Surface elevation standard deviation scales linearly with subsurface velocity fluctuations, with wavenumber and frequency spectra both showing -2.5 power-law exponents explained by a linear passive-response model to turbulent pressure that predicts -7/3 scaling.
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Free-surface deformations induced by three-dimensional turbulence
Surface elevation standard deviation scales linearly with subsurface velocity fluctuations, with wavenumber and frequency spectra both showing -2.5 power-law exponents explained by a linear passive-response model to turbulent pressure that predicts -7/3 scaling.