Titlebook: Waves in the Ocean and Atmosphere; Introduction to Wave Joseph Pedlosky Textbook 2003 Springer-Verlag Berlin Heidelberg 2003 Fluid Dynamics

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Energy and Energy Flux in Rossby Waves, is horizontally non-divergent and therefore has no effect on the wave energy. To discuss the real energy flux, one has to include the divergent, non-geostrophic .(ε) part of the velocity field as well as the pressure contribution at this order. This would be a messy business, and what is worse is t

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Vertical Propagation of Waves: Steady Flow and the Radiation Condition,uld imagine that internal gravity waves, if the fluid is stratified, would be generated. Such situations are of interest in their own right, but additionally they force us to carefully examine the radiative properties of the waves, which must be understood, sometimes, to actually solve the problem.

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Laplace Tidal Equations and the Vertical Structure Equation,s that the analysis of the homogeneous model can be carried over, in important cases, to the motion of a stratified fluid. A vertical modal decomposition can be done for these cases, and we will be able to show that the equations for . are analogous to the equations for the single layer. Exactly wha

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Stratified Quasi-Geostrophic Motion and Instability Waves,we consider will be in near (quasi-)geostrophic balance, but we will develop the equations in an informal, heuristic way, leaning heavily on the formal analysis of Lecture 15. We will also employ the beta-plane approximation so that we are assuming that two parameters, ε = ./... β. /.., are both sma

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Large-Scale Hydrostatic Motions, occurring in the thermocline will have a vertical scale of a kilometer or less, while the horizontal scales might be of the order of hundreds of kilometers. Motions in the ocean induced by traveling meteorological systems will have such large scales. If the . has such disparate scales in the vertic

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