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  2. Dispersion (water waves) - Wikipedia

    en.wikipedia.org/wiki/Dispersion_(water_waves)

    Using another normalization for the same frequency dispersion relation, the figure on the right shows that for a fixed wavelength λ the phase speed c p increases with increasing water depth. [1] Until, in deep water with water depth h larger than half the wavelength λ (so for h/λ > 0.5), the phase velocity c p is independent of the water ...

  3. Airy wave theory - Wikipedia

    en.wikipedia.org/wiki/Airy_wave_theory

    Water depth is classified into three regimes: [8] Visualization of deep and shallow water waves by relating wavelength to depth to bed. deep water – for a water depth larger than half the wavelength, h > ⁠ 1 / 2 ⁠ λ, the phase speed of the waves is hardly influenced by depth (this is the case for most wind waves on the sea and ocean ...

  4. Atmospheric tide - Wikipedia

    en.wikipedia.org/wiki/Atmospheric_tide

    Tidal waves can be either internal (travelling waves) with positive eigenvalues (or equivalent depth) which have finite vertical wavelengths and can transport wave energy upward, or external (evanescent waves) with negative eigenvalues and infinitely large vertical wavelengths meaning that their phases remain constant with altitude.

  5. Theory of tides - Wikipedia

    en.wikipedia.org/wiki/Theory_of_tides

    High and low tide in the Bay of Fundy. The theory of tides is the application of continuum mechanics to interpret and predict the tidal deformations of planetary and satellite bodies and their atmospheres and oceans (especially Earth's oceans) under the gravitational loading of another astronomical body or bodies (especially the Moon and Sun).

  6. Internal tide - Wikipedia

    en.wikipedia.org/wiki/Internal_tide

    The Hawaiian Ridge produces depth-integrated energy fluxes as large as 10 kW/m. The longest wavelength waves are the fastest and thus carry most of the energy flux. Near Hawaii, the typical wavelength of the longest internal tide is about 150 km while the next longest is about 75 km. These waves are called mode 1 and mode 2, respectively.

  7. Tide - Wikipedia

    en.wikipedia.org/wiki/Tide

    The two high waters on a given day are typically not the same height (the daily inequality); these are the higher high water and the lower high water in tide tables. Similarly, the two low waters each day are the higher low water and the lower low water. The daily inequality is not consistent and is generally small when the Moon is over the ...

  8. What caused the huge waves that battered California’s coast?

    www.aol.com/news/caused-huge-waves-battered...

    “Those wind-driven waves occur on top of the tides and any effect from the coastal Kelvin waves.” High surf sent waves all the way up the beach in Cayucos, flooding the playground and nearby ...

  9. Seiche - Wikipedia

    en.wikipedia.org/wiki/Seiche

    where T is the longest natural period, L and h are the length and average depth of the body of water, and g the acceleration of gravity. [8] Higher-order harmonics are also observed. The period of the second harmonic will be half the natural period, the period of the third harmonic will be a third of the natural period, and so forth.