Limitations in the enhancement of visible light absorption due to mixing state
By T. Bond, G. Habib, R. Bergström. 2006
623 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change, Health, Toxicology and Mutagenesis
View Paper: https://www.semanticscholar.org/paper/6a3c990497557f7e5622448d994052c27945e88f
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Citations in the corpus
- Light Absorption by Carbonaceous Particles: An Investigative Review (2006, background): “Our investigation of this issue, originally intended for inclusion here, evolved to extend beyond the review nature of this paper and will be provided elsewhere ( Bond et al. 2005 ).”
- Shapes of soot aerosol particles and implications for their effects on climate (2010, methodology): “Embedding materials and coatings (hereafter “host materials or particles”) act as lenses that focus light on soot and thus amplify absorption [ Bond et al., 2006; Fuller et al., 1999].”
- Simulating the evolution of soot mixing state with a particle-resolved aerosol model (2008, background): “This effect on radiative properties has been studied by a number of investigators [e.g., Chy´lek et al., 1995; Jacobson, 2001; Riemer et al., 2003; Schnaiter et al., 2005; Bond et al., 2006 ].”
- Exploring the observational constraints on the simulation of brown carbon (2017, background): “When coated by other materials, typically inorganic and nonabsorbing OA, the absorption of BC will be enhanced by the lensing effect (Jacobson, 2001; Bond et al., 2006).”
- Particulate emissions from commercial shipping: Chemical, physical, and optical properties (2008, background): “: PARTICULATE EMISSIONS FROM SHIPS 11 of 16 D00F04 aerosol cannot be formed this quickly (if at all) and enhancement of absorption due to coating of scattering material [Bond et al., 2006] does not appear to be effective within the timeframe of interest.”
- Aerosol Mixing State: Measurements, Modeling, and Impacts (2019, background): “…of the atmospheric aerosol and its constituent particles have been discussed in a number of reviews (McNeill, 2017), including CCN (Farmer et al., 2015; McFiggans et al., 2006), INPs (DeMott et al., 2016; Knopf et al., 2018), and aerosol optical properties (Bond et al., 2006; Moise et al., 2015).”
- Size-resolved measurements of brown carbon in water and methanol extracts and estimates of their contribution to ambient fine-particle light absorption (2013, methodology): “This means the method does not consider possible light-absorption enhancements due to particle morphology, such as shell-core configurations (Bond et al., 2006; Cappa et al., 2012; Lack et al., 2010).”
- Amplification of Light Absorption of Black Carbon by Organic Coating (2010, background): “The absorption of BC can be significantly enhanced by internal mixing with other compounds according to Mie theory (Bond et al. 2006).”
- Internally mixed soot, sulfates, and organic matter in aerosol particles from Mexico City (2008, background): “5 relative to one without a coating (Bond et al., 2006).”
- Aircraft Instrument for Comprehensive Characterization of Aerosol Optical Properties, Part 2: Black and Brown Carbon Absorption and Absorption Enhancement Measured with Photo Acoustic Spectroscopy (2012, background): “These coatings can result in (1) collapse of the fractal BC cores emitted from efficient combustion (Zhang et al. 2008) and (2) enhanced absorption of BC by lensing radiation through the coating to the BC core (Schnaiter et al. 2005; Bond et al. 2006).”
- Coatings and their enhancement of black carbon light absorption in the tropical atmosphere (2008, background): “The effects of coatings on the optical properties of BC have been addressed primarily in theoretical treatments [Jacobson, 2006; Lesins et al., 2002; Bond et al., 2006] and in the laboratory [Schnaiter et al.”
- Variation of the radiative properties during black carbon aging: theoretical and experimental intercomparison (2015, background): “Bond et al. (2006) recommended a 50 % increase in BC absorption to account for the averaged coating effect during atmospheric aging.”
- Mass Absorption Cross-Section of Ambient Black Carbon Aerosol in Relation to Chemical Age (2009, methodology): “Bond et al. (2006b) describe a method of calculating theoretical absorption amplifications for individual particles based on the sizes of their BC cores and non-BC coatings.”
- Exploiting simultaneous observational constraints on mass and absorption to estimate the global direct radiative forcing of black carbon and brown carbon (2014, methodology): “The large bias in South Africa is likely due to the underestimate of both the poorly constrained emission factors for biomass burning (Bond et al., 2013) and the uncertainty of burned area. The GFED3 emissions used here are close to the FINNv1 (The Fire Inventory from NCAR version 1.0, Wiedinmyer et”
- Black carbon vertical profiles strongly affect its radiative forcing uncertainty (2012, background): “However, three models in P2 have mass extinction coefficients that deviate significantly from recommendations given in the literature (Bond et al., 2006) and thus unduly influence the RSD.”