Aerosol optical properties were measured with a seven-wavelength aethalometer and a three-wavelength nephelometer at the suburban site SORPES in Nanjing, China, in September 2013-January 2015. The aethalometer compensation parameter , calculated with the Virkkula et al. (2007) method depended on the backscatter fraction, measured with an independent method, the integrating nephelometer. At λ = 660 nm the daily averaged compensation parameter 0.0017 ± 0.0002 and 0.0042 ± 0.0013 when backscatter fraction at λ = 635 nm was in the ranges of 0.100 ± 0.005 and 0.160 ± 0.005, respectively. Also, the wavelength dependency of the compensation parameter depended on the backscatter fraction: when b(λ = 525 nm) was less than approximately 0.13 the compensation parameter decreased with wavelength and at larger b it increased with wavelength. This dependency has not been considered in any of the algorithms that are currently used for processing aethalometer data. The compensation parameter also depended on the single-scattering albedo ω0 so that decreased with increasing ω0. For the green light (λ = 520 nm) in the ω0 range 0.870 ± 0.005, the average (± standard deviation) 0.0047 ± 0.006 and in the ω0 range 0.960 ± 0.005, 0.0028 ± 0.0007. This difference was larger for the near-infrared light (λ = 880 nm): in the ω0 range 0.860 ± 0.005, 0.0055 ± 0.0023 and in the ω0 range 0.960 ± 0.005, 0.0019 ± 0.0011. The negative dependence of on ω0 was also shown with a simple theoretical analysis.
CITATION STYLE
Virkkula, A., Chi, X., Ding, A., Shen, Y., Nie, W., Qi, X., … Kulmala, M. (2015). On the interpretation of the loading correction of the aethalometer. Atmospheric Measurement Techniques, 8(10), 4415–4427. https://doi.org/10.5194/amt-8-4415-2015
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