Chemical characterization of submicron aerosol and particle growth events at a national background site (3295 m a.s.l.) on the Tibetan Plateau

We find that the variability in the CCN concentrations in the central Amazon is mostly driven by aerosol particle number concentration and size distribution, while variations in

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

Measurements of size distributions of submicron (by a Scanning Mobility Particle Sizer, SMPS, TSI) and supermicon (by a Laser Aerosol Spectrometer, LAS, TSI Inc.) aerosols

Both the ability of an aerosol particle to act as a CCN at a given S level and its contribution to extinction depends on the aerosol particle size distribution. Particle size is

“Particle hygroscopicity during atmospheric new particle formation events: implications for the chemical species contributing to particle growth” published in

Aircraft – based measurements of aerosol hygroscopicity, both in the form of size- resolved, diameter growth factors and in the dependence of particle light scattering on

Here we have a detail characterization of submicron aerosol species including mass concentrations, chemical composition, diurnal variations, and day-of-week patterns during

As discussed above the dominant mode diameter of particles during the particle growth event was smaller than during the fresh plume and so a change in particle composition leading