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 ar...

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Detalles Bibliográficos
Clasificación:Libro Electrónico
Autor Corporativo: SpringerLink (Online service)
Otros Autores: O'Dowd, Colin D. (Editor ), Wagner, Paul E. (Editor )
Formato: Electrónico eBook
Idioma:Inglés
Publicado: Dordrecht : Springer Netherlands : Imprint: Springer, 2007.
Edición:1st ed. 2007.
Temas:
Physics.
Astronomy.
Physics and Astronomy.
Classical and Continuum Physics.
Acceso en línea:Texto Completo

MARC

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245 1 0 |a Nucleation and Atmospheric Aerosols  |h [electronic resource] :  |b 17th International Conference, Galway, Ireland, 2007 /  |c edited by Colin D. O'Dowd, Paul E. Wagner. 
250 |a 1st ed. 2007. 
264 1 |a Dordrecht :  |b Springer Netherlands :  |b Imprint: Springer,  |c 2007. 
300 |a XXXVIII, 1256 p.  |b online resource. 
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505 0 |a Nucleation: Experiment and Theory -- Nucleation: Binary, Homogeneous, and Heterogeneous -- Nucleation: Ion and Cluster Properties -- Ice Nucleation -- Air Quality - Climate -- Aerosol - Cloud Interactions -- Aerosol Characterisation and Properties -- Aerosol Formation, Dynamics and Growth -- Marine Aerosol Production -- Remote Sensing of Aerosols and Clouds -- Chemical Composition and Cloud Drop Activation. 
520 |a 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 - 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 formation of ice crystals in mixed phase or cold clouds. This book brings together the leading experts from the nucleation and atmospheric aerosols research communities to present the current state-of-the-art knowledge in these related fields. Topics covered are: Nucleation Experiment & Theory, Binary, Homogeneous and Heterogeneous Nucleation, Ion & Cluster Properties During Nucleation, Aerosol Characterisation & Properties, Aerosol Formation, Dynamics and Growth, Marine Aerosol Production, Aerosol-Cloud Interactions, Chemical Composition & Cloud Drop Activation, Remote Sensing of aerosol & clouds and Air Quality-Climate Interactions. 
650 0 |a Physics. 
650 0 |a Astronomy. 
650 1 4 |a Physics and Astronomy. 
650 2 4 |a Classical and Continuum Physics. 
700 1 |a O'Dowd, Colin D.  |e editor.  |4 edt  |4 http://id.loc.gov/vocabulary/relators/edt 
700 1 |a Wagner, Paul E.  |e editor.  |4 edt  |4 http://id.loc.gov/vocabulary/relators/edt 
710 2 |a SpringerLink (Online service) 
773 0 |t Springer Nature eBook 
776 0 8 |i Printed edition:  |z 9789048115099 
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950 |a Physics and Astronomy (SpringerNature-11651) 
950 |a Physics and Astronomy (R0) (SpringerNature-43715) 

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