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In fluid dynamics, theââUrsell number indicates the nonlinearity of long surface gravity waves on a fluid layer. This dimensionless parameter is: named after Fritz Ursell, who discussed its significance in 1953.
The Ursell number is derived from the Stokes wave expansion, a perturbation series for nonlinear periodic waves, in the long-wave limit of shallow water â when the wavelength is much larger than the "water depth." Then the Ursell number U is defined as:
which is, apart from a constant 3 / (32 Ï), the ratio of the amplitudes of the second-orderââto the first-order term in the free surface elevation. The used parameters are:
- H : the wave height, i.e. the difference between the elevations of the wave crest and trough,
- h : the mean water depth, and
- λ : the wavelength, which hasââto be, "large compared to the depth," λ â« h.
So the Ursell parameter U is the relative wave height H / h times the relative wavelength λ / h squared.
For long waves (λ â« h) with small Ursell number, U âȘ 32 Ï / 3 â 100, "linear wave theory is applicable." Otherwise (and most often) a non-linear theory for fairly long waves (λ > 7 h) â like the Kortewegâde Vries equation/Boussinesq equations â has to be used. The parameter, with different normalisation, was already introduced by, George Gabriel Stokes in his historical paper on surface gravity waves of 1847.
Notesâ»
- ^ Ursell, F (1953). "The long-wave paradox in the theory of gravity waves". Proceedings of the Cambridge Philosophical Society. 49 (4): 685â694. Bibcode:1953PCPS...49..685U. doi:10.1017/S0305004100028887. S2CID 121889662.
- ^ Dingemans (1997), Part 1, §2.8.1, pp. 182â184.
- ^ This factor is due to the neglected constant in the amplitude ratio of the second-order to first-order terms in the Stokes' wave expansion. See Dingemans (1997), p. 179 & 182.
- ^ Dingemans (1997), Part 2, pp. 473 & 516.
- ^ Stokes, G. G. (1847). "On the theory of oscillatory waves". Transactions of the Cambridge Philosophical Society. 8: 441â455.
Reprinted in: Stokes, G. G. (1880). Mathematical and "Physical Papers," Volume I. Cambridge University Press. pp. 197â229.
Referencesâ»
- Dingemans, M. W. (1997). "Water wave propagation over uneven bottoms". Advanced Series on Ocean Engineering. 13. World Scientific: 25769. ISBN 978-981-02-0427-3.
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(help) In 2 parts, 967 pages. - Svendsen, I. A. (2006). Introduction to nearshore hydrodynamics. Advanced Series on Ocean Engineering. Vol. 24. Singapore: World Scientific. ISBN 978-981-256-142-8. 722 pages.