UUU VVV Van De Kreeke, Jacobus, and Jef T. F. Zimmerman, "Gravitational circulation in well- and partially-mixed estuaries," In _The Sea, Vol. 9, Part A: Ocean Engineering Science_, John Wiley & Sons, N.Y., 1990, pp. 495-521. 1. Introduction 2. Basic equations and parametrizations a. Equations b. Vertical eddy viscosity and diffusivity c. Longitudinal diffusivity 3. Nondimensional equations and parameter regimes a. Scaling b. Diffusive scaling c. Convective scaling d. Nondimensional parameters in terms of velocity scales 4. Similarity solutions of Hansen and Rattray 5. Perturbation solution for the diffusive regime 6. Solutions for the convective regime 7. Conclusions Van Delden, Aarnout, "The dynamics of meso-scale atmospheric circulations," Physics Reports, Vol. 211, 1992, pp. 251-374. 1. General introduction 2. A phenomenological introduction to the meso-scale 3. Models, equations and approximations 3.1 Basic equations 3.2 Approximations 3.3 Balanced circulations 3.4 Simplified models of the atmosphere 4. Stability 4.1 Stability of stratified shear flow 4.2 Symmetric stability of thermal wind balance 5. Adjustment 5.1 Geostrophic adjustment in the shallow-water layer model 5.2 Adjustment to thermal wind balance in the shallow Boussinesq model 5.3 The meso-scale as a transition regime between dynamic regimes 5.4 Unbalanced flow 5.5 Balanced flow 6. Forcing 6.1 Latent heat release 6.2 Water loading, rainfall and evaporation 6.3 Vertical wind-shear 6.4 Frontogenesis and jet streaks 6.5 Topography 6.6 Friction 6.7 Diabatic heating 7. Conclusion 7.1 Prediction of meso-scale weather systems 7.2 Final remarks Veronis, George, "Analogy between rotating and stratified fluids," Ann. Rev. of Fluid Mech., Vol. 2, 1970, pp. 37-66. Veronis, George, "Large scale ocean circulation," Advances in Applied Mechanics, Vol. 13, 1973, pp. 1-92. Introduction 1. The equilibrium figure of a self-gravitating, rotating, homogeneous mass of fluid 2. Transformations of the equations of motion of a fluid 3. The Coriolis acceleration 4. Thermodynamic simplifications - the Boussinesq approximation 5. Scaling of the equations 6. Geostrophic flow 7. Frictional dissipation 8. Modeling of current systems 9. The thermohaline circulation 10. Abyssal circulation 11. Laboratory simulation of large scale circulation Veronis, George, "Dynamics of large-scale ocean circulation," In _Evolution of Physical Oceanography_, Bruce A. Warren, Carl Wunsch, eds., MIT, 1981, pp. 504-548. 1. Introduction and summary 2. The equations for large-scale dynamics 3. The quasi-geostrophic equations and the beta-plane a. Continuous stratification b. Equations more commonly encountered c. Layered stratification 4. Ekman layers a. Pure Ekman layers b. Effect of Ekman layers on interior flows c. Additional considerations 5. Steady linear models of the wind-driven circulation a. Sverdrup transport b. Stommel's friction model c. Topography and lateral friction d. Laboratory models 6. Preliminary nonlinear considerations 7. Why does the Gulf Stream leave the coast? 8. Thermohaline circulation a. Continuous models for an open basin b. Layered models 9. Free waves for a constant-depth two-layer ocean on the beta-plane 10. Effect of bottom topography on quasi-geostrophic waves a. Two-layer model b. Uniform stratification 11. Baroclinic instability a. Linear theory b. Finite-amplitude effects 12. Effect of nonlinearity and turbulence a. Nonlinear effects with constant depth b. Effects of topography in two-layer flow c. Closed basin circulation Voit, S. S., "Tsunamis," Ann. Rev. of Fluid Mech., Vol. 19, 1987, pp. 217-236.