Single‐particle measurements of midlatitude black carbon and light‐scattering aerosols from the boundary layer to the lower stratosphere

By Joshua P. Schwarz, R. Gao, D. Fahey, D. Thomson, L. Watts, J. Wilson, J. Reeves, M. Darbeheshti, D. Baumgardner, G. Kok and 11 more. 2006

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Dependence of Laser-Induced Incandescence on Physical Properties of Black Carbon Aerosols: Measurements and Theoretical Interpretation (2010, methodology): “The single-particle soot photometer (Model SP2) developed by Droplet Measurement Technologies, Inc. in Boulder, CO (Stephens et al. 2003; Schwarz et al. 2006; Moteki and Kondo 2007 and references therein) quantifies the mass of BC inside individual particles by means of laser-induced incandescence…”
Amplification of Light Absorption of Black Carbon by Organic Coating (2010, background): “0 g cm –3 ( Slowik et al. 2007 ) and ∼ 4000 K ( Schwarz et al.”
Effects of Mixing State on Black Carbon Measurements by Laser-Induced Incandescence (2007, methodology): “The particle temperature at the peak of the LII signal (hereafter, denoted as T peak) was used to estimate the chemical composition of the particle (e.g., metals, EC) (Stephens et al. 2003; Baumgardner et al. 2004; Schwarz et al. 2006).”
Aerosol light absorption and its measurement: A review (2009, methodology): “, single particle soot photometer (SP2)) has been based on a continuous laser source [336–338] and has found use for the diagnostic of individual particles sampled by an airborne SP2 from the troposphere and lower stratosphere [336,337] and in the laboratory for the diagnostic of individual particle”