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Observational and numerical study on the influence of large-scale flow direction and coastline shape on sea-breeze evolution

Author
GILLIAM, Robert C1 ; RAMAN, Sethu1 ; NIYOGI, Dev Dutta S1
[1] Department of Marine, Earth and Atmospheric Sciences, State Climate Office of North Carolina, North Carolina State University, Raleigh, NC 27695-7236, United States
Source

Boundary - layer meteorology. 2004, Vol 111, Num 2, pp 275-300, 26 p ; ref : 1 p.3/4

CODEN
BLMEBR
ISSN
0006-8314
Scientific domain
Climatology, meteorology
Publisher
Springer, Dordrecht
Publication country
Netherlands
Document type
Article
Language
English
Author keyword
Complex coastline Doppler radar Sea breeze Sea-breeze circulations Sea-breeze modelling Synoptic-flow effects
Keyword (fr)
Brise mer Couche limite atmosphérique Intensité Modèle Météorologie Observation radar Plage Radar Doppler Régime écoulement Simulation numérique Troposphère Caroline du Nord Amérique du Nord Etats Unis
Keyword (en)
Sea breeze Atmospheric boundary layer intensity models meteorology Radar observation beaches Doppler radar Flow regime digital simulation troposphere North Carolina North America United States
Keyword (es)
Brisa marina Capa límite atmosférico Intensidad Modelo Meteorología Observación radar Playa Radar Doppler Régimen flujo Simulación numérica Carolina del norte America del norte Estados Unidos
Classification
Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E02 External geophysics / 001E02D Meteorology / 001E02D02 Convection, turbulence, diffusion. Boundary layer structure and dynamics

Discipline
External geophysics
Origin
Inist-CNRS
Database
PASCAL
INIST identifier
15492972

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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