Nucleation and Atmospheric Aerosols 17th International Conference, Galway, Ireland, 2007
Atmospheric particles are ubiquitous in the atmosphere: they form the seeds for cloud droplets and they form haze layers, blocking out incoming radiation and contributing to a partial cooling of our climate. They also contribute to poor air quality and health impacts. A large fraction of aerosols are formed from nucleation processes a" that is a phase transition from vapour to liquid or solid particles. Examples are the formation of stable clusters about 1 nm in size from molecular collisions and these in turn can grow into larger (100 nm or more) haze particles via condensation to the fo.
"Atmospheric particles are ubiquitous in the atmosphere: they form the seeds for cloud droplets and they form haze layers, blocking out incoming radiation and contributing to a partial cooling of our climate. They also contribute to poor air quality and health impacts. A large fraction of aerosols are formed from nucleation processes a" that is a phase transition from vapour to liquid or solid particles. Examples are the formation of stable clusters about 1 nm in size from molecular collisions and these in turn can grow into larger (100 nm or more) haze particles via condensation to the fo."@en
International Conference on Nucleation and Atmospheric Aerosols (17 : 2007 : Galway, Ireland)
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International Conference on Nucleation and Atmospheric Aerosols (17e : 2007 : Galway, Irlande)
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International Conference on Nucleation and Atmospheric Aerosols (17th : 2007 : Galway, Ireland)
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International Conference on Nucleation and Atmospheric Aerosols (ICNAA) (17 2007.08.13-17 Galway)
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