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  2. Internal tide - Wikipedia

    en.wikipedia.org/wiki/Internal_tide

    The interfacial movement between two layers of ocean is large compared to surface movement because although as with surface waves, the restoring force for internal waves and tides is still gravity, its effect is reduced because the densities of the two layers are relatively similar compared to the large density difference at the air-sea interface.

  3. Waterlogging (agriculture) - Wikipedia

    en.wikipedia.org/wiki/Waterlogging_(agriculture)

    Antique Dutch windmills used to pump water into the embanked river to prevent waterlogging of the lowlands behind them. Waterlogging water is the saturation of soil with water. [1] Soil may be regarded as waterlogged when it is nearly saturated with water much of the time such that its air phase is restricted and anaerobic conditions prevail.

  4. Hydraulic jump - Wikipedia

    en.wikipedia.org/wiki/Hydraulic_jump

    A tidal bore is a hydraulic jump which occurs when the incoming tide forms a wave (or waves) of water that travel up a river or narrow bay against the direction of the current. [16] As is true for hydraulic jumps in general, bores take on various forms depending upon the difference in the waterlevel upstream and down, ranging from an undular ...

  5. Barrier island - Wikipedia

    en.wikipedia.org/wiki/Barrier_island

    Mixed-energy barrier islands are molded by both wave energy and tidal flux. The flow of a tidal prism moves sand. Sand accumulates at both the inshore and off shore sides of an inlet, forming a flood delta or shoal on the bay or lagoon side of the inlet (from sand carried in on a flood tide), and an ebb delta or shoal on the open water side ...

  6. Wave power - Wikipedia

    en.wikipedia.org/wiki/Wave_power

    It appears that this was the first oscillating water-column type of wave-energy device. [10] From 1855 to 1973 there were 340 patents filed in the UK alone. [8] Modern pursuit of wave energy was pioneered by Yoshio Masuda's 1940s experiments. [11] He tested various concepts, constructing hundreds of units used to power navigation lights.

  7. Dispersion (water waves) - Wikipedia

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

    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. This is the velocity with which the mean wave energy is transported horizontally in a narrow-band wave field. [8 ...

  8. Oscillating water column - Wikipedia

    en.wikipedia.org/wiki/Oscillating_water_column

    The PTO system is the second main component of an OWC device. It converts the pneumatic power into a desired energy source (i.e. sound or electricity). The PTO system design is very important to the efficiency of the oscillating water column. It must be able to convert airflow going both out of and into the collecting chamber into energy.

  9. Water cycle - Wikipedia

    en.wikipedia.org/wiki/Water_cycle

    In doing so, the water goes through different forms: liquid, solid and vapor. The ocean plays a key role in the water cycle as it is the source of 86% of global evaporation. [2] The water cycle involves the exchange of energy, which leads to temperature changes. When water evaporates, it takes up energy from its surroundings and cools the ...