Wave Overtopping Discharge for Very Gently Sloping Foreshores
The spectral wave period T m − 1 , 0 at the toe of sea-dikes is a crucial parameter to predict wave overtopping discharge over sea-dikes. It is known from literature that this period quickly increases when waves reach shallow foreshores; however, sometimes the assumption is made that the wave period...
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Veröffentlicht in: | Water (Basel) 2020-06, Vol.12 (6), p.1695 |
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Hauptverfasser: | , , , |
Format: | Artikel |
Sprache: | eng |
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