The significant wave height can be either the zero-crossing wave height, H1/3 or the spectral wave height, Hm0. The ratio of H1/3/Hm0 in deeper water is about 0.95; in shallow water the ratio increases and may reach 1.1 for sea and about 1.5 for swell. Conversion of Hm0 to H1/3 may be necessary when Hm0 is predicted by wave hindcast models or recorded by wave buoys while design formulae for coastal structures are based on H1/3. Existing conversion methods by Thompson and Vincent (1985), Battjes and Groenendijk (2000) and Goda (2010) were reviewed and compared with field data. Non-linear wave transformation in shallow water and the resulting H1/3/Hm0 ratio was investigated analytically with a line-model extending from deep to very shallow water. The effect of wave height, wave steepness, water depth and seabed slope were analysed. The findings were combined in a conversion formula of Hm0 and H1/3 that is applicable inside and outside the surf zone. The new approach was validated against field data.

You do not currently have access to this chapter.
Don't already have an account? Register

Purchased this content as a guest? Enter your email address to restore access.

Please enter valid email address.
Email address must be 94 characters or fewer.