A laboratory flume holds water of depth

PHYSICS · Multi-part · Fermi University Physics · Fluids & Continuum Physics · Waves, acoustics and compressible flow · Waves, acoustics and compressible flow

Signal Speeds in Fluids, Ch Long waves of finite height: bores, jumps and solitary waves

Problem

A laboratory flume holds water of depth h=0.40 mh = 0.40\,\mathrm{m}. A paddle stroke launches a single hump of amplitude A=0.10 mA = 0.10\,\mathrm{m} that runs along the flume without changing shape. ((a)) Estimate its speed VV and width LL using the solitary-wave relations V=gh(1+A/2h)V = \sqrt{gh}(1+A/2h) and L=4h3/3AL = \sqrt{4h^3/3A}. ((b)) Taking the wave's inverse width, k∼1/Lk \sim 1/L, as its effective wavenumber, estimate its Ursell number Ur=(A/h)/(kh)2\mathrm{Ur} = (A/h)/(kh)^2, show that this value does not depend on AA or hh, and say what that tells us about the balance between steepening and dispersion.

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