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  • Growth (vertical and/or horizontal) of morphological structures ([[#Beach|beach]], [[#Bar|bar]], [[#Dune|dune]], [[#Sand bank|sand bank]], [[#Tidal flat|ti ...a dune coast the front [[#Dunes|dune]] is part of the active coastal zone. See: [[Active coastal zone]].
    79 KB (11,862 words) - 21:40, 1 April 2024
  • ...drodynamic factors (tidal cycles, wave climate) and sediment supply. These beach fluctuations correspond to alternating phases of erosion and accretion. [[D ...of coastal erosion. The presence of the structure has a series of effects (see [[Coastal Hydrodynamics And Transport Processes]] and [[Littoral drift and
    29 KB (4,651 words) - 22:27, 2 July 2022
  • ...rishments can be regarded as a 'natural' way of combating dune erosion and beach erosion as it artificially replaces a deficit in the sediment budget over a .... Generally practiced nourishment methods. Pipe discharge on the beach for beach nourishment, over the bow pumping (rainbowing) for nearshore nourishment an
    12 KB (1,875 words) - 15:32, 23 July 2023
  • ...ignates the boundary between land and sea for use in shoreline management, see the article [[Shoreline]]. ...ch). Disadvantage for sedimentary coasts: it does not provide insight into beach erosion or accretion.
    6 KB (879 words) - 17:04, 26 August 2022
  • {{Definition|title=Foreshore / Beach face ...f wave uprush at high tide (the latter is identical to the seaward [[beach berm]]). For practical reasons the administrative upper delineation of the [[for
    2 KB (233 words) - 16:11, 5 October 2021
  • ...al Functions. EOF methods have been used with success to analyze nearshore beach topography, as will be described below. However, the technique may not be a ...the past (Dette and Newe, 1997).<ref> Dette, H. H. and Newe, J. 1997.Depot beach fill in front of a cliff. Monitoring of a nourishment site on the Island of
    25 KB (4,098 words) - 15:59, 20 November 2021
  • ...idal coast of the southern North Sea. Marine Geology 276: 100–104</ref>, see also the article [[Dune development]]. The coastal dune belt in many cases ...can be taken away over several tens of meters, leaving a steep dune scarp, see Fig. 1. For the Dutch coast it has been estimated that under exceptional ci
    42 KB (6,534 words) - 12:05, 15 November 2023
  • {{Definition|title=Beach nourishment |definition=Artificial sand supply to the beach with sand imported from a source outside the [[active coastal zone]].}}
    9 KB (1,432 words) - 21:41, 21 November 2023
  • Definition|title=Berm |definition= There are two types of berm.
    367 bytes (50 words) - 11:56, 8 September 2020
  • Definition|title=Beach face ...from the low-water line to the limit of maximum wave uprush (or the beach berm) at high tide. <ref>USACE 2008. Coastal Engineering Manual. Part IV, Ch. 1.
    1 KB (208 words) - 16:31, 31 March 2021
  • ...t can be more dangerous for surfing safety. For more detailed information, see [[Stability of rubble mound breakwaters and shore revetments]]. For more detailed information, see [[Sand-filled geosystems in coastal engineering]].
    41 KB (6,487 words) - 22:37, 2 July 2022
  • ...ef name="Buscome 2006">Buscome D., Masselink G. (2006). Concepts in gravel beach dynamics. Earth science Reviews 79 33-52.</ref>. In the UK, about one third ..."Diserens">Diserens, A. P. & Coates, T. T. (1993). UK South Coast shingle beach study: storm response of shingle beaches. HR Wallingford Report SR 323.</r
    40 KB (6,109 words) - 17:19, 24 February 2023
  • ...s: Status and Challenges. Energies 11, 1250; doi:10.3390/en11051250</ref>, see also [[Wave energy converters]]. Six sites were selected (see Fig. 5) for a preliminary study of wave energy flux and capacity of integra
    20 KB (3,003 words) - 15:51, 25 February 2023
  • ...setup and longshore currents, due to radiation stresses in shallow water (see [[Shallow-water wave theory]]). ...e gravitational effect of sun and moon, are periodic and very predictable (see [[Ocean and shelf tides]]). Surges, on the other hand, are quasi-periodic a
    99 KB (15,083 words) - 13:37, 7 November 2021
  • where the coefficients <math>a, b, c</math> depend on (see Fig. 2): ...ath> (approximately equal to the significant wave height <math>H_s</math>, see [[Statistical description of wave parameters]])
    7 KB (1,059 words) - 17:19, 24 January 2024
  • See also: [[Definitions of coastal terms]]. * [[Wave transformation]] , see [[Shallow-water wave theory]]
    20 KB (2,422 words) - 12:26, 20 February 2024
  • [[Image:PrinosFig1.2a.jpg|thumb|300px|right|Fig. 1b. Damage to beach front homes on Dauphin Island, AL, due to storm surge from Hurricane Katrin ...g1.4.jpg|thumb|300px|right|Fig. 1d. Storm waves from Lake Erie wash over a beach at Point Pelee National Park, Ontario. (credit: Environment and Climate Cha
    25 KB (3,812 words) - 20:36, 18 September 2023
  • ...eing very visible, is the region of the littoral zone most associated with beach erosion and the impacts of climate change. The landward edge of the swash z ...factor in the design of coastal protection and also generates hazards for beach users, and is the dominant process leading to the erosion of coastal dunes.
    32 KB (4,942 words) - 12:58, 5 April 2021
  • ...d modification of littoral drift is a ubiquitous cause of coastal erosion (see [[Human causes of coastal erosion]]). Measuring littoral drift in field sit ...acterizing longshore transport potential and divergence of drift to inform beach loss trends. Coastal Engineering 189, 104473</ref>.
    26 KB (4,053 words) - 13:58, 30 April 2024
  • |definition= The shoreface profile, often called beach profile, is the cross-shore coastal depth profile of the shoreface. }} ...from wave climate. Coast. Eng. 4: 253–277</ref>), yielding the formula (see also [[Closure depth]])
    59 KB (9,016 words) - 11:16, 19 April 2024

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