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The main period parameter obtainable from a wave spectrum is the peak period Tp defined as the inverse of the peak frequency fp. The period parameters defined by the zero-upcrossing (or zero-downcrossing)method such as T1l3cannot be derived from a wave spectrum theoretically. Their relationship with Tp must be established on the basis of many field data or by means Statwtid Properties and Speetm of Sea Waves 43 of numerical simulations. 14 As the spectral peak becomes sharp, the differences between various wave period parameters become small and these periods approach the peak period Tp.

K. Ochi and E. N. Hubble, “On six-parameter wave spectra,” Pmc. 15th Int. Conf. Coastal Engrg. (Hawaii, 1976), pp. 301-328. 14. Y. Goda, “Statistical variability of sea state parameters as a function of a wave spectrum,” Coastal Engineering in Japan 31 (1) (1988), pp. 39-52. H. Gunther, W. Rosenthal and C. Vincent, “Similarity of the wind 15. E. BOUWS, wave spectrum in finite depth water,” J. Geophys. Res. 90 (Cl)pp. 975-986. 16. N. E. , “A unified two-parameter wave spectral model for a general sea state,” J.

24. Y. Goda, “A comparative review on the functional forms of directional wave spectrum,” Coastal Engineering Journal 41 (1) (1999), pp. 1-20. 25. For example, Y. Goda, “A review on statistical interpretation of wave data,” Rept. Port and Harbour Res. Inst. 18 (1) (1979), pp. 5-32. 26. Y. Goda, “A unified nonlinearity parameter of water waves,” Rept. Port and Harbour Res. Inst. 22 (3) (1983), pp. 3-30. 27. The IAHR Working Group on Wave Generation and Analysis. “List of sea&ate parameters,” J. , and Ocn.

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Airbus A320 SOP 08dRNAV GPS Approach


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