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JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 108, NO. D23, 8647, doi:10.1029/2002JD003247, 2003

Variability of aerosol optical properties derived from in situ aircraft measurements during ACE-Asia

Theodore L. Anderson

Joint Institute for the Study of the Atmosphere and Oceans, University of Washington, Seattle, Washington, USA


Sarah J. Masonis

Department of Atmospheric Sciences, University of Washington, Seattle, Washington, USA


David S. Covert

Department of Atmospheric Sciences, University of Washington, Seattle, Washington, USA


Norman C. Ahlquist

Department of Atmospheric Sciences, University of Washington, Seattle, Washington, USA


Steven G. Howell

Department of Oceanography, University of Hawaii, Honolulu, Hawaii, USA


Antony D. Clarke

Department of Oceanography, University of Hawaii, Honolulu, Hawaii, USA


Cameron S. McNaughton

Department of Oceanography, University of Hawaii, Honolulu, Hawaii, USA


Abstract

Airborne measurements of aerosol light scattering (using nephelometers) and absorption (using particle/soot absorption photometers; PSAPs) in the Asian outflow region are presented. Aerosol particles were sampled through a new low turbulence inlet that proved very effective at transmitting coarse-mode particles. Noise and artifacts are characterized using in-flight measurements of particle-free air and measurements with identical instruments operated in parallel. For example, the sensitivities of PSAP noise to changing altitude, changing relative humidity (RH), and particle-loading on the internal filter are quantified. On the basis of these and previous instrument characterizations, we report averages, variations, and uncertainties of optical properties, focusing on data from approximately 300 level-leg samples obtained during 19 research flights in the spring of 2001. Several broad patterns emerge from this analysis. Two dominant components, fine-mode pollution and coarse-mode mineral dust, were observed to vary independently when separated using a cut point of 1 μm aerodynamic diameter at low RH. Fine-mode pollution was found to be moderately absorbing (single scatter albedo at low RH and 550 nm, ω = 0.88 ± 0.03; mean and 95% confidence uncertainty) and moderately hygroscopic (relative increase in scattering from 40% to 85% RH, fRH = 1.7 ± 0.2), while coarse-mode dust was found to have very low absorption (ω = 0.96 ± 0.01) and to be almost nonhygroscopic (fRH = 1.1 ± 0.1). These and other optical properties are intended to serve as constraints on optical models of the Asian aerosol for the purpose of satellite retrievals and calculations of direct radiative effects.

Received 29 November 2002; accepted 5 March 2003; published 19 August 2003.

Index Terms: 0305 Atmospheric Composition and Structure: Aerosols and particles (0345, 4801); 0360 Atmospheric Composition and Structure: Transmission and scattering of radiation; 0365 Atmospheric Composition and Structure: Troposphere—composition and chemistry; 0394 Atmospheric Composition and Structure: Instruments and techniques; 1610 Global Change: Atmosphere (0315, 0325).


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Citation: Anderson, T. L., S. J. Masonis, D. S. Covert, N. C. Ahlquist, S. G. Howell, A. D. Clarke, and C. S. McNaughton (2003), Variability of aerosol optical properties derived from in situ aircraft measurements during ACE-Asia, J. Geophys. Res., 108(D23), 8647, doi:10.1029/2002JD003247.