2017
DOI: 10.5194/amt-10-3203-2017
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Estimation of aerosol complex refractive indices for both fine and coarse modes simultaneously based on AERONET remote sensing products

Abstract: Abstract. Climate change assessment, especially model evaluation, requires a better understanding of complex refractive indices (CRIs) of atmospheric aerosols -separately for both fine and coarse modes. However, the widely used aerosol CRI obtained by the global Aerosol Robotic Network (AERONET) corresponds to total-column aerosol particles without separation for fine and coarse modes. This paper establishes a method to separate CRIs of fine and coarse particles based on AERONET volume particle size distributi… Show more

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Cited by 31 publications
(35 citation statements)
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References 48 publications
(44 reference statements)
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“…Considering that most of high absorption coarse‐particle components result from soot or flying ash related to coal burning, highly emitted during winter season in China, we think that the high‐absorbing c‐UHS is related to the coarse particles in north winter. In contrast, it is also reasonable to infer that the c‐ULW model represents the summer conditions, especially considering its high water content (i.e., small value n c ) as suggested in Zhang, Li, Zhang, et al (). The c‐UNW model shows an extraordinarily high volume concentration ( C c = 0.482) together with weak absorption and moderate refractivity, which implies the natural dust.…”
Section: Resultsmentioning
confidence: 90%
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“…Considering that most of high absorption coarse‐particle components result from soot or flying ash related to coal burning, highly emitted during winter season in China, we think that the high‐absorbing c‐UHS is related to the coarse particles in north winter. In contrast, it is also reasonable to infer that the c‐ULW model represents the summer conditions, especially considering its high water content (i.e., small value n c ) as suggested in Zhang, Li, Zhang, et al (). The c‐UNW model shows an extraordinarily high volume concentration ( C c = 0.482) together with weak absorption and moderate refractivity, which implies the natural dust.…”
Section: Resultsmentioning
confidence: 90%
“…Scholars have suggested to mark these peaks as the standard fine mode (subscript f ), the standard coarse mode (subscript c ), the submicron fine mode (subscript SMF , i.e., particle radius larger than the standard fine mode but still in the fine particle size domain), and the super‐micron coarse mode (subscript SMC , i.e., particle radius smaller than the standard coarse mode but still in the coarse particle size domain; Li et al, ; Zhang et al, ). Zhang, Li, Zhang, et al () method (see Text S1 in the supporting information) is used to provide the individual fine‐/coarse‐mode aerosol products (as listed in Table ) from instantaneous measurements as the inputs of clustering analyses of this study. Considering that the optical parameters (e.g., AOD and single scattering albedo) can be derived from aerosol microphysical parameters, we only employ aerosol microphysical parameters in the clustering analyses.…”
Section: Methodsmentioning
confidence: 99%
“…In this paper, the sub-mode VSDs and CRIs were retrieved by the aerosol products [24,26] , following by Zhang et al (2016) and Zhang et al (2017). The method developed by Cuesta et al (2008) is employed to separate VSD into a single Log-Normal Modes (LNM).…”
Section: Methodsmentioning
confidence: 99%
“…Most research analyzed aerosol total-columnar CRI, but fine-and coarse-mode particles are associated with different composition and source of pollution. So, in this study we recalculated the complex refractive indices for both of fine and coarse mode, following Zhang et al (2017). For the calculation of the sub-mode CRI, we also choose the same radius limit (1 μm) as the sub-mode VSD.…”
Section: Methodsmentioning
confidence: 99%
“…The k c (675 nm) retrievals of SMART‐s were relatively higher than AERONET with a slightly larger variability even with their comparable estimated retrieval accuracy than fine mode as compared in Appendix A ( compare the black circles in between panels c and d in Figure ). Therefore, the significant variabilities of the n c and k c in Figure also can be attributed to diversity of dust composition and their microphysical properties (e.g., Gillespie & Lindberg, ; Sokolik & Toon, ; Zhang et al, ). In general, the retrievals of n and k are estimated to be highly uncertain, particularly for coarse mode (e.g., Sinyuk et al, ), which result in noisy values in Figures a and b.…”
Section: Algorithm Consistency Check Using Aeronet Measurementsmentioning
confidence: 99%