Etudes et évaluation de processus océaniques par des hiérarchies ...
Etudes et évaluation de processus océaniques par des hiérarchies ... Etudes et évaluation de processus océaniques par des hiérarchies ...
72 CHAPITRE 4. ETUDES DE PROCESSUS OCÉANOGRAPHIQUES 2000] Wirth: Parameterization of baroclinic instability 583 Roberts, M. and D. Marshall. 1998. Do we require adiabatic dissipation schemes in eddy-resolving ocean models? J. Phys. Oceanogr., 28, 2050–2063. Salmon, R. 1980. Baroclinicinstabilityand geostrophicturbulence.Geophys.Astrophys.Fluid Dyn., 15, 11–37. Smagorinsky, J. 1963. General circulation experiments with the primitive equations: I. The basic experiment. Mon. Wea. Rev., 91, 99–164. Straub, D. N. 1993. On the transport and angular momentum balance of channel models of the Antarctic Circumpolar Current. J. Phys. Oceanogr., 23, 776–782. Treguier,A. M. 1999. Evaluatingeddy mixing coefficientsfrom eddy-resolvingocean models:A case study. J. Mar. Res., 57, 89–108. Treguier,A. M., I. M. Held and V. D. Larichev. 1997. Parameterizationof quasi-geostrophiceddies in primitive equation ocean models. J. Phys. Oceanogr., 27, 567–580. Welander, P. 1973. Lateral friction in the ocean as an effect of potential vorticity mixing. Geophys. Fluid Dyn., 5, 173–189. tel-00545911, version 1 - 13 Dec 2010 Received: 3 January, 2000; revised: 8 May, 2000.
4.3. A NON-HYDROSTATIC FLAT-BOTTOM OCEAN MODEL ENTIRELY BASE ON FOURIER EX 4.3 A non-hydrostatic flat-bottom ocean model entirely base on Fourier expansion tel-00545911, version 1 - 13 Dec 2010
- Page 27 and 28: 3.2. PROCESSUS SUBMÉSO ECHELLES ET
- Page 29 and 30: 3.4. RETOUR À LA GRANDE ECHELLE PA
- Page 31 and 32: 3.5. MA RECHERCHE DANS LE CONTEXTE
- Page 33 and 34: 3.5. MA RECHERCHE DANS LE CONTEXTE
- Page 35 and 36: Bibliographie tel-00545911, version
- Page 37 and 38: Deuxième partie tel-00545911, vers
- Page 39 and 40: 33 Curriculum Vitae du Dr. Achim WI
- Page 41 and 42: 35 tel-00545911, version 1 - 13 Dec
- Page 43 and 44: Colloque bilan LEFE, Plouzané, Mai
- Page 45 and 46: Troisième partie tel-00545911, ver
- Page 47 and 48: Chapitre 4 Etudes de Processus Océ
- Page 49 and 50: 4.1. VARIABILITY OF THE GREAT WHIRL
- Page 51 and 52: 4.1. VARIABILITY OF THE GREAT WHIRL
- Page 53 and 54: 4.1. VARIABILITY OF THE GREAT WHIRL
- Page 55 and 56: 4.1. VARIABILITY OF THE GREAT WHIRL
- Page 57 and 58: 4.1. VARIABILITY OF THE GREAT WHIRL
- Page 59 and 60: 4.1. VARIABILITY OF THE GREAT WHIRL
- Page 61 and 62: 4.1. VARIABILITY OF THE GREAT WHIRL
- Page 63 and 64: 4.1. VARIABILITY OF THE GREAT WHIRL
- Page 65 and 66: 4.2. THE PARAMETRIZATION OF BAROCLI
- Page 67 and 68: 4.2. THE PARAMETRIZATION OF BAROCLI
- Page 69 and 70: 4.2. THE PARAMETRIZATION OF BAROCLI
- Page 71 and 72: 4.2. THE PARAMETRIZATION OF BAROCLI
- Page 73 and 74: 4.2. THE PARAMETRIZATION OF BAROCLI
