Size distributions and mixtures of dust and black carbon aerosol in Asian outflow: Physiochemistry and optical properties

By A. Clarke, Yohei Shinozuka, V. Kapustin, S. Howell, B. Huebert, S. Doherty, T. Anderson, D. Covert, James R. Anderson, X. Hua and 4 more. 2004

418 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/47a0fd86ae6d7a6cc5ce1e6193933425040bb293

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Citations in the corpus

Single-scattering properties of tri-axial ellipsoidal mineral dust aerosols: A database for application to radiative transfer calculations (2010, neutral): “For this reason, numerous laboratory studies and theoretical modeling simulations have been carried out (e.g. Bi, Yang, Kattawar, & Kahn, 2009, 2010; Clarke et al., 2004; Curtis et al., 2008; Li, Kattawar, & Yang, 2004; Muñoz et al., 2004, 2006; Nousiainen, Kahnert, & Veihelmann, 2006; Sokolik &…”
Coatings and their enhancement of black carbon light absorption in the tropical atmosphere (2008, background): “Airborne BC is the most significant particulate absorber of solar radiation in the atmosphere and an important contributor to both globaland regional-scale climate forcing [ Chylek et al., 1984; Ramanathan et al., 2001; Jacobson, 2004, 2006; Koch and Hansen, 2005; Chung and Seinfeld, 2005; Tripathi”
Export efficiency of black carbon aerosol in continental outflow: Global implications (2005, background): “A mass absorption efficiency of 7 m2 g 1 [Clarke et al., 2004] was assumed to convert to mass concentration.”
Light Absorption by Carbonaceous Particles: An Investigative Review (2006, background): “Clarke et al. (2004) reported values of 6–8 m 2 /g by normalizing absorption to the non-volatile fraction of the aerosol.”
Relative humidity dependence of aerosol optical properties and direct radiative forcing in the surface boundary layer at Xinken in Pearl River Delta of China : An observation based numerical study (2008, background): “This is because water generally comprises more than 50% of the fine particle mass as RH exceeding 70–80% (Hänel, 1976; Zhang and McMurry, 1993; McMurry, 2000), and the other indicated variables are humidity dependent, too (Covert et al., 1972; Clarke et al., 2004).”
Airborne measurements of dust layer properties, particle size distribution and mixing state of Saharan dust during SAMUM 2006 (2009, neutral): “Data are taken from Hess et al. (1998), Dubovik et al. (2002), Clarke et al. (2004) and this study.”