Comparison of size and morphological measurements of coarse mode dust particles from Africa

By J. Reid, H. Jonsson, H. Maring, Alexander Smirnov, D. Savoie, S. Cliff, E. Reid, J. Livingston, M. Meier, Oleg Dubovik and 1 more. 2003

317 citations recorded by the source corpus.

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

View Paper: https://www.semanticscholar.org/paper/5f04740fa64999fb045624919ecc4b75a91c68b4

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Citations in the corpus

Aerosol light absorption and its measurement: A review (2009, background): “5mm with a large variability, which is partly due to measurement methods [234].”
Modeling the radiative properties of nonspherical soil-derived mineral aerosols (2004, methodology): “These distributions are representative of atmospheric dust particle spectra based on the data from the NASA AERONET network [37] and recent Ield experiments [38,39].”
Ability of multiangle remote sensing observations to identify and distinguish mineral dust types : Optical models and retrievals of optically thick plumes : Quantifying the radiative and biogeochemical impacts of mineral dust (2005, methodology): “672 mm to those obtained by Volten et al. [2001] and Muñoz et al.”
Airborne measurements of dust layer properties, particle size distribution and mixing state of Saharan dust during SAMUM 2006 (2009, methodology): “A comprehensive comparison of the measured size distributions with published information is difficult since different measurement techniques result in different equivalent diameters (e.g. Reid et al., 2003a).”
Statistically optimized inversion algorithm for enhanced retrieval of aerosol properties from spectral multi-angle polarimetric satellite observations (2010, methodology): “First, the utilization of this model has significantly improved the AERONET operational retrieval of aerosol with pronounced coarse mode fraction (e.g. see Reid et al., 2003; Eck et al., 2005; Dubovik et al., 2006).”
Characterization of iron oxides in mineral dust aerosols: Implications for light absorption (2006, background): “The Niger local erosion samples (hereinafter referred to as Ni-LE) were collected in spring during dust storms that originated from local erosion [ Rajot, 2001 ].”