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Titlebook: IUTAM Symposium on Reynolds Number Scaling in Turbulent Flow; Proceedings of the I Alexander J. Smits Conference proceedings 2004 Springer

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A top-down theory for the neutral atmospheric surface layer compared with measurements, above the top of the surface layer play a fundamental role for the dynamics of this boundary layer. Eddies impinging onto the surface result in strongly distorted elongated eddies in the lower one third of the surface layer. This paper demonstrates that the theory gives predictions in good agreemen
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The Non Self Similar Scaling of Vorticity in a Shear Layer,ions, as measured by the standard deviation, was normalized using dissipation variables and compared at two streamwise locations. These data indicate that the vorticity fluctuations do not follow a self similar form. Rather, it was found that the values increase in magnitude with downstream distance
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Reynolds and Froude Number Scaling in Stably-Stratified Flows,table stratification, and to estimate the Reynolds number above which laboratory and numerical experiments of these flows must be conducted in order for the results to scale up to geophysical cases. For low Froude number .. and high enough Reynolds number .., where .. and .. are based upon the horiz
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Evidence of shear sheltering in atmospheric surface layer flow, provided the horizontal velocity of the eddy is not far from that of the mean flow and the size of the eddy is appropriate. Analysis of atmospheric surface layer data from two marine sites indicates that this effect may explain observed reduction of spectral energy within a wide frequency range in
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Iutam and Turbulence Symposium Opening Address,Professor Smits, Ladies and Gentlemen! Just now we have had our moment of silent remembrance on the tragic events which took place in New York and Washington just one year ago. First of all, let me express my deepest grief to the victims and their relatives and profound sympathy to all people concerned.
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