Titlebook: Environmental Stratified Flows; Roger Grimshaw Book 2002 Springer Science+Business Media New York 2002 Coast.Ocean.Oceanography.Tide.atmos

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Obituary

Internal Solitary Waves,es in shallow coastal seas and in the atmospheric boundary layer. Commencing with the equations of motion for an inviscid, incompressible density-stratified fluid, we describe asymptotic reductions to model long-wave equations, such as the well-known Korteweg-de Vries equation. We then describe vari

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Internal Tide Transformation and Oceanic Internal Solitary Waves,cussed. Development of a model to describe this transformation is presented and is based on the Korteweg-de Vries equation. The model includes cubic as well as quadratic nonlinearity, dispersion, Earth’s rotation and quadratic dissipation. An initial waveform, described in terms of a vertical modal

Bernstein-test

Atmospheric Internal Solitary Waves,near the ground and those that occupy the entire troposphere. We present a survey of the observations of both types of solitary waves. The generation mechanisms differ substantially for these two types of solitary waves. Those that propagate in a shallow stratified layer are generated by small scale

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Turbulence in Stratified Fluids,est. These flow phenomena are described based on a dynamical framework provided by the equations of motion. Various broad categories of stratified turbulent flows are identified and their characteristics are briefly reviewed.

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Elements of Instability Theory for Environmental Flows,

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