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Persistent ice cloud in the midsummer upper mesosphere at high latitudes: Three-dimensional modeling and cloud interactions with ambient water vapor : Layered Phenomenoa in the mesopause region (LPMR)

Author
VON ZAHN, U1 ; BERGER, U1
[1] Leibniz Institute of Atmospheric Physics, Kühlungsborn, Germany
Source

Journal of geophysical research. 2003, Vol 108, Num D8, pp PMR19.1-PMR19.15 ; ref : 51 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)
Croissance Echo radar Eté Fréquence apparition Haute latitude Modèle 3 dimensions Modèle chimique Mouvement particule Mésopause Mésosphère Nuage glace Nuage nocturne lumineux Rapport mélange Sublimation Transport particule Vapeur eau Zone polaire
Keyword (en)
Growth Radar echo Summer Occurrence frequency High latitude Three dimensional model Chemical model Particle motion Mesopause Mesosphere Ice cloud Noctilucent cloud Mixing ratio Sublimation Particle transport Water vapor Polar region
Keyword (es)
Crecimiento Eco radar Verano Frecuencia aparición Alta latitud Modelo 3 dimensiones Modelo químico Movimiento partícula Mesopausa Mesosfera Nube hielo Nube noctilucente Relación mezcla Sublimación Transporte partícula Vapor agua Zona polar
Classification
Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E02 External geophysics / 001E02H Physics of the high neutral atmosphere / 001E02H02 Atmospheric composition. Chemical and photochemical reactions

Discipline
External geophysics
Origin
Inist-CNRS
Database
PASCAL
INIST identifier
14837307

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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