2016
DOI: 10.3390/jmse4030055
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Effects of Harbor Shape on the Induced Sedimentation; L-Type Basin

Abstract: Tsunamis in shallow water zones lead to sea water level rise and fall, strong currents, forces (drag, impact, uplift, etc.), morphological changes (erosion, deposition), dynamic water pressure, as well as resonant oscillations. As a result, ground materials under the tsunami motion move, and scour/erosion/deposition patterns can be observed in the region. Ports and harbors as enclosed basins are the main examples of coastal structures that usually encounter natural hazards with small or huge damaging scales. M… Show more

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Cited by 10 publications
(4 citation statements)
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“…Recently, many research attempts have been made with physical and numerical models to investigate sediment transport in harbor basins for the purpose of mitigating sedimentation issues [2,6,[16][17][18][19][20][21][22][23][24][25]. Physical modeling methodologies strive to incorporate diverse influences for assessing and determining harbors' sedimentation quantities.…”
Section: Introductionmentioning
confidence: 99%
“…Recently, many research attempts have been made with physical and numerical models to investigate sediment transport in harbor basins for the purpose of mitigating sedimentation issues [2,6,[16][17][18][19][20][21][22][23][24][25]. Physical modeling methodologies strive to incorporate diverse influences for assessing and determining harbors' sedimentation quantities.…”
Section: Introductionmentioning
confidence: 99%
“…Due to incoming tides and waves, sediment is generally formed in tidal estuary and wave dominated estuary on the landward side [20][21][22]. e flow direction and sediment entrainment in the coastal zone are mainly driven by the simultaneous action of swell and tide [23]. Sediment transport is mainly composed of bed sediment and suspended sediment [24][25][26].…”
Section: Introductionmentioning
confidence: 99%
“…In the framework of coastal sediment transport, 3D models for the simulation of the hydrodynamic fields [3][4][5][6] require considerable computational time, due to the long-time scale of the sea bottom variations. For this reason, in the context of morphodynamic simulations, the hydrodynamic equations [7][8][9][10][11][12][13] and the suspended sediment concentration equation are usually depth averaged [14].…”
Section: Introductionmentioning
confidence: 99%