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  • ..., [[#Tidal flat|tidal flat]], [[#Salt marsh|salt marsh]], [[#Tidal channel|tidal channel]], etc.) by sedimentation. The tidal levels and water motion which would result from Earth's rotation and gravit
    79 KB (11,862 words) - 21:40, 1 April 2024
  • The hydrodynamic conditions or processes, that come about from [[Tidal wave|waves]] transforming over a coastal profile and generating wave set up *The sources and sinks of sediment, such as rivers, eroding coasts or tidal inlets
    29 KB (4,518 words) - 11:18, 6 July 2020
  • ...semi-protected areas. They are especially suited for areas where the tidal range is high, as they follow the water-level. Floating breakwaters are seldom us
    31 KB (4,715 words) - 23:55, 30 March 2024
  • ! style="border:2px solid lightblue;"| Ordinary tidal waves ! style="border:2px solid lightblue;"| Trans-tidal waves
    20 KB (2,992 words) - 16:09, 14 February 2024
  • ...fshore by a-large [[rip current]] or an ebb [[tide|tidal]] shoal where the tidal current is a major contributor to the sediment-transporting processes. ...ions of the distance offshore. The envelope tends to converge in the depth range of 5 to 6 m for this particular profile, seaward of which the profile eleva
    23 KB (3,596 words) - 12:03, 24 April 2024
  • ...ment transport related to [[Tidal asymmetry and tidal basin morphodynamics|tidal asymmetry]] and [[estuarine circulation]]. These processes are a major caus ...water mass. In estuaries, fluid mud layers can be entrained by near-bottom tidal currents over considerable distances without being dispersed over the whole
    15 KB (2,305 words) - 19:30, 12 January 2024
  • |definition= Bed forms induced by the interaction of the seabed with (mainly tidal) currents. ...mobilisation of sediment, sand dunes develop from sand grains in the size range 0.2-2.0mm.
    2 KB (268 words) - 13:49, 2 February 2023
  • ! width="10% style=" border:1px solid blue;"| Main periodicity range [year] ! width="15% style=" border:1px solid bleu;"| SLR range [m]
    41 KB (6,164 words) - 16:08, 21 January 2024
  • Coastal locations are also susceptible to a range of natural hazards such as [[Extreme storms|storm surges]], erosion and sea ...ater is too rough for swimming, a swimming pool, possibly in the form of a tidal pool, is a good solution.
    38 KB (5,697 words) - 22:31, 2 July 2022
  • {{Definition|title=Tidal flat ...lative tidal range RTR, defined as the ratio between the mean spring tidal range and the annual average significant wave height, is higher than 15<ref name=
    891 bytes (130 words) - 23:07, 22 June 2020
  • Analysis of coastal dynamics and evolution is difficult due to both the range of spatial and temporal scales over which coastal changes occur, and the co ...ucture and developing an understanding of how these elements interact on a range of both temporal and spatial scales. In this exercise it is the interaction
    20 KB (3,041 words) - 12:04, 7 September 2020
  • ...l and chemical environment (including salinity, wave exposure, strength of tidal streams, geology, biological zone, substratum, 'features' (e.g. crevices, o ...wave exposure, salinity and tidal currents. Such conditions vary within a range, which is characteristic of the [[habitat]]. This means that a [[habitat]]
    17 KB (2,420 words) - 13:14, 6 March 2022
  • ...ki (2005) <ref>Różyński, G. 2005. Long term shoreline response of a non-tidal, barred coast. Coastal Engineering 52: 79-91</ref>, who analyzed shoreline The 2nd wave had the wavelength in the range of 1,000-1,400 m, amplitudes of 10 m and the period of 8 years, see Fig. 3.
    25 KB (4,098 words) - 15:59, 20 November 2021
  • ...ing<ref>Van Coppenolle, R. and Temmerman, S. 2019. A global exploration of tidal wetland creation for nature-based flood risk mitigation in coastal cities. ...X., Yuan, J., Liu, W. and Li, Z. 2021. Global blue carbon accumulation in tidal wetlands increases with climate change. National Science Review 8: nwaa296<
    41 KB (6,267 words) - 13:40, 21 April 2024
  • ...-bottom layer that is maintained and kept in movement by oceanic currents, tidal currents or currents generated by internal waves<ref>Porz, L., Zhang, W., H ...ietrzak, J.D. 2020. The Formation of Turbidity Maximum Zones by Minor Axis Tidal Straining in Regions of Freshwater Influence. Journal Phys. Ocean. 50: 1265
    24 KB (3,842 words) - 18:14, 13 January 2024
  • ...aries. A qualitative discussion is given of the mutual interaction between tidal asymmetry generation and morphological development of these systems, which ==Tidal wave skewness==
    53 KB (8,417 words) - 12:56, 20 January 2024
  • ...: 670 </ref> and the discharge of reactive (available for uptake) P in the range 5-8.6 Tg P/yr <ref>Seitzinger, S.P., Mayorga, E., Bouwman, A.F., Kroeze, C. ...ll make a major contribution to the oceanic stock of nutrient N. Estimates range from 13 to 134 Tg N / yr <ref>Benavides, M., Bonnet, S., Berman-Frank, I. a
    26 KB (3,923 words) - 20:02, 4 August 2023
  • ...ion process, the intensity data are normalised over the lens’s intensity range and thus dimensionless. The dark, slightly curved patterns represent indivi ...n. The vertical reference level (z = 0) is generally set to match the mean tidal level or a commonly used (often national) ordinance level (like NAP in the
    7 KB (1,069 words) - 21:30, 10 August 2020
  • ...hour or more for hydrographic and topographic modes, respectively. For the tidal zone, this is crucial as usually only short tide windows are available for ==Range of systems==
    15 KB (2,393 words) - 22:55, 9 October 2023
  • ...observed dune erosion rates when using values of <math>C_s</math> in the range 10<sup>-3</sup> - 2.10<sup>-3</sup>. ...The erosion volumes become similar for long duration storms, assuming that tidal water level variations can be ignored. Another drawback is the restriction
    42 KB (6,534 words) - 12:05, 15 November 2023

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