Explaining global surface aerosol number concentrations in terms of primary emissions and particle formation

Initial growth rates attributable to organic compounds observed with the CPC battery as a function of sulfuric acid concentration color coded with α -pinene decay rate (di ff

We use a global aerosol microphysics model to estimate the effect of particle formation through activation nucleation in the boundary layer (BL) on cloud droplet num- ber

Leaf BVOC emissions fluxes, above-canopy monoterpene concentration and aerosol particle size and number concentrations were measured during the growing season 2009 at the

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

O., and Pöschl, U.: Biomass burning aerosol emissions from vegetation fires: particle number and mass emission factors and size distributions, Atmos. W.: Properties and evolution

Temperature- and size-dependent values of volume- and surface-based homogeneous nucleation rates between 234.8 and 236.2 K were derived using a microphysical model and aerosol

In- vestigations of particle compositions with TEM in combina- tion with EDX showed negligible concentrations of mineral dust ( < 0. 5 % by number) and very minor concentrations

signed case studies corresponding to representative (in terms of the observed ranges of sulfuric acid gas concentrations, concentrations and charged fractions of freshly nu-