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Results: 1-11 |
Results: 11
EMERGENCE OF INERTIAL GYRES IN A 2-LAYER QUASI-GEOSTROPHIC OCEAN MODEL
Authors: OZGOKMEN TM CHASSIGNET EP
Citation: Tm. Ozgokmen et Ep. Chassignet, EMERGENCE OF INERTIAL GYRES IN A 2-LAYER QUASI-GEOSTROPHIC OCEAN MODEL, Journal of physical oceanography, 28(3), 1998, pp. 461-484
IMPACT OF WIND FORCING, BOTTOM TOPOGRAPHY, AND INERTIA ON MIDLATITUDEJET SEPARATION IN A QUASI-GEOSTROPHIC MODEL
Authors: OZGOKMEN TM CHASSIGNET EP PAIVA AM
Citation: Tm. Ozgokmen et al., IMPACT OF WIND FORCING, BOTTOM TOPOGRAPHY, AND INERTIA ON MIDLATITUDEJET SEPARATION IN A QUASI-GEOSTROPHIC MODEL, Journal of physical oceanography, 27(11), 1997, pp. 2460-2476
THE WALL-JET IN A ROTATING FLUID
Authors: STERN ME CHASSIGNET EP WHITEHEAD JA
Citation: Me. Stern et al., THE WALL-JET IN A ROTATING FLUID, Journal of Fluid Mechanics, 335, 1997, pp. 1-28
A MODEL COMPARISON - NUMERICAL SIMULATIONS OF THE NORTH AND EQUATORIAL ATLANTIC OCEANIC CIRCULATION IN-DEPTH AND ISOPYCNIC COORDINATES
Authors: CHASSIGNET EP SMITH LT BLECK R BRYAN FO
Citation: Ep. Chassignet et al., A MODEL COMPARISON - NUMERICAL SIMULATIONS OF THE NORTH AND EQUATORIAL ATLANTIC OCEANIC CIRCULATION IN-DEPTH AND ISOPYCNIC COORDINATES, Journal of physical oceanography, 26(9), 1996, pp. 1849-1867
INERTIAL GYRE SOLUTIONS FROM A PRIMITIVE EQUATION OCEAN MODEL
Authors: GRIFFA A CHASSIGNET EP COLES V OLSON DB
Citation: A. Griffa et al., INERTIAL GYRE SOLUTIONS FROM A PRIMITIVE EQUATION OCEAN MODEL, Journal of marine research, 54(4), 1996, pp. 653-677
EXTRATROPICAL LARGE-SCALE AIR-SEA INTERACTION IN A COUPLED AND UNCOUPLED OCEAN-ATMOSPHERE MODEL
Authors: OBRIEN EW CHASSIGNET EP
Citation: Ew. Obrien et Ep. Chassignet, EXTRATROPICAL LARGE-SCALE AIR-SEA INTERACTION IN A COUPLED AND UNCOUPLED OCEAN-ATMOSPHERE MODEL, Climate dynamics, 12(1), 1995, pp. 53-65
VORTICITY DISSIPATION BY WESTERN BOUNDARY CURRENTS IN THE PRESENCE OFOUTCROPPING LAYERS
Authors: CHASSIGNET EP
Citation: Ep. Chassignet, VORTICITY DISSIPATION BY WESTERN BOUNDARY CURRENTS IN THE PRESENCE OFOUTCROPPING LAYERS, Journal of physical oceanography, 25(2), 1995, pp. 242-255
THE INFLUENCE OF LAYER OUTCROPPING ON THE SEPARATION OF BOUNDARY CURRENTS .2. THE WIND-DRIVEN AND BUOYANCY-DRIVEN EXPERIMENTS
Authors: CHASSIGNET EP BLECK R ROOTH CGH
Citation: Ep. Chassignet et al., THE INFLUENCE OF LAYER OUTCROPPING ON THE SEPARATION OF BOUNDARY CURRENTS .2. THE WIND-DRIVEN AND BUOYANCY-DRIVEN EXPERIMENTS, Journal of physical oceanography, 25(10), 1995, pp. 2404-2422
WIND-FORCED VARIATIONS IN THE BRAZIL-MALVINAS CONFLUENCE REGION AS SIMULATED IN A COARSE RESOLUTION NUMERICAL-MODEL OF THE SOUTH-ATLANTIC
Authors: SMITH LT CHASSIGNET EP OLSON DB
Citation: Lt. Smith et al., WIND-FORCED VARIATIONS IN THE BRAZIL-MALVINAS CONFLUENCE REGION AS SIMULATED IN A COARSE RESOLUTION NUMERICAL-MODEL OF THE SOUTH-ATLANTIC, J GEO RES-O, 99(C3), 1994, pp. 5095-5117
LAYER OUTCROPPING IN NUMERICAL-MODELS OF STRATIFIED FLOWS
Authors: SUN S BLECK R CHASSIGNET EP
Citation: S. Sun et al., LAYER OUTCROPPING IN NUMERICAL-MODELS OF STRATIFIED FLOWS, Journal of physical oceanography, 23(8), 1993, pp. 1877-1884
THE INFLUENCE OF LAYER OUTCROPPING ON THE SEPARATION OF BOUNDARY CURRENTS .1. THE WIND-DRIVEN EXPERIMENTS
Authors: CHASSIGNET EP BLECK R
Citation: Ep. Chassignet et R. Bleck, THE INFLUENCE OF LAYER OUTCROPPING ON THE SEPARATION OF BOUNDARY CURRENTS .1. THE WIND-DRIVEN EXPERIMENTS, Journal of physical oceanography, 23(7), 1993, pp. 1485-1507
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