Modeling particle nucleation and growth over northern California during the 2010 CARES campaign

6 presents the change in the r (top), the STDV(middle) and the absolute value of the mean di ff erence (bottom) between modeled and observed daily averaged surface SO 2 for the

The UK’s Fa- cility for Airborne Atmospheric Measurements (FAAM) BAe-146 research aircraft was deployed to Nova Scotia, Canada where a number of BB plumes of di ff ering ages

In the future, this treatment of the rim- ing process will be employed in a new snow growth model that predicts the vertical evolution of ice particle size spectra, mass,

This method provides mean diameters and widths for OPC bins based upon Mie-Lorenz theory or any other particle scattering theory, without the need for smoothing, despite the

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The ver- tical distribution of trace gases from DC-8 flight 13 during the campaign had mixing ratios of CH 4 and CO of up to 1843 ppbv and 134 ppbv respectively, and low mixing

Aerosol–computational fluid dynamics modeling of ultrafine and black carbon particle emission, dilution, and growth near roadwaysL.

The concentration of particles at the critical cluster size is determined by numerically in- tegrating the pseudo-first order losses that occurred between the time of nucleation ( t