Abstract. Multi-year observations of aerosol microphysical and optical properties,
obtained through ground-based remote sensing at 50 China Aerosol Remote
Sensing Network (CARSNET) sites, were used to characterize the aerosol
climatology for representative remote, rural, and urban areas over China to
assess effects on climate. The annual mean effective radii for total
particles (ReffT) decreased from north to south and from rural to urban
sites, and high total particle volumes were found at the urban sites. The
aerosol optical depth at 440 nm (AOD440 nm) increased from remote and rural
sites (0.12) to urban sites (0.79), and the extinction Ångström
exponent (EAE440–870 nm) increased from 0.71 at the arid and semi-arid sites
to 1.15 at the urban sites, presumably due to anthropogenic emissions.
Single-scattering albedo (SSA440 nm) ranged from 0.88 to 0.92,
indicating slightly to strongly absorbing aerosols. Absorption
AOD440 nm values were 0.01 at the remote sites versus 0.07 at the urban
sites. The average direct aerosol radiative effect (DARE) at the bottom of
atmosphere increased from the sites in the remote areas (−24.40 W m−2) to the
urban areas (−103.28 W m−2), indicating increased cooling at the latter.
The DARE for the top of the atmosphere increased from −4.79 W m−2 at the
remote sites to −30.05 W m−2 at the urban sites, indicating overall
cooling effects for the Earth–atmosphere system. A classification method
based on SSA440 nm, fine-mode fraction (FMF), and EAE440–870 nm showed that coarse-mode particles (mainly dust) were dominant at the
rural sites near the northwestern deserts, while light-absorbing, fine-mode
particles were important at most urban sites. This study will be important
for understanding aerosol climate effects and regional environmental
pollution, and the results will provide useful information for satellite
validation and the improvement of climate modelling.