Light Absorption by Carbonaceous Particles: An Investigative Review

By T. Bond, R. Bergström. 2006

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Subfields: Atmospheric Science, Global and Planetary Change

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Citations in the corpus

Variation of the radiative properties during black carbon aging: theoretical and experimental intercomparison (2015, methodology): “In the first sensitivity calculation for each aging stage, a lower bound of BC RI of 1.75–0.63i recommended by Bond and Bergstrom (2006) was used.”
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): “…Hasan and Dzubay, 1983; Kent et al., 1983; Hänel, 1987; Covert et al., 1990; d’ Almeida et al., 1991; Sloane et al., 1991; Tang and Munkelwitz, 1994; Seinfeld and Pandis, 1998; Redemann et al., 2000; Mallet et al., 2003; Bond and Bergstrom, 2006; Hoffer et al., 2006; Schkolnik et al., 2007, etc.).”
Simulation of direct radiative forcing of aerosols and their effects on East Asian climate using an interactive AGCM-aerosol coupled system (2012, methodology): “In this study, the assuming external mixing states of black carbon aerosols could potentially lead to an underestimate of BC forcing (Bond and Bergstrom 2006). The main optical property of OC is its scattering of solar radiation. This results in negative DRF at the TOA under all-sky conditions (Fig.”
Improved Aerosol Processes and Effective Radiative Forcing in HadGEM3 and UKESM1 (2018, methodology): “To address this low bias, using recent evidence that reviews the optical properties for BC (Bond et al., 2013), the BC refractive index is updated to the middle estimate recommended by Bond and Bergstrom (2006).”
Particulate emissions from commercial shipping: Chemical, physical, and optical properties (2008, methodology): “Conversion of EFAbs to EFBC is achieved using a mass absorption coefficient, at 532 nm, of 7.75 m 2 g � 1 [ Bond and Bergstrom, 2006 ].”
Minimizing light absorption measurement artifacts of the Aethalometer: evaluation of five correction algorithms (2009, methodology): “Instruments and methods to measure the light absorption by atmospheric particles have been described in detail elsewhere (Bohren and Huffman, 1983; Horvath, 1993; Heintzenberg et al., 1997; Moosm̈uller et al., 1997; Bond and Bergstrom, 2006).”
Shapes of soot aerosol particles and implications for their effects on climate (2010, methodology): “Using optical properties determined by the ET‐DDA method discussed above, the mass‐normalized scattering and absorption cross sections of soot for all standard particles were determined by using 1.8 g/cm 3 for the soot density [ Bond and Bergstrom, 2006 ].”
Single Particle Soot Photometer intercomparison at the AIDA chamber (2012, background): “This value is within the likely RI range of light absorbing carbon reported by Bond and Bergstrom (2006). Using an RI of n= 2.”
Physically based snow albedo model for calculating broadband albedos and the solar heating profile in snowpack for general circulation models (2011, result): “As the refractive index of BC we employed the spectrally independent value nBC = 1.85 − 0.71i, which is an intermediate value among those recommended by Bond and Bergstrom [2006] .”
Limitations in the enhancement of visible light absorption due to mixing state (2006, methodology): “However, this particle size is unrealistically small [ Bond and Bergstrom, 2006, section 7.7 ].”
Enhanced Solar Energy Absorption by Internally-Mixed Black Carbon in Snow Grains (2012, methodology): “5 m2 g−1 at 550 nm, which is also recommended byBond and Bergstrom(2006). This choice was derived from Mie calculations applying the refractive indices described above and a BC size distribution with numbermedian radius of 40 nm (effective radius of 95 nm), which is”
Contrasting the direct radiative effect and direct radiative forcing of aerosols (2014, background): “Annual mean surface direct albedo in the UV visible (left) and near infrared (right) from MODIS 2002–2007 observations. and refractive index to follow recommendations of Bond and Bergstrom (2006) and the shortwave refractive indices for dust following Sinyuk (2003).”
Aerosol Mixing State: Measurements, Modeling, and Impacts (2019, background): “See the review of Bond et al. (2013) for a comprehensive summary of the current state of knowledge about BC aerosols (and also the reviews of Bond & Bergstrom, 2006 and Andreae & Gelencsér, 2006).”
Particle sizing calibration with refractive index correction for light scattering optical particle counters and impacts upon PCASP and CDP data collected during the Fennec campaign (2012, background): “Refractive indices are taken from Bond and Bergstrom (2006), Dinar et al.”
Internally mixed soot, sulfates, and organic matter in aerosol particles from Mexico City (2008, background): “In the latter case, the effective refractive indices are calculated for the mixed materials using various mixing rules (Bond and Bergstrom, 2006; Bond et al., 2006; Stier et al., 2007; Bohren and Huffman, 1983).”
Exploiting simultaneous observational constraints on mass and absorption to estimate the global direct radiative forcing of black carbon and brown carbon (2014, methodology): “In addition, this coating or internal mixing can enhance the absorption of solar radiation (Fuller et al., 1999; Schnaiter et al., 2005; Bond and Bergstrom, 2006); therefore the aging process is important www.atmos-chem-phys.net/14/10989/2014/ Atmos.”
Color of brown carbon: A model for ultraviolet and visible light absorption by organic carbon aerosol (2007, background): “At a wavelength of 550 nm, the simple forcing efficiency of Bond and Bergstrom [2006] for a 150-nm particle is negative if the refractive index is 1.55 + 0.05i and positive if it is 1.55 + 0.06i.”
A review of biomass burning: Emissions and impacts on air quality, health and climate in China. (2017, background): “Mass absorption efficiency (MAE) of fresh soot particle is 4–9m(2)/g at 550 nmwavelength, aggregation and encapsulation with organic or inorganic condensates though atmospheric aging might increase its MAE by 30%–50% (Fuller et al., 1999; Bond and Bergstrom, 2006; Mustard et al., 2008; Zhang et al.,”
Dependence of Laser-Induced Incandescence on Physical Properties of Black Carbon Aerosols: Measurements and Theoretical Interpretation (2010, background): “1, respectively, corresponding to the ranges of reported values for BC and graphite at visible-to-near infrared wavelengths (Bond and Bergstrom 2006; Borghesi and Guizzetti 1991).”