2021
DOI: 10.1007/s10236-021-01476-7
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The 2nd international workshop on waves, storm surges and coastal hazards incorporating the 16th international workshop on wave hindcasting and forecasting

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Cited by 3 publications
(2 citation statements)
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“…By comparison, the other source terms for the development and evolution of windwaves, such as wind forcing input S in (f, q) and wave dissipation, S ds (f, q) largely operate locally in spectral space, adding or subtracting local energy at given frequencydirection locations, (f, q), WW3DG, 2016). There is a long history of studies related to these latter physical processes in simulations of ocean surface waves, like workshops reported by Swail et al (2021), or specific studies like that given by Hsiao et al (2020).…”
Section: Introductionmentioning
confidence: 99%
“…By comparison, the other source terms for the development and evolution of windwaves, such as wind forcing input S in (f, q) and wave dissipation, S ds (f, q) largely operate locally in spectral space, adding or subtracting local energy at given frequencydirection locations, (f, q), WW3DG, 2016). There is a long history of studies related to these latter physical processes in simulations of ocean surface waves, like workshops reported by Swail et al (2021), or specific studies like that given by Hsiao et al (2020).…”
Section: Introductionmentioning
confidence: 99%
“…By comparison, the other source terms for the development and evolution of windwaves, such as wind forcing input S in (f, q) and wave dissipation, S ds (f, q) largely operate locally in spectral space, adding or subtracting local energy at given frequencydirection locations, (f, q), (Komen et al, 1994;Holthuijsen, 2007;WW3DG, 2016). There is a long history of studies related to these latter physical processes in simulations of ocean surface waves, like workshops reported by Swail et al (2021), or specific studies like that given by Hsiao et al (2020).…”
Section: Introductionmentioning
confidence: 99%