Disp_bouss.svg


Summary

Description
English: Linear frequency dispersion characteristics of the Boussinesq (1872) equations, modelling surface gravity waves of fairly long wavelength (as compared to the water depth).

Linear phase speed squared c 2 /(gh) as a function of relative wave number kh .
A = Boussinesq (1872), equation (25),
B = Boussinesq (1872), equation (26),

C = full linear wave theory, see dispersion of water waves .
Date
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Author Kraaiennest
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12 January 2008