Radiative properties and direct radiative effect of Saharan dust measured by the C-130 aircraft during SHADE: 1. Solar spectrum

By J. Haywood, Peter N. Francis, S. Osborne, M. Glew, Norman G. Loeb, E. Highwood, Didier Tanré, G. Myhre, P. Formenti, E. Hirst. 2003

380 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/784e42edd87dfb661d78c5a5b76123e568232e83

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Citations in the corpus

Modeling the radiative impact of mineral dust during the Saharan Dust Experiment (SHADE) campaign (2003, methodology): “The aircraft measurements of the radiative impact compare well with satellite derived radiative impact from the CERES instrument [Haywood et al., 2003].”
Estimates of global multicomponent aerosol optical depth and direct radiative perturbation in the Laboratoire de Météorologie Dynamique general circulation model (2005, result): “This larger dust SSA has been confirmed by various studies [Kaufman et al., 2001; Clarke et al., 2001; Haywood et al., 2003].”
Application of spheroid models to account for aerosol particle nonsphericity in remote sensing of desert dust (2006, background): “: DUST REMOTE SENSING USING SPHEROID MODEL 14 of 34 D11208 2003a, 2003b; Haywood et al., 2003].”
Influence of aerosol climatology on forecasts of the African Easterly Jet (2005, background): “Aerosol influence on AEJ forecasts Table 2: Characteristics of the aerosol components for dust-like aerosols in the new climatology, adapted from Hess et al. (1998). RH is the relative humidity assumed for the computations of the relevant optical properties. The nuclei, accumulation, and coarse mode”
Airborne measurements of dust layer properties, particle size distribution and mixing state of Saharan dust during SAMUM 2006 (2009, background): “Haywood et al. (2003a) pointed out that one of the optical particle counters (OPCs) responsible for the measurement of particles in the size range between 1 and 23.”
Bounding Global Aerosol Radiative Forcing of Climate Change (2020, background): “Aerosol contributions to outgo-226 ing shortwave radiative fluxes can exceed 100 W m−2 in some cases, as estimated for ex-227 ample by J. Haywood et al. (2003) from aircraft measurements of a mineral dust plume228 over the ocean.”
Single-scattering properties of tri-axial ellipsoidal mineral dust aerosols: A database for application to radiative transfer calculations (2010, background): “…region, the real part of the dust particle refractive index is from 1.5 to 1.6 (Claquin, Schulz, & Balkanski, 1999; Nousiainen, 2009; Sokolik & Toon, 1999), and the imaginary part is set to be 0.0015 or smaller (Haywood et al., 2003; Nousiainen, Muinonen, & Raisanen (2003); Sokolik & Toon, 1999).”
Developments in the CSU-RAMS Aerosol Model: Emissions, Nucleation, Regeneration, Deposition, and Radiation (2013, neutral): “This method of tracking aerosol mass contained within hy-drometeors is similar to the aerosol mass ratio transfer scheme of Rutledge et al. (1986) and Hegg et al. (1986).”
Measurement and modeling of the Saharan dust radiative impact: Overview of the Saharan Dust Experiment (SHADE) (2003, methodology): “The direct radiative effect was shown to reach instantaneous values of approximately À130 W m À2 over ocean in the solar spectrum on 25 September [Haywood et al., 2003], which is very large compared to other aerosol types Figure 7.”
Saharan dust absorption and refractive index from aircraft-based observations during SAMUM 2006 (2009, background): “The single-scattering albedo measured during SHADE is 0.96– 0.97 at 550 nm (Haywood et al., 2003), which agrees with recent values of 0.95–0.98 from laboratory studies (Linke et al., 2006).”
Observations of the impact of a major Saharan dust storm on the atmospheric radiation balance (2006, result): “The retrieved single scattering albedos at 0.5 mm are in the range 0.89–0.95, compared with 0.95–0.99 at 0.55 mm in a recent aircraft study [Haywood et al., 2003], indicating higher absorption in the retrievals used here.”
Reevaluation of Mineral aerosol radiative forcings suggests a better agreement with satellite and AERONET data (2006, background): “Haywood et al. (2003) and Anderson et al. (2005) inferred the DRE from airborne measurements of the radiation.”