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Online First:31 January 2013,
Published:1997
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Ke-jian, W., Fu, S. General theory for apparent energy distribution of sea waves., Chin. J. Ocean. Limnol. 15, 322–331 (1997). https://doi.org/10.1007/BF02850566
This paper presents a general theory for the apparent energy distribution of sea waves. Using the joint distribution of wave periods and heights proposed earlier by the second author
the authors define the generalized apparent energy distribution and derive the analytical form of the so called generalized outer frequency spectrum ornth-order frequency spectrum. Some possible relationships between it and the Fourier frequency spectrum are discussed. It is shown that the widely used Bretschneider spectrum can be easily obtained from the above definition and that generalized outer frequency spectrum has equilibrium range with exponent −(n+3) whose upper limit is −3.
Bretschneider, C. L., 1959. Wave variability and wave spectra for wind-generated gravity waves. Tech. Memo. No. 113. Beach Erosion Board, U. S. Army Corps of Engineers.
Cavanic, A., Arhan, M., Ezraty, R., 1976. A statistical relationship between heights and periods of storm sea.In: Proc. Conf., On Behaviour of Offshore Structures, Trondheim, Norwigian Inst. of Tech. pp. 334–360.
Goda, Y., 1978. The observed joint distribution of periods and heights of sea waves.In: Pro. 16th Int. Conf. on Coastal Eng., Sydney, Australia, pp. 227–246.
Huang, N. E., Tung, C. C., Long, S. R., 1990. The sea (eds. Le Mechante, B. & Hanes, D. M.), John wiley and Sons, Inc., New York. PP. 197–237.
Kitaigorodskii, S. A., Krasitskii, V. P., Zaslavskii, M. M., 1975. On Phillips' theory of equilibrium range in the spectra of wind-generated waves.J. Phys. Oceanogr. 5: 410–420.
Kitaigorodskii, S. A., 1983. On the theory of the equillibrium range in the spectrum of wind-generated gravity waves.J. Phys. Oceanogr. 13: 816–827.
Lindgreen, G., Rychilk, I., 1982. Wave characteristic distribution for Gaussian waves wavelength, amplitude and steepness.Ocean Eng. 9: 411–432.
Longuet-Higgins, M. S., 1975. On the joint distribution of the periods and amplitudes of sea waves.J. Geophys. Res. 80: 2688–2694.
Longuet-Higgins, M. S., 1983. On the joint distribution of the periods and amplitudes in random wave field.Proc. Roy. Soc. Lond. Ser. A.389: 241–258.
Phillips, O. M., 1958. The equillibrium range in the spectrum of wind-generated waves.J. Fluid Mech. 4: 426–434.
Phillips, O. M., 1985. Spectral and statistical properties of the equilibrium range in wind-generated gravity waves.J. Fluid Mech. 156: 505–531.
Pierson, W. J. Jr. Moskowitz, L. 1964 A proposed spectral form for developed wind seas based on the similarity theory of S. A. Kitaigorodskii.J. Geophys. Res. 69: 5181–5190.
Sun Fu, 1987. On the joint distribution of the periods and heights of sea waves.Acta Oceanologica Sinica 6: 503–509.
Sun Fu, Ding, Pingxing, 1994. A note on Bretschneider spectrum.Oceanol. et Limnol. 25: 395–398. (in Chinese with English abstract)
Sun Fu, Ding Pingxing, 1995. Apparent energy distribution of sea waves.Science in China (Series B).38: 116–123.
Toba, Y., 1973. Local balance in the air-sea boundary process. II. On the spectrum of wind waves.J. Oceanogr. Soc. Japan. 29: 209–220.
Yamasaki, H., Herbich, J. B., 1985. Determination of wave height spectrum by means of a joint probability density function.J. Geophys. Res. 90: 3381–3390.
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