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- The Use of the Primitive Equations of Motion in Numerical Prediction
- Continuity Equation Or Conservation of Mass;
- Chapter 2. the Continuous Equations Fig. 2.5: Schematic of the Shallow
- Complete Derivation of 2D Shallow-Water Model from the Primitive Equations Governing Geophysical Flows
- Mean-Flow Effects of Thermal Tides in the Mesosphere and Lower Thermosphere
- Studies of the General Circulation of the Atmosphere with a Simplified Moist General Circulation Model
- Primitive Equations Chaos and Numerical Weather Prediction
- Oceanic and Atmospheric Fluid Dynamics
- Consistent Shallow-Water Equations on the Rotating Sphere with Complete Coriolis Force and Topography
- Generic Frequency Dependence for the Atmospheric Tidal Torque of Terrestrial Planets P
- Hydrostatic, Quasihydrostatic, and Nonhydrostatic Ocean Modeling
- A Fourth Order Numerical Method for the Primitive Equations Formulated
- A Technique of Objective Analysis and Initialization for the Primitive Forecast Equations
- Description of a Global Shallow Water Model Based on the Spectral Transform Method
- Lecture 2: Basic Conservation Laws
- Section 2: Equations Governing Atmospheric Flow
- Compressible Primitive Equation: Formal Derivation and Stability of Weak Solutions Mehmet Ersoy, Timack Ngom, Mamadou Sy
- Atmospheric Modeling and the Community Atmospheric Model (CAM)
- Appendix B: the Primitive Equations
- Formulating the Equations of Ocean Models
- The Stochastic Primitive Equations in Two Space Dimensions with Multiplicative Noise
- Andrews, D.G., Holton, J.R., Leovy C.B. Middle Atmosphere Dynamics
- Atmospheric Tides and Their Roles in Vertical Coupling
- Ch2.6 Vertical Coords
- Part I a Few Basic Facts About Atmospheric Fluid Dynamics
- Potential~Vorticity
- Conservation Law of Momentum
- 4 Shallow Water Equations
- General Circulation Models
- Global Well-Posedness of the Ocean Primitive Equations with Nonlinear Thermodynamics
- The Primitive Equations Formulated in Mean Vorticity
- Dynamically Consistent, Quasi-Hydrostatic Equations for Global Models with a Complete Representation of the Coriolis Force
- Compressible Primitive Equations: Formal Derivation and Stability of Weak Solutions
- Numerical Integration of the Primitive Equations on the Hemisphere
- Quasi-Hydrostatic Primitive Equations for Ocean Global Circulation Models Carine Lucas, Madalina Petcu, Antoine Rousseau
- Primitive Equations of Large Scale Oceanic and Atmospheric Dynamics