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  2. Shallow water drilling - Wikipedia

    en.wikipedia.org/wiki/Shallow_water_drilling

    Shallow water drilling is the process of oil and gas exploration and production in less than 150 meters (500 feet) of water. [1] Shallow water drilling differs from deepwater drilling in several key aspects. Shallow water rigs have legs that reach the bottom of the sea floor and have blowout preventers (BOPs) above the surface of the water that ...

  3. Cnoidal wave - Wikipedia

    en.wikipedia.org/wiki/Cnoidal_wave

    Cnoidal wave descriptions, through a renormalisation, are also well suited to waves on deep water, even infinite water depth; as found by Clamond. [13] [14] A description of the interactions of cnoidal waves in shallow water, as found in real seas, has been provided by Osborne in 1994. [15]

  4. Dispersion (water waves) - Wikipedia

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

    In shallow water, the group velocity is equal to the shallow-water phase velocity. This is because shallow water waves are not dispersive. In deep water, the group velocity is equal to half the phase velocity: {{math|c g = ⁠ 1 / 2 ⁠ c p. [7] The group velocity also turns out to be the energy transport velocity.

  5. Waves and shallow water - Wikipedia

    en.wikipedia.org/wiki/Waves_and_shallow_water

    When waves travel into areas of shallow water, they begin to be affected by the ocean bottom. [1] The free orbital motion of the water is disrupted, and water particles in orbital motion no longer return to their original position. As the water becomes shallower, the swell becomes higher and steeper, ultimately assuming the familiar sharp ...

  6. Airy wave theory - Wikipedia

    en.wikipedia.org/wiki/Airy_wave_theory

    Boussinesq approximation (water waves) – nonlinear theory for waves in shallow water. Capillary wave – surface waves under the action of surface tension; Cnoidal wave – nonlinear periodic waves in shallow water, solutions of the Korteweg–de Vries equation; Mild-slope equation – refraction and diffraction of surface waves over varying ...

  7. Ursell number - Wikipedia

    en.wikipedia.org/wiki/Ursell_number

    h : the mean water depth, and; λ : the wavelength, which has to be large compared to the depth, λ ≫ h. So the Ursell parameter U is the relative wave height H / h times the relative wavelength λ / h squared. For long waves (λ ≫ h) with small Ursell number, U ≪ 32 π 2 / 3 ≈ 100, [3] linear wave theory is applicable.

  8. Korteweg–De Vries equation - Wikipedia

    en.wikipedia.org/wiki/Korteweg–De_Vries_equation

    For modelling shallow water waves, is the height displacement of the water surface from its equilibrium height. The constant 6 {\displaystyle 6} in front of the last term is conventional but of no great significance: multiplying t {\displaystyle t} , x {\displaystyle x} , and ϕ {\displaystyle \phi } by constants can be used to make the ...

  9. Marine geology - Wikipedia

    en.wikipedia.org/wiki/Marine_geology

    The two major resources mined at sea include oil and minerals. Over the last 30 years, deep-sea mining has generated between $9 -$11 billion USD in the United States of America. [43] [44] Although this sector seems profitable, it is a high risk, high reward industry with many harmful environmental impacts. [45]