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

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978-1-4757-7668-3Springer Science+Business Media New York 2002

最有利

偏离

1387-6961 any contexts, ranging from industrial settings to the oceanic and atmospheric environments. It is the latter topic which is the focus of this book. Both the ocean and atmosphere are characterised by the basic vertical density stratification, and this feature can affect the dynamics on all scales ran

冒失

Adoption-centric Usability Engineeringty differences. However, the theory for the internal two-layer bore is successful only for Boussinesq fluids and even then only for a certain class of bores. The main difficulty with the hydraulic theory for a two-layer bore is determining how the necessary dissipation is distributed between the layers.

变异

Book 2002ts, ranging from industrial settings to the oceanic and atmospheric environments. It is the latter topic which is the focus of this book. Both the ocean and atmosphere are characterised by the basic vertical density stratification, and this feature can affect the dynamics on all scales ranging from

aerial

Internal Solitary Waves,ous solitary wave solutions, and propose a variable-coefficient extended Korteweg-de Vries equations as an appropriate evolution equation to describe internal solitary waves in environmental situations, when the effects of a variable background and dissipation need to be taken into account.

beta-cells

Adoption, Family and the Paradox of Originso compare these observations with weakly nonlinear solitary wave theory. It appears that models with a deep passive upper layer are generally not applicable, while Korteweg-de Vries models, perhaps enhanced with higher-order nonlinearity, provide the best comparison; but it remains unclear what constitutes a suitable upper boundary condition.

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Atmospheric Internal Solitary Waves,o compare these observations with weakly nonlinear solitary wave theory. It appears that models with a deep passive upper layer are generally not applicable, while Korteweg-de Vries models, perhaps enhanced with higher-order nonlinearity, provide the best comparison; but it remains unclear what constitutes a suitable upper boundary condition.

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Silent-Ischemia