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A simple explanation for the increase in relative humidity between 11 and 14 km in the tropics

Author
FOLKINS, Ian1 ; KELLY, K. K2 ; WEINSTOCK, E. M3
[1] Department of Physics and Atmospheric Science, Dalhousie University, Halifax, Nova Scotia, Canada
[2] National Oceanic and Atmospheric Administration, Aeronomy Laboratory, Boulder, Colorado, United States
[3] Department of Chemistry and Chemical Biology, Harvard University, Cambridge, Massachusetts, United States
Source

Journal of geophysical research. 2002, Vol 107, Num D23, pp ACL26.1-ACL26.7 ; ref : 31 ref

ISSN
0148-0227
Scientific domain
Astronomy earth cosmic environment; Geology; Geophysics; Climatology, meteorology; Oceanography
Publisher
American Geophysical Union, Washington, DC
Publication country
United States
Document type
Article
Language
English
Keyword (fr)
Convection atmosphérique Humidité relative Répartition altitudinale Simulation numérique Troposphère Vapeur eau Zone tropicale
Keyword (en)
Atmospheric convection Relative humidity Altitudinal distribution Numerical simulation Troposphere Water vapor Tropical zone
Keyword (es)
Convección atmosférica Humedad relativa Distribución de altitud Simulación numérica Troposfera Vapor agua Zona tropical
Classification
Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E02 External geophysics / 001E02D Meteorology / 001E02D05 Water in the atmosphere (humidity, clouds, evaporation, precipitation)

Discipline
External geophysics
Origin
Inist-CNRS
Database
PASCAL
INIST identifier
14716778

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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