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Rip-current pulses tied to Lagrangian coherent structures

Author
RENIERS, A. J. H. M1 2 ; MACMAHAN, J. H3 ; BERON-VERA, F. J1 ; OLASCOAGA, M. J1
[1] Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, Florida, United States
[2] Department of Hydraulic Engineering, Delft University of Technology, Delft, Netherlands
[3] Department of Oceanography, Naval Postgraduate School, Monterey, California, United States
Source

Geophysical research letters. 2010, Vol 37, Num 5 ; L05605.1-L05605.5 ; ref : 1/2 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)
Circulation Courant retour Courant sagittal Distribution vitesse Filament Lagrangien Matériau Modèle numérique Paquet onde Plateforme continentale interne Simulation numérique Structure cohérente Tourbillon Très basse fréquence Zone surf
Keyword (en)
circulation Eddying current Rip current Velocity distribution Filament Lagrangian materials numerical models Wave packet inner shelf digital simulation Coherent structures Vortex Very low frequency Surf zone
Keyword (es)
Resaca Corriente sagital Distribución velocidad Filamento Lagrangiano Paquete onda Plataforma continental interna Simulación numérica Torbellino Frecuencia muy baja Zona surf
Classification
Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences

Discipline
Earth sciences
Origin
Inist-CNRS
Database
PASCAL
INIST identifier
22624130

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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