The Formation of Nonzonal Jets over Sloped Topography
- Author
- BOLAND, Emma J. D1 ; THOMPSON, Andrew F2 ; SHUCKBURGH, Emily3 ; HAYNES, Peter H4
[1] The University of Cambridge, and The British Antarctic Survey, Cambridge, United Kingdom
[2] California Institute of Technology, Pasadena, California, United States
[3] The British Antarctic Survey, Cambridge, United Kingdom
[4] The University of Cambridge, Cambridge, United Kingdom - Source
Journal of physical oceanography. 2012, Vol 42, Num 10, pp 1635-1651, 17 p ; ref : 1 p.1/4
- CODEN
- JPYOBT
- ISSN
- 0022-3670
- Scientific domain
- Oceanography
- Publisher
- American Meteorological Society, Boston, MA
- Publication country
- United States
- Document type
- Article
- Language
- English
- Keyword (fr)
- Approximation quasi géostrophique Champ écoulement Circulation océanique Courant jet Dynamique océanique Déflexion Modèle 2 couches Modèle Structure cohérente Topographie
- Keyword (en)
- Quasi geostrophic approximation flow field ocean circulation Jet stream Ocean dynamics Deflection two-layer models models Coherent structures topography
- Keyword (es)
- Aproximación casi geostrófica Circulación oceánica Corriente chorro Dinámica oceánica Deflección Modelo 2 capas Modelo Topografía
- Classification
- Pascal
- 001 Exact sciences and technology / 001E Earth, ocean, space / 001E02 External geophysics / 001E02B Physics of the oceans / 001E02B02 Dynamics of the ocean (upper and deep oceans)
- Discipline
- External geophysics
- Origin
- Inist-CNRS
- Database
- PASCAL
- INIST identifier
- 26470978
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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DOI
10.1175/JPO-D-11-0152.1 
https://dx.doi.org/10.1175/JPO-D-11-0152.1
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