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The average wave energy is defined as [math]\lt E\gt = g \rho \, m_0 \equiv g \rho \lt (\, \eta(t)-\lt \eta\gt )^2\gt [/math], where [math]g[/math] is the gravitational acceleration, [math]\rho[/math] the seawater density and where [math]\; \lt …\gt \; [/math] designates the average over a period much longer than the characteristic wave periods.
- Hydrodynamics
Pages in category "Hydrodynamics" The following 43 pages are...
- Infragravity Waves
Infragravity waves are ocean surface waves with a typical...
- Reviewed Articles
Pages in category "Reviewed articles" The following 138...
- Hydrodynamics
The major parameters to describe sea state are the different peak periods (Tp composed of Tp1, Tp2, Tpw), the different mean periods (Tm composed of Tm02, Tm-10), the significant wave heights (Hs composed of Hs1, Hs2, Hsw) and the different peak directions (dp composed of dp1, dp2, dp3).
5 Φεβ 2005 · The continuous 45-year length of the ERA-40 data set makes it especially suitable to study climate variability and to estimate extreme values of certain wave parameters, for example, the 100-year return wave height [Caires and Sterl, 2005b].
21 Δεκ 2022 · We find that about 30–40% of the global ocean experienced robust seasonal trends in mean and extreme wave height, period, and direction.
15 Οκτ 2009 · INTRODUCTION. For a complete description of wind-generated random waves, it is necessary to consider wave height and period as well as the direction of travel. In particular, serious consideration must be given to the combined effect of height, period and direction, if any correlation exists.
20 Απρ 2022 · Certain “characteristic” ocean wave heights (i.e., averages relating to various percentiles in a time series) are frequently employed in the planning of various coastal and maritime operations.
7 Νοε 2023 · The resulting ocean wave factor enhances the mean wave period values calculated using the model and other parameterization schemes. The experimental results demonstrate that our new parameterization scheme effectively improves the abnormal peak of the fitting data.
