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

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Forced Wavesct and can be created by other waves. We have discussed a general treatment in Section 9.6, using a Lagrangian framework. We expand the treatment to a situation where a random ensemble of waves is an adequate representation for the wave field.

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Geostrophic Turbulencection 12.2 is devoted to the more realistic inhomogeneous situation of the real ocean. In Section 12.3 we discuss alternative averaging frameworks to differentiate between advective and diffusive effects of turbulent mixing.

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Small-Scale Turbulenceiscussed in Section 11.1, while basic concepts of turbulent mixing are described in Section 11.2. The application to the real, i. e. inhomogeneous, ocean in the presence of density stratification and large gravity force and the development of basic turbulence closure schemes can be found in Section 11.3.

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The Wind-Driven Circulationstigated using the model BARBI. This model represents the interaction of barotropic and baroclinic fields in a minimal way. The spin-up of the wind-driven circulation by wave processes was presented in Section 8.2.6.

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Physics of Heat Exchange with the Environment,t temperature difference (. .C.). In the case of evaporation on the skin, the water vapour pressure difference (.) between the body surface and the ambient air substitutes for the temperature difference.

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