How ambient pressure influences water droplet nucleation at tropospheric conditions
- Author
- HYVÄRINEN, Antti-Pekka1 ; BRUS, David1 2 ; WEDEKIND, Jan3 ; LIHAVAINEN, Heikki1
[1] Finnish Meteorological Institute, Helsinki, Finland
[2] Laboratory of Aerosol Chemistry and Physics, Institute of Chemical Process Fundamentals, Academy of Sciences of the Czech Republic, Prague, Czech Republic
[3] Departament de Fisica Fonamental, Universitat de Barcelona, Barcelona, Spain - Source
Geophysical research letters. 2010, Vol 37, Num 21 ; L21802.1-L21802.4 ; ref : 1/4 p
- CODEN
- GPRLAJ
- ISSN
- 0094-8276
- Scientific domain
- Astronomy earth cosmic environment; Geophysics; Climatology, meteorology; Oceanography
- Publisher
- American Geophysical Union, Washington, DC
- Publication country
- United States
- Document type
- Article
- Language
- English
- Keyword (fr)
- Chambre diffusion Condensation Ecoulement laminaire Effet pression Germination homogène Germination hétérogène Gouttelette Hélium Modèle Nucléation Pression Température Théorie Troposphère Vapeur eau
- Keyword (en)
- Diffusion chamber condensation laminar flow Pressure effect Homogeneous nucleation Heterogeneous nucleation droplets helium models nucleation pressure temperature theory troposphere water vapor
- Keyword (es)
- Cámara difusión Condensación Efecto presión Germinación homogénea Germinación heterogénea Helio Modelo Nucleación Presión Temperatura Teoría Vapor agua
- Classification
- Discipline
- Earth sciences
- Origin
- Inist-CNRS
- Database
- PASCAL
- INIST identifier
- 23668117
Sauf mention contraire ci-dessus, le contenu de cette notice bibliographique peut être utilisé dans le cadre d’une licence CC BY 4.0 Inist-CNRS / Unless otherwise stated above, the content of this bibliographic record may be used under a CC BY 4.0 licence by Inist-CNRS / A menos que se haya señalado antes, el contenido de este registro bibliográfico puede ser utilizado al amparo de una licencia CC BY 4.0 Inist-CNRS
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DOI
10.1029/2010GL045013 
https://dx.doi.org/10.1029/2010GL045013
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