Journal of Geophysical Research Atmospheres · 1981 · 358 citations · 23 references
Natural SciencesOcean EngineeringOceanographyOcean ModelingOcean WavesPhysical OceanographyOcean ForecastingSurface Wave DynamicsWave ForecastingWave RefractionWave ShoalingWave SpectraBottom Friction EffectsDirectional Wave SpectrumShallow Water WavesShallow-water HydrodynamicsSignificant Wave HeightWind Wave ForecastingWind Wave GenerationWind Wave Spectra
The study presents a wind wave forecasting model based on the ray technique, tailored for shallow water regions. The model incorporates wave generation, refraction, shoaling, and parametrized nonlinear dissipation, delivering a directional spectrum from which the one‑dimensional spectrum and significant wave height are derived. Hindcasts of storms in the Northern Adriatic and Tyrrhenian Seas showed 10–20 % rms error in significant wave height, but highlighted a major issue in accurately evaluating the wind field.
A wind wave forecasting model is described, based upon the ray technique, which is specifically designed for shallow water areas. The model explicitly includes wave generation, refraction, and shoaling, while nonlinear dissipative processes (breaking and bottom friction) are introduced through a suitable parametrization. The forecast is provided at a specified time and target position, in terms of a directional spectrum, from which the one‐dimensional spectrum and the significant wave height are derived. The model has been used to hindcast storms both in shallow water (Northern Adriatic Sea) and in deep water conditions (Tyrrhenian Sea). The results have been compared with local measurements, and the rms error for the significant wave height is between 10 and 20%. A major problem has been found in the correct evaluation of the wind field.
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On the generation of surface waves by shear flows
John W. Miles · Journal of Fluid Mechanics · 1957 · 1.5K citations
On the generation of waves by turbulent wind
O. M. Phillips · Journal of Fluid Mechanics · 1957 · 841 citations