Convective and Shear Flow Turbulence with Rotation
As an introduction to this section we present an extension of the discussion of Mory  to include a case of more general geophysical significance, where the source of the initial turbulent motion is a natural one rather than the rather artificial case of turbulence generated by an oscillating grid. Firstly we give a somewhat different argument to show the effect of rotation on turbulent fluctuations. Referring to figure 1, consider a typical turbulent eddy of scale, l, (the integral scale) and characteristic velocty, u′, (the rms velocity fluctuation).
KeywordsCritical Reynolds Number Turbulent Channel Flow Baroclinic Instability Longitudinal Vortex Pressure Gradient Force
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