Alcune registrazioni di onde effettuate nella stazione di misura entro la diga foranea di Genova, producono nuove conferme di una tendenza delle onde più alte verso forme di quasi-determinismo, similmente a quanto è stato recentemente trovato dall'autore per i processi stazionari gaussiani.
Referenze Bibliografiche
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[7] C.CARRY and G.CHABERT D'HIERES (1957) - Compléments sur le calcul approché au troisième ordre d'un clapotis parfait monochromatique, «C.R. Acad. Sc. Paris», p. 1377.
[8] W.J. PIERSON and L. MOSKOWITZ (1967) - A proposed spectral form for fully developed wind seas based on the similarity theory of S.A. Kitaigorodskii, «J. Geoph. Res.», 69, p.5181.
[9] K. HASSELMAN et al. (1973) - Measurement of wind-wave growth and swell decay during the Joint North Sea Wave Project (JONSWAP), «Deut. Hydrogr. Zeit.», Suppl. A, 8, pp. 95.
[10] L. BORGMAN (1973) - Probabilities for highest wave in hurricane, «J. Waterways, Harbours and Coast. Engr. ASCE», 99, WWR, p. 185.
R.E. HARING, A.R. OSBORNE and L.P. SPENCER (1976) - Extreme wave parameters based on continental shelf storm wave records, Proc. 15th Conf. on Coast. Engr., ASCE, 1, p. 151.
G.Z. FORRISTALL (1978) - On the statistical distribution of wave heights in a storm. «J. Geoph. Res.», 83, p. 2353.
M.S. LONGUET-HIGGINGS (1980) - On the distribution of the heights of sea waves: some effects of nonlinearity and finite band width, «J. Geoph. Res.», 85, p. 1519.