dc.contributor.author | Pirjola, Liisa | |
dc.date.accessioned | 2018-08-24T08:26:11Z | |
dc.date.available | 2018-08-24T08:26:11Z | |
dc.date.issued | 2002-01-01 | |
dc.identifier.citation | Pirjola, Liisa (2002). A model prediction of the yield of cloud condensation nuclei from coastal nucleation events. Journal of Geophysical Research 107 , | |
dc.identifier.issn | 0148-0227 | |
dc.identifier.uri | http://hdl.handle.net/10379/9781 | |
dc.description.abstract | [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. | |
dc.publisher | Wiley-Blackwell | |
dc.relation.ispartof | Journal of Geophysical Research | |
dc.rights | Attribution-NonCommercial-NoDerivs 3.0 Ireland | |
dc.rights.uri | https://creativecommons.org/licenses/by-nc-nd/3.0/ie/ | |
dc.subject | aerosol dynamics | |
dc.subject | coastal particles | |
dc.subject | nucleation rate | |
dc.subject | vapor source rate | |
dc.subject | ccn | |
dc.subject | marine boundary-layer | |
dc.subject | sulfate aerosol formation | |
dc.subject | sea-salt aerosol | |
dc.subject | particle formation | |
dc.subject | free troposphere | |
dc.subject | north-atlantic | |
dc.subject | sulfuric-acid | |
dc.subject | atmospheric particles | |
dc.subject | size distribution | |
dc.subject | dimethyl sulfide | |
dc.title | A model prediction of the yield of cloud condensation nuclei from coastal nucleation events | |
dc.type | Article | |
dc.identifier.doi | 10.1029/2000jd000213 | |
dc.local.publishedsource | http://onlinelibrary.wiley.com/doi/10.1029/2000JD000213/pdf | |
nui.item.downloads | 0 | |