- Page 75 and 76: 4.2. THE PARAMETRIZATION OF BAROCLI
- Page 77: 4.2. THE PARAMETRIZATION OF BAROCLI
- Page 81 and 82: 4.3. A NON-HYDROSTATIC FLAT-BOTTOM
- Page 83 and 84: 4.3. A NON-HYDROSTATIC FLAT-BOTTOM
- Page 85 and 86: 4.3. A NON-HYDROSTATIC FLAT-BOTTOM
- Page 87 and 88: 4.3. A NON-HYDROSTATIC FLAT-BOTTOM
- Page 89 and 90: 4.3. A NON-HYDROSTATIC FLAT-BOTTOM
- Page 91 and 92: 4.3. A NON-HYDROSTATIC FLAT-BOTTOM
- Page 93 and 94: 4.3. A NON-HYDROSTATIC FLAT-BOTTOM
- Page 95 and 96: 4.3. A NON-HYDROSTATIC FLAT-BOTTOM
- Page 97 and 98: 4.4. TILTED CONVECTIVE PLUMES IN NU
- Page 99 and 100: 4.4. TILTED CONVECTIVE PLUMES IN NU
- Page 101 and 102: 4.4. TILTED CONVECTIVE PLUMES IN NU
- Page 103 and 104: 4.4. TILTED CONVECTIVE PLUMES IN NU
- Page 105 and 106: 4.4. TILTED CONVECTIVE PLUMES IN NU
- Page 107 and 108: 4.4. TILTED CONVECTIVE PLUMES IN NU
- Page 109 and 110: 4.5. MEAN CIRCULATION AND STRUCTURE
- Page 111 and 112: 4.5. MEAN CIRCULATION AND STRUCTURE
- Page 113 and 114: 4.5. MEAN CIRCULATION AND STRUCTURE
- Page 115 and 116: 4.5. MEAN CIRCULATION AND STRUCTURE
- Page 117 and 118: 4.5. MEAN CIRCULATION AND STRUCTURE
- Page 119 and 120: 4.5. MEAN CIRCULATION AND STRUCTURE
- Page 121 and 122: 4.5. MEAN CIRCULATION AND STRUCTURE
- Page 123 and 124: 4.5. MEAN CIRCULATION AND STRUCTURE
- Page 125 and 126: 4.6. ESTIMATION OF FRICTION PARAMET
- Page 127 and 128: 4.6. ESTIMATION OF FRICTION PARAMET
72 CHAPITRE 4. ETUDES DE PROCESSUS OCÉANOGRAPHIQUES<br />
2000] Wirth: Param<strong>et</strong>erization of baroclinic instability<br />
583<br />
Roberts, M. and D. Marshall. 1998. Do we require adiabatic dissipation schemes in eddy-resolving<br />
ocean mo<strong>de</strong>ls? J. Phys. Oceanogr., 28, 2050–2063.<br />
Salmon, R. 1980. Baroclinicinstabilityand geostrophicturbulence.Geophys.Astrophys.Fluid Dyn.,<br />
15, 11–37.<br />
Smagorinsky, J. 1963. General circulation experiments with the primitive equations: I. The basic<br />
experiment. Mon. Wea. Rev., 91, 99–164.<br />
Straub, D. N. 1993. On the transport and angular momentum balance of channel mo<strong>de</strong>ls of the<br />
Antarctic Circumpolar Current. J. Phys. Oceanogr., 23, 776–782.<br />
Treguier,A. M. 1999. Evaluatingeddy mixing coefficientsfrom eddy-resolvingocean mo<strong>de</strong>ls:A case<br />
study. J. Mar. Res., 57, 89–108.<br />
Treguier,A. M., I. M. Held and V. D. Larichev. 1997. Param<strong>et</strong>erizationof quasi-geostrophiceddies in<br />
primitive equation ocean mo<strong>de</strong>ls. J. Phys. Oceanogr., 27, 567–580.<br />
Welan<strong>de</strong>r, P. 1973. Lateral friction in the ocean as an effect of potential vorticity mixing. Geophys.<br />
Fluid Dyn., 5, 173–189.<br />
tel-00545911, version 1 - 13 Dec 2010<br />
Received: 3 January, 2000; revised: 8 May, 2000.