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Turbulence spectra from a tidal channel

Published online by Cambridge University Press:  28 March 2006

H. L. Grant
Affiliation:
Pacific Naval Laboratory of the Defence Research Board of Canada, Esquimalt, B.C. Canada
R. W. Stewart
Affiliation:
Pacific Naval Laboratory of the Defence Research Board of Canada, Esquimalt, B.C. Canada
A. Moilliet
Affiliation:
Pacific Naval Laboratory of the Defence Research Board of Canada, Esquimalt, B.C. Canada

Abstract

This paper describes the use of a hot film flowmeter in the sea and presents experimental measurements of the ‘downstream’ component of turbulent velocity in a tidal channel. The Reynolds number of the flow is about 108 and the scale of the turbulence is so large that a ship is carried about to a considerable extent by the energy-containing eddies. Under these conditions, a velocity measuring probe attached to a ship cannot be used for reliable measurements in the energy-containing range of the spectrum. It is possible, however, to observe the intertial and dissipation ranges. Records have been made at various stages of the tide. The one-dimensional spectra are found to be proportional to $k|^{-{\frac {5}{3}}}$ for several decades in k as predicted by Kolmogoroff, and a value is given for Kolmogoroff's constant. In the dissipation range there is close agreement with both Kovasznay's theory and Heisenberg's theory. These two theories are not very different in the low wave-number end of the range and the observations do not extend to high enough wave-numbers to distinguish between them.

Type
Research Article
Copyright
© 1962 Cambridge University Press

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References

Anonymous 1959 Chart no. 3565, Discovery Passage. Canadian Hydrographic Service, Surveys and Mapping Branch, Department of Mines and Technical Surveys, Ottawa.
Anonymous 1959 Pacific Coast Tide and Current Tables. Canadian Hydrographic Service.
Anonymous 1960 Pacific Coast Tide and Current Tables. Canadian Hydrographic Service.
Batchelor, G. K. 1953 The Theory of Homogeneous Turbulence.. Cambridge University Press.
Batchelor, G. K. & Townsend, A. A. 1949 Proc. Roy. Soc. A, 199, 238.
Betchov, R. 1957 J. Fluid Mech. 3, 205.
Bowden, K. F. & Fairbairn, L. A. 1956 Proc. Roy. Soc. A, 237, 422.
Corrsin, S. 1958 N.A.C.A. Research Memorandum, RM58B11.
Grant, H. L., Moilliet, A. & Stewart, R. W. 1959 Nature, Lond., 811, 808.
Heisenberg, W. 1948 Proc. Roy. Soc. A, 195, 402.
Hinze, J. O. 1959 Turbulence. New York and London: McGraw-Hill Book Co.
Kistler, A. L. & Vrebalovich, T. 1961 Bull. Amer. Phys. Soc. II, 6, 207.
Klebanoff, P. S. 1955 N.A.C.A. Report, no. 1247.
Kolesnikov, A. G., Panteleyev, N. A., Pyrkin, Yu. G., Petrov, V. P. & Ivanov, V. N. 1958 Isvest. Akad. Nauk SSSR, Ser. Geofiz. pp. 40513 (English edition published by American Geophysical Union, July 1959, pp. 229–34).
Kolesnikov, A. G. 1960 Izvest. Akad. Nauk SSSR, Ser. Geofiz. pp. 161423 (English edition published by American Geophysical Union, April 1961, pp. 1079–84).
Kolmogoroff, A. N. 1941 C.R. Acad. Sci., U.R.S.S. 30, 301.
Kovasznay, L. S. G. 1948 J. Aero. Soc. 15, 745.
Laufer, J. 1951 N.A.C.A. Rep. no. 1053.
Laufer, J. 1954 N.A.C.A. Rep. no. 1174.
Ling, S. C. 1955 Ph.D. dissertation, University of Iowa.
Munk, W. H. & Macdonald, G. J. F. 1960 The Rotation of the Earth. Cambridge University Press.
Obukhov, A. M. 1941 C.R. Acad. Sci., U.R.S.S. 32, 19.
Reid, W. H. 1960 Phys. Fluids, 3, 72.
Sandborn, V. A. 1959 J. Fluid Mech. 6, 221.
Stewart, R. W. & Townsend, A. A. 1951 Phil. Trans. A, 243, 359.