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DeutschFile:Shoaling coefficient as a function of depth.svg
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Summary
| Description | English: Shoaling coefficient KS as a function of relative water depth h/L0, describing the effect of wave shoaling on the wave height – based on conservation of energy and results from Airy wave theory. The local wave height H at a certain mean water depth h is equal to H = KS H0, with H0 the wave height in deep water (i.e. when the water depth is greater than about half the wavelength). The shoaling coefficient KS depends on h/L0, where L0 is the wavelength in deep water: L0 = g/(2π) T2, with T the wave period and g the gravity of Earth. The blue line is the shoaling coefficient according to Green's law for waves in shallow water, i.e. when the water depth is less than 1/20 times the local wavelength L = T √(gh). |
| Date | |
| Source | Own work |
| Author | Kraaiennest |
| SVG development | |
| Background | See:
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 16:24, 24 July 2017 | | 853 × 489 (146 KB) | Kraaiennest | == {{int:filedesc}} == {{Information |description={{en|1=Shoaling coefficient ''K''<sub>S</sub> as a function of relative water depth ''h''/''L''<sub>0</sub>, describing the effect of wave shoaling on the [[w:wave height|wave height... |
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