Radiative heating rates and direct radiative forcing by mineral dust in cloudy atmospheric conditions

By A. Quijano, I. Sokolik, O. B. Toon. 2000

171 citations recorded by the source corpus.

Subfields: Atmospheric Science, Earth-Surface Processes, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/3ff45736f2d84dd4f8a2dcc1fffae5af7f654516

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Citations in the corpus

Impact of radiatively interactive dust aerosols in the NASA GEOS‐5 climate model: Sensitivity to dust particle shape and refractive index (2014, background): “These are manifest in the composition of the dust—generally a function of source and particle size—and these will have important effects on the radiative properties of the aerosol [Sokolik and Toon, 1999; Quijano et al., 2000].”
Comparison of size and morphological measurements of coarse mode dust particles from Africa (2003, background): “Reid et al. [2003]. [39] Figure 3a shows the existence of large, amorphous alumino-silicates particles transported across the north tropical Atlantic Ocean.”
Dust cycle: An emerging core theme in Earth system science (2011, background): “Dust particles vary in composition and the differences in dust mineralogy can drastically affect the magnitude of the aerosol radiative forcing in the infrared and the visible range (Sokolik et al., 1998; Quijano et al., 2000).”
Modeling the radiative properties of nonspherical soil-derived mineral aerosols (2004, background): “Several previous studies have demonstrated how aerosol radiative e8ects (such as the top-of-the atmosphere (TOA) radiative forcing, radiative forcing at the surface, and radiative heating rates) might be a8ected by variations in optical depth, single scattering albedo, and asymmetry parameter of a d”
Single-Scattering Albedo and Radiative Forcing of Various Aerosol Species with a Global Three-Dimensional Model (2002, methodology): “The singlescattering albedo of soil dust aerosols is different among desert regions (Sokolik and Toon 1999), and the one used in this model is similar to that of the Saharan dust particles proposed by Quijano et al. (2000).”
Radiative properties and direct effect of Saharan dust measured by the C‐130 aircraft during Saharan Dust Experiment (SHADE): 2. Terrestrial spectrum (2003, background): “depending particularly on the height of the dust and the nature of the underlying surface and the presence of cloud [e.g., Sokolik and Toon, 1996; Quijano et al., 2000].”