Wind mediated vorticity-generation and eddy-confinement, leeward of the Madeira Island: 2008 numerical case study

Author:

Couvelard X.,Caldeira R.M.A.,Araújo I.B.,Tomé R.

Funder

FCT-Portuguese National Science and Technology Foundation

Publisher

Elsevier BV

Subject

Atmospheric Science,Computers in Earth Sciences,Geology,Oceanography

Reference57 articles.

1. Antonov, J.I., Locarnini, R.A., Boyer, T.P., Mishonov, A.V., Garcia, H.E., 2006. In: Levitus, S. (Ed.), World Ocean Atlas 2005, vol. 2: Salinity. NOAA Atlas NESDIS 62. Government Printing Office, Washington, DC, p. 182.

2. Island Induced (Sub) Mesoscale Features Around Madeira Archipelago (Initial Findings);Araújo,2010

3. Numerical simulation of flow around a tall isolated seamount. Part I: Problem formulation and model accuracy;Beckmann;J. Phys. Oceanogr.,1993

4. A new convective adjustment scheme. Part I: Observational and theoretical basis;Betts;Quart. J. Roy. Meteorol. Soc.,1986

5. A new convective adjustment scheme. Part II: Single column tests using gate wave, bomex, and arctic air-mass data sets;Betts;Quart. J. Roy. Meteorol. Soc.,1986

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