A model prediction of the yield of cloud condensation nuclei from coastal nucleation events

• Published in: Journal of Geophysical Research
• Main Author: Pirjola, Liisa
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: Wiley-Blackwell 2002
• Subjects: aerosol dynamics; coastal particles; nucleation rate; vapor source rate; ccn; marine boundary-layer; sulfate aerosol formation; sea-salt aerosol; particle formation; free troposphere; north-atlantic; sulfuric-acid; atmospheric particles; size distribution; dimethyl sulfide; North Atlantic
• Online Access: http://hdl.handle.net/10379/9781; https://doi.org/10.1029/2000jd000213

[1] The formation and evolution of new particles during coastal nucleation events are examined using the aerosol dynamic and gas-phase chemistry model AEROFOR2. Coastal regions are known to be a strong source of natural aerosol particles and are also strong sources of biogenic vapors which can condense onto aerosol particles, thus resulting in particle growth. A number of model simulations were performed to determine the instantaneous nucleation rate along with the source rate of a generic biogenic vapor leading to the observed particle size distributions which indicate the rapid appearance of similar to10(5)-10(6) cm(-3) nucleation mode particles in this environment. Model calculations suggest values of 3 x 10(5) cm(-3) s(-1) to 3 x 10(6) cm(-3) s(-1) for the instantaneous nucleation rate and a value of 5 x 10(7) cm(-3) s(-1) for the condensable vapor source rate in order to reproduce the observed concentrations. A significant fraction of these new particles survive to grow into cloud condensation nuclei (CCN) sizes for supersaturations typically encountered in boundary layer clouds during subsequent evolution over 3 days under clear-sky conditions, thus contributing to the indirect radiative effect of aerosols. The amount of CCN is mainly affected by coagulation between particles and condensation of the biogenic vapor and, to a lesser extent, by condensation of sulphuric acid formed by DMS oxidation. In all simulated cases, an increase of more than 100% in CCN concentration, for supersaturations >0.35% was observed.