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  2. Wind fetch - Wikipedia

    en.wikipedia.org/wiki/Wind_fetch

    In oceanography wind fetch, also known as fetch length or simply fetch, is the length of water over which a given wind has blown without obstruction. [ 2 ] [ 3 ] Fetch is used in geography and meteorology and its effects are usually associated with sea state and when it reaches shore it is the main factor that creates storm surge which leads to ...

  3. Roughness length - Wikipedia

    en.wikipedia.org/wiki/Roughness_length

    A plot of a typical log wind profile under statically neutral conditions. The roughness length plays a part in determining the slope of the line. Roughness length ( z 0 {\displaystyle z_{0}} ) is a parameter of some vertical wind profile equations that model the horizontal mean wind speed near the ground.

  4. Wind wave model - Wikipedia

    en.wikipedia.org/wiki/Wind_wave_model

    In fluid dynamics, wind wave modeling describes the effort to depict the sea state and predict the evolution of the energy of wind waves using numerical techniques.These simulations consider atmospheric wind forcing, nonlinear wave interactions, and frictional dissipation, and they output statistics describing wave heights, periods, and propagation directions for regional seas or global oceans.

  5. Wind wave - Wikipedia

    en.wikipedia.org/wiki/Wind_wave

    In fluid dynamics, a wind wave, or wind-generated water wave, is a surface wave that occurs on the free surface of bodies of water as a result of the wind blowing over the water's surface. The contact distance in the direction of the wind is known as the fetch. Waves in the oceans can travel thousands of kilometers before reaching land.

  6. Wind setup - Wikipedia

    en.wikipedia.org/wiki/Wind_setup

    This equation assumes that the fetch is small and simplifies the wind setup process by making the wind setup linearly proportional to the square of the wind speed. In their 2023 analysis of Van Sickle Island, Algra et al. found this model effective for environments with limited fetch and shallow depth, where the more complex approaches used for ...

  7. Eddy covariance - Wikipedia

    en.wikipedia.org/wiki/Eddy_covariance

    The eddy covariance (also known as eddy correlation and eddy flux) is a key atmospheric measurement technique to measure and calculate vertical turbulent fluxes within atmospheric boundary layers. The method analyses high-frequency wind and scalar atmospheric data series, gas, energy, and momentum, [ 1 ] which yields values of fluxes of these ...

  8. Wave power - Wikipedia

    en.wikipedia.org/wiki/Wave_power

    Wave power is the capture of energy of wind waves to do useful work – for example, electricity generation, desalination, or pumping water. A machine that exploits wave power is a wave energy converter (WEC). Waves are generated primarily by wind passing over the sea's surface and also by tidal forces, temperature variations, and other factors.

  9. Airy wave theory - Wikipedia

    en.wikipedia.org/wiki/Airy_wave_theory

    Phase and group velocity divided by √ gh as a function of ⁠ h / λ ⁠. A: phase velocity, B: group velocity, C: phase and group velocity √ gh valid in shallow water. Drawn lines: based on dispersion relation valid in arbitrary depth. Dashed lines: based on dispersion relation valid in deep water.