Jean-François Filipot

TL;DR: In this article, the spectral dissipation of wind-generated waves is modeled as a function of the wave spectrum and wind speed and direction, in a way consistent with observations of wave breaking and swell dissipation properties.

TL;DR: In this article, an empirical equation based on observed tidal water level and offshore wave height was produced to estimate extreme water levels over the whole period of dune morphological change monitoring, and a good correlation between this empirical equation (1.01Hmoξo) and field runup measurements (Rmax) was obtained (R2 85%).

TL;DR: In this paper, the authors analyzed and adjusted the breaking statistics used in two wave dissipation parameterizations implemented in the spectral wave model WAVEWATCH III and now used operationaly at NOAA/NCEP.

TL;DR: In this paper, the authors used new data including hydrodynamic measurements in both deep and intertidal waters, and records of cliff-top storm deposits displacement and deposition across Banneg Island during the stormy winter 2013-2014.

TL;DR: In this article, a wave-breaking dissipation parameterization for phase-averaged spectral wave models is presented, which combines wave breaking basic physical quantities, namely, the breaking probability and the dissipation rate per unit area.