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The Storm-Track Response to Idealized SST Perturbations in an Aquaplanet GCM

Author
BRAYSHAW, David James1 ; HOSKINS, Brian2 ; BLACKBURN, Michael1
[1] Walker Institute, Department of Meteorology, University of Reading, Reading, United Kingdom
[2] Department of Meteorology, University of Reading, Reading, United Kingdom
Source

Journal of the atmospheric sciences. 2008, Vol 65, Num 9, pp 2842-2860, 19 p ; ref : 3/4 p

CODEN
JAHSAK
ISSN
0022-4928
Scientific domain
Climatology, meteorology
Publisher
American Meteorological Society, Boston, MA
Publication country
United States
Document type
Article
Language
English
Keyword (fr)
Anomalie Cellule Hadley Circulation atmosphérique Haute résolution Modèle atmosphère Modèle circulation générale Moyenne latitude Simulation numérique Température surface marine Tempête Tourbillon Trajectoire Troposphère Zone subtropicale
Keyword (en)
anomalies Hadley cell atmospheric circulation high resolution Atmosphere model General circulation models Mid latitude digital simulation Sea surface temperature storms Vortex trajectory troposphere subtropical zone
Keyword (es)
Anomalía Célula Hadley Alta resolucion Modelo atmósfera Latitud media Simulación numérica Temperature superficie marina Tempestad Torbellino Zona subtropical
Classification
Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E02 External geophysics / 001E02D Meteorology

Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E02 External geophysics / 001E02H Physics of the high neutral atmosphere

Discipline
External geophysics
Origin
Inist-CNRS
Database
PASCAL
INIST identifier
20657185

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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