Titlebook: Dynamics of Internal Gravity Waves in the Ocean; Yu. Z. Miropol’sky,O. D. Shishkina Book 2001 Springer Science+Business Media Dordrecht 20

慌張

Insubordinate

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噴油井

Brief Information about Oceanic ThermohydrodynamicsIn this chapter the principles of oceanic thermohydrodynamics are presented briefly. For the relatively short internal waves with length scales less than 100 km, considered in this hook, it is obviously possible to neglect the radius of the Earth restricting the local description.

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MITE

Resonant Interactions of Wave Triads and Kinetic Equation for Oceanic Internal Waves’ SpectrumNonlinear effects while internal waves propagate in the ocean are caused not only by the self-modulation of almost monochromatic internal wave packets, but also by the interaction of internal waves with different wave numbers, frequencies and mode numbers.

拘留

Equations of the Theory of Internal Wavesf oceanic thermodynamics derived in Chapter 1. A list of different forms of these equations for special cases plane (twodimensional) stationary and nonstationary problems, equations linearized relative to the state of rest and to background flow — is given here for convenience.

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辯論的終結(jié)

Propagation of Internal Waves in Horizontally Inhomogeneous Oceanaracteristic horizontal inhomogeneities are: bottom unevenness; horizontal inhomogeneities of the density field; and horizontal variations of the mean flows. The influence of these phenomena on internal waves’ propagation will be studied in this chapter.