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  2. Seiche - Wikipedia

    en.wikipedia.org/wiki/Seiche

    The same storm system that caused the 1995 seiche on Lake Superior produced a similar effect in Lake Huron, in which the water level at Port Huron changed by 6 feet (1.8 m) over two hours. [12] On June 26, 1954, on Lake Michigan in Chicago, eight fishermen were swept away from piers at Montrose and North Avenue Beaches and drowned when a 10 ...

  3. Beach ridge - Wikipedia

    en.wikipedia.org/wiki/Beach_ridge

    A beach ridge is a wave-swept or wave-deposited ridge running parallel to a shoreline. It is commonly composed of sand as well as sediment worked from underlying beach material. The movement of sediment by wave action is called littoral transport. Movement of material parallel to the shoreline is called longshore transport.

  4. 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.

  5. 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.

  6. Coastal sediment transport - Wikipedia

    en.wikipedia.org/wiki/Coastal_sediment_transport

    Coastal sediment transport (a subset of sediment transport) is the interaction of coastal land forms to various complex interactions of physical processes. [1] [2] The primary agent in coastal sediment transport is wave activity (see Wind wave), followed by tides and storm surge (see Tide and Storm surge), and near shore currents (see Sea#Currents) . [1]

  7. Undertow (water waves) - Wikipedia

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

    An exact relation for the mass flux of a nonlinear periodic wave on an inviscid fluid layer was established by Levi-Civita in 1924. [9] In a frame of reference according to Stokes' first definition of wave celerity, the mass flux of the wave is related to the wave's kinetic energy density (integrated over depth and thereafter averaged over wavelength) and phase speed through:

  8. List of national lakeshores and seashores of the United States

    en.wikipedia.org/wiki/List_of_national...

    Twenty-one islands and shoreline on the northern tip of Wisconsin on Lake Superior offer a variety of recreation opportunities, including scuba diving at four shipwrecks. It is known for its sandstone sea caves, a few old growth remnant forests, natural animal habitats, and eight lighthouses, the most at any NPS site. [27]

  9. Ice shove - Wikipedia

    en.wikipedia.org/wiki/Ice_shove

    Water then exists between the ice sheet and the shoreline, facilitating the movement of ice sheets when wind acts on them. An open channel of water allows for reduced resistive forces on the ice sheet, increasing the likelihood that an ice shove event can occur. [1] The direction of the wind ultimately directs the motion of the ice shove.

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