A storm sends out deep-water swell in a narrow band of frequencies near

PHYSICS · Multi-part · Fermi University Physics · Oscillations, Waves & Acoustics · Waves in two and three dimensions, dispersion and wave packets · Waves in two and three dimensions, dispersion and wave packets

Modes, Packets and Media, Ch Water waves and de Broglie waves

Problem

A storm sends out deep-water swell in a narrow band of frequencies near ff, for which the group velocity is vg(f)=g/(4πf)v_{\rm g}(f) = g/(4\pi f). ((a)) Show that, following this band as it travels a distance DD from the storm, the length of ocean it occupies grows in direct proportion to DD, and that, because the wave energy carried by the band (per unit length of crest) is unchanged along the way, its wave height falls as D−1/2D^{-1/2}. ((b)) Spreading over the curved sea surface from a compact storm multiplies this by a further factor [Rsin⁡(D/R)]−1/2\left[R\sin(D/R)\right]^{-1/2}, where R=6371 kmR = 6371\,\mathrm{km} is the Earth's radius. This geometric factor is itself close to D−1/2D^{-1/2} when D≪RD \ll R, but it is a separate effect from the stretching of part (a). Two recording stations lie on the same great circle from a storm, at distances D1=6.0×103 kmD_1 = 6.0\times10^3\,\mathrm{km} and D2=9.0×103 kmD_2 = 9.0\times10^3\,\mathrm{km}. Find the ratio h1/h2h_1/h_2 of the heights of this frequency band at the two stations.

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