Asian dust events are generated by deep convection from strong low pressure systems that form over mineral dust source regions. This study compares the mineral dust optical properties of two strong Asian dust events from the winter (December 2007) and spring (March 2010) seasons using AERONET retrieved parameters from three sites along the dust event path: SACOL (dust source region), Xianghe (downwind mixed aerosol region), and Taihu (downwind pollution region). The parameters include: aerosol effective radius, optical depth (τ), absorptive optical depth (τabs), their respective wavelength dependences or Angstrom exponents (α and αabs), and the spectral single scattering albedo (ω0(λ)). The α440-870 values in both cases do not exceed 0.62 indicating coarse mode particle dominance at all three sites. The winter case is shown to have carbonaceous influences at all three sites as given by αabs440-870 between 1.3 and 1.8 with strong spectral tabs absorption. The spring case is more dust dominant with αabs440-870 of 1.7-2.5 (noting that the largest value occurred at Taihu) with strong tabs absorption primarily in the visible wavelengths. Comparison studies between the observed and theoretically calculated (ω0(λ)) for the winter and spring cases have shown an excellent agreement except for the winter case at Taihu due to pollution influences. The comparison studies also suggest that (ω0(λ)) is more sensitive to particle absorptive properties rather than particle size. The sharp increase in the aerosol radiative effect (ARE) during the dust events with AREBOA < ARETOA suggests a stronger aerosol cooling effect at the surface than at the TOA.
- Aerosol absorptive properties
- Asian dust events
- Mineral dust
ASJC Scopus subject areas
- Environmental Science (miscellaneous)
- Atmospheric Science