Airborne Measurements of the Wavenumber Spectra of Ocean Surface Waves. Part I: Spectral Slope and Dimensionless Spectral Coefficient*

By P. Hwang, David W. Wang, E. Walsh, W. Krabill, R. Swift. 2000

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Performance of a Saturation-Based Dissipation-Rate Source Term in Modeling the Fetch-Limited Evolution of Wind Waves (2003, methodology): “…our results, predicted maxima of the directional wave energy spreading ulobe for mature seas from simulations made with all forms of Sds tend to match the unimodal behavior at the spectral peak, making a transition to a bimodal distribution above k/kp ø 3, that was observed by Hwang et al. (2000b).”
Statistical properties of mechanically generated surface gravity waves: a laboratory experiment in a three-dimensional wave basin (2009, methodology): “Concerning remote-sensing methods, Hwang et al. (2000) have used airborne scanning lidar measurements of wavenumber spectra of ocean surface waves to investigate their directional properties. Although, the resolution in angle increases with wavenumbers, it is 10◦ at the peak of the spectrum; unfortu”