Climatology of aerosol composition (organic versus inorganic) at nonurban sites on a west-east transect across Europe

The well- predicted aerosol quantities, such as aerosol number, mass composition and optical properties, and the inclusion of full aerosol-cloud couplings lead to

Without considering water uptake, mass yields calculated with the HSP method are systematically lower than with UNIFAC-Raatikainen (Fig. 4) or without activity coefficients

In addition to the comparison with hourly concentrations of AMS-derived marine or- ganic aerosol at an inland site, we have also evaluated terrestrial and total organic

The spatial distribution of aerosol chemical com- position and the evolution of the Organic Aerosol (OA) fraction is investigated based upon airborne measurements of aerosol

In order to determine the Fe dissolution kinetics in the dust aerosol water, which contains organic ligands, such as oxalate, and high concentration of inorganic ions, such as

trends. Nitrate was observed to peak in early morning, during the rush hours. The peak in nitrate concentration in the morning was most pronounced when the concentrations were large

At these sites, about 30% of measured organic carbon was found in the coarse mode and was to a certain level attributed to primary biogenic organic aerosol (Puxbaum et al., 2003),

(1992) observed that fog scavenging efficiency of different chemical compounds was related to their water solubility, with higher scavenging for water-soluble species like sulfate,