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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.
Copyright 2003 by the American Geophysical Union.
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