Variability of anomalous transport exponents versus different physical situations in geophysical and laboratory turbulence-Reference-Cited by-同舟云学术

Variability of anomalous transport exponents versus different physical situations in geophysical and laboratory turbulence

Published: Issue: Volume: Page:1-33
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Container-title:Lévy Flights and Related Topics in Physics
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Author:

Tsinober A.

Publisher

Springer Berlin Heidelberg

Link

http://link.springer.com/content/pdf/10.1007/3-540-59222-9_23.pdf

Reference70 articles.

1. Tsinober A., Kit E. and Dracos T. 1992 Experimental investigation of the field of velocity gradients in turbulent flows. J. Fluid Mech. 242, 169–192.

2. Kit E., Tsinober A. & Dracos T. 1993 Velocity gradients in a turbulent jet flow, in Proceedings of the 4th European Conference on Turbulence, ed. F.T.M. Nieuwstadt (Kluwer), Appl. Sci. Res., 51, 185–190.

3. Richardson L. F. 1926 Atmospheric diffusion on a distance-neighbor graph, Proc. Roy. Soc. London, A110, 709–737.

4. Taylor G. I. 1959 The present position in the theory of turbulent diffusion, In Atmospheric Diffusion and Air Pollution, ededs.} F. N. Frenkiel and P. A. Sheppard, pp. 101–112, Academic Press, New York London.

5. Contrary to the velocity field experimental results for passive scalars are significantly different from ‘theoretical’ predictions. Among the reasons for such ‘misbehavior’ of passive scalars in turbulent flows is the fact that the passive scalar carries the signature (at least in part) of the complex structure of the turbulent velocity field and that even in a purely laminar flow the passive scalar can behave in a turbulent manner (Lagrangian chaos). For an overview and a partial list of references on ‘misbehavior’ of a passive scalar in turbulent flows see [45] and Holzer M. and Siggia E. 1994 Turbulent mixing of a passive scalar, Phys. Fluids, 6, 1820–1837.

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