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- W2063798521 abstract "High concentrations (e.g. 104–105 cm−3) of condensation nuclei are occasionally observed in the polar regions or over the central oceans in air that has been free of passage over continental surfaces for many days. The particles are relatively fresh, being no more than a few days old, as otherwise interparticle coagulation would lower the concentration well below that observed. We show a plausible scheme through which the particles (assumed to be droplets of H2SO4) may be produced from the acid vapor phase through the process of homogeneous nucleation, and develop (approximate) analytic expressions to estimate the particle production. A large fraction of pre-existing aerosol, however, must first be scavenged, as they would otherwise serve as surfaces of condensation and inhibit the nucleation. We conclude that the production of substantial (> 103 cm−3) numbers of new particles can take place only in humid pre-cleaned air mass systems." @default.
- W2063798521 created "2016-06-24" @default.
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- W2063798521 date "1989-01-01" @default.
- W2063798521 modified "2023-09-27" @default.
- W2063798521 title "Production of condensation nuclei in clean air by nucleation of H2SO4" @default.
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- W2063798521 doi "https://doi.org/10.1016/0004-6981(89)90564-7" @default.
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