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  2. Wind wave - Wikipedia

    en.wikipedia.org/wiki/Wind_wave

    A man standing next to large ocean waves at Porto Covo, Portugal Video of large waves from Hurricane Marie along the coast of Newport Beach, California. 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.

  3. Swell (ocean) - Wikipedia

    en.wikipedia.org/wiki/Swell_(ocean)

    Breaking swell waves at Hermosa Beach, California. A swell, also sometimes referred to as ground swell, in the context of an ocean, sea or lake, is a series of mechanical waves that propagate along the interface between water and air under the predominating influence of gravity, and thus are often referred to as surface gravity waves.

  4. Sea - Wikipedia

    en.wikipedia.org/wiki/Sea

    Deep seawater has a temperature between −2 °C (28 °F) and 5 °C (41 °F) in all parts of the globe. [30] Seawater with a typical salinity of 35 ‰ [31] has a freezing point of about −1.8 °C (28.8 °F). [32] When its temperature becomes low enough, ice crystals form on the surface.

  5. Ocean - Wikipedia

    en.wikipedia.org/wiki/Ocean

    The top of a wave is known as the crest, the lowest point between waves is the trough and the distance between the crests is the wavelength. The wave is pushed across the surface of the ocean by the wind, but this represents a transfer of energy and not horizontal movement of water.

  6. 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 ...

  7. Ocean current - Wikipedia

    en.wikipedia.org/wiki/Ocean_current

    An ocean current is a continuous, directed movement of seawater generated by a number of forces acting upon the water, including wind, the Coriolis effect, breaking waves, cabbeling, and temperature and salinity differences. [1]

  8. Ocean stratification - Wikipedia

    en.wikipedia.org/wiki/Ocean_stratification

    The dependence on pressure is not significant, since seawater is almost perfectly incompressible. [3] A change in the temperature of the water impacts on the distance between water parcels directly. [clarification needed] When the temperature of the water increases, the distance between water parcels will increase and hence the density will ...

  9. Marine energy - Wikipedia

    en.wikipedia.org/wiki/Marine_energy

    The interaction between wind and the surface of water creates waves, which are larger when there is a greater distance for them to build up. Wave energy potential is greatest between 30° and 60° latitude in both hemispheres on the west coast because of the global direction of wind.