Titlebook: Ocean Dynamics; Dirk Olbers,Jürgen Willebrand,Carsten Eden Book 2012 Springer-Verlag Berlin Heidelberg 2012 Environmental Physics.Geophysi

Expostulate

collagen

Emasculate

地殼

秘傳

Geostrophic and Quasi-Geostrophic Motionsed by a small Rossby number. Geostrophic balance is assumed to dominate for lateral scales comparable to the Rossby radius – leading to the quasi-geostrophic approximation – or on scales comparable to Earth’s radius – the planetary geostrophic approximation. The latter set of equations can be reform

名詞

使困惑

Gravity Wavesg to mixing processes in the ocean interior, especially to diapycnal mixing. Surface gravity waves are effective in the exchange of momentum, heat, water, and gases between the ocean and the atmosphere, in addition to their practical significance for shipping.

Sleep-Paralysis

Long Wavesenerally called long waves) are of particular importance in the ocean. We have already encountered the hydrostatic limit for gravity waves in Sections 7.4.1 and 7.5. In addition to long gravity waves, planetary and topographic waves are in hydrostatic balance and hence also are long waves. Near the

熱心助人

Lagrangian Theory of Ocean Wavesfor incompressible flow, for isentropic compressible flow and for a rotating stratified fluid system. Some of the wave equations, derived and analyzed in the previous chapters, may be transferred into this Lagrangian framework, including Rossby waves and gravity waves. The present chapter is devoted

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