin Valley (California) on two flights during July 2007. The Center for Interdisciplinary Remotely-Piloted Aircraft Studies (CIRPAS) Twin Otter probed chemical composition, particle size distribution, mixing state, sub- and supersaturated water uptake behavior, light scattering properties, and the interrelationship between these parameters and meteorology. Total PM_(1.0) levels and concentrations of organics. nitrate. and ammonium were enhanced in the plume from the source as compared to the background aerosol. Organics dominated the plume aerosol mass (~56-64%), followed either by sulfate or nitrate. and then ammonium. Particulate amines were detected in the plume aerosol by a particle-into-liquid sampler (PILS) and via mass spectral inarkers in the Aerodvne C-ToF-AMS. Amines were found to be a significant atmospheric base even in the presence of arnmonia; particulate amine concentrations are estimated as at least 14-23% of that of ammonium in the plume. Enhanced sub- and supersaturated water uptake and reduced refractive indices were coincident with lower organic mass fractions, higher nitrate mass fractions, and the detection of amines. The likelihood of suppressed droplet growth owing to kinetic limitations from hydrophobic organic material is explored. After removing effects associated with size distribution and mixing state, the normalized activated fraction of cloud condensation nuclei (CCN) increased as a function of the subsaturated hygroscopic growth factor, with the highest activated fractions being consistent with relatively lower organic mass fractions and higher nitrate mass fractions. Subsaturated hygroscopic growth factors for the organic fraction of the aerosol are estimated based on employing the Zdanovskii-Stokes Robinson (ZSR) mixing rule. Representative values for a parameterization treating particle water uptake in both the sub- and supersaturated regimes are reported for incorporation into atmospheric models.
|Additional Information:||© Author(s) 2008. Received: 23 April 2008 – Published in Atmos. Chem. Phys. Discuss.: 3 June 2008 Revised: 12 August 2008 – Accepted: 15 August 2008 – Published: 12 September 2008. This work was supported, in part, by NOAA grant NA06OAR4310082. A. N. acknowledges support from an NSF CAREER award, NOAA, and NASA. L. T. P. acknowledges support from a NASA Earth System Science Fellowship. The authors gratefully acknowledge the NOAA Air Resources Laboratory (ARL) for provision of the HYSPLIT transport and dispersion model.|
|Subject Keywords:||CLOUD CONDENSATION NUCLEI; HYGROSCOPIC GROWTH MEASUREMENTS; PARTICULATE AMMONIUM-NITRATE; FLIGHT MASS-SPECTROMETRY; FINE PARTICLES PM2.5; ORGANIC-COMPOUNDS; CHEMICAL-COMPOSITION; NITRIC-ACID; RELATIVE-HUMIDITY; ALIPHATIC-AMINES|
|Usage Policy:||No commercial reproduction, distribution, display or performance rights in this work are provided.|
|Deposited By:||Tony Diaz|
|Deposited On:||24 Apr 2009 22:19|
|Last Modified:||26 Dec 2012 10:49|
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