FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4205656505> ?p ?o ?g. }

• W4205656505 endingPage "104645" @default.
• W4205656505 startingPage "104645" @default.
• W4205656505 abstract "Typhoon Mangkhut, in 2018, was one of the worst typhoons in recent history that has made landfall in the Pearl River Estuary (PRE) China. It swept along the coast of Guangdong Province, causing severe damage to many areas and affecting more than one million people. To study the hydrodynamics and sediment dynamics in different sub-regions of the PRE during the typhoon, we implemented a 3D wave-current-sediment coupled ocean model based on the Semi-implicit Cross-scale Hydroscience Integrated System Model (SCHISM). A series of numerical experiments were conducted to study the variation in suspended sediment concentration (SSC) under different external forcing mechanisms, including tides, waves, river discharges and strong winds. Moderate Resolution Imaging Spectroradiometer (MODIS) images, collected after the typhoon landed, were used to assess the simulation results. We found that in the area where the water depth was shallower than 20 m, the increased total suspended sediment concentration was dominated by the regional erosion of fine sediment which was caused by near-bottom wave orbital velocity and bottom shear stress, especially at the four western outlets and along the western coast of the PRE. For the deeper coastal zone, at depths between 20 and 30 m offshore of the western coast, the high total SSC resulted from the contribution of fine sediment transported from the upper and middle estuaries by southwestward advection. A small amount of sand eroded and migrated locally, owing to the corresponding increase in the bottom shear stress. The variation in SSC during the typhoon had a time lag compared with other dynamic conditions, resulting in a maximum 1 h delayed response after the typhoon made landfall. Based on the results of the sensitivity experiments under the same typhoon conditions, we found that, as a result of wave-enhanced bottom shear stress, the SSC values associated with wave-current interaction were significantly higher, by as much as 1.5 and 1.3 times those of simulations without the waves at the surface and near-bottom layers, respectively. This indicated that the sediment resuspension induced by waves was important during typhoon landfall. However, the strong wind-induced current was weakened owing to the joint effect of wave radiation stress and enhanced bottom stress; thus, considering wave effects, the magnitude of the resulting sediment transport rate was smaller than that without considering wave effects, especially in shallow waters. During the approach, landfall and retreat of Typhoon Mangkhut, Lingding Bay experienced two transitions from a slight state of sediment loss to a relatively high state of sediment gain, followed by an even greater state of sediment loss. During an M2 tidal cycle after Typhoon Mangkhut made landfall, the net seaward suspended load sediment transport in Lingding Bay reached 0.37 megatonnes. For the typhoon period covering three M2 tidal cycles, the overall state of suspended load sediment transport in Lingding Bay was sediment loss, with the magnitude of sediment loss on the west side being larger than that of sediment gain on the east side. The magnitude of the overall sediment loss in Lingding Bay would be enlarged unrealistically by approximately 73% if the wave effects were excluded. In each period, the extent of sediment transport between the two sides of the bay was strengthened by the wave-current interaction under typhoon conditions. We determined that the net effect of wave-current interaction and strong wind-induced currents under typhoon conditions was a key factor for erosion, which resulted in SSC-influenced areas being approximately 8.7 and 4.4 times as large as those under normal weather conditions for the surface and near-bottom layers, respectively. The turbidity maximum moved from the West Shoal of Lingding Bay under normal weather to the Modaomen Estuary, which was the most affected area during the typhoon when wave effects were considered. We also showed that the relative location of the typhoon path with respect to the estuary had a more significant effect on erosion than the intensity of the typhoon." @default.
• W4205656505 created "2022-01-25" @default.
• W4205656505 creator A5002468134 @default.
• W4205656505 creator A5034624355 @default.
• W4205656505 creator A5050154269 @default.
• W4205656505 creator A5077259298 @default.
• W4205656505 date "2022-01-01" @default.
• W4205656505 modified "2023-10-15" @default.
• W4205656505 title "Hydrodynamic and sediment transport modelling in the Pearl River Estuary and adjacent Chinese coastal zone during Typhoon Mangkhut" @default.
• W4205656505 cites W1966178316 @default.
• W4205656505 cites W1967163252 @default.
• W4205656505 cites W1968320838 @default.
• W4205656505 cites W1970489089 @default.
• W4205656505 cites W1984547519 @default.
• W4205656505 cites W2007111468 @default.
• W4205656505 cites W2016166722 @default.
• W4205656505 cites W2018623377 @default.
• W4205656505 cites W2039058988 @default.
• W4205656505 cites W2043425497 @default.
• W4205656505 cites W2045508335 @default.
• W4205656505 cites W2049904659 @default.
• W4205656505 cites W2051238063 @default.
• W4205656505 cites W2071787167 @default.
• W4205656505 cites W2073542150 @default.
• W4205656505 cites W2083778668 @default.
• W4205656505 cites W2085552165 @default.
• W4205656505 cites W2087880724 @default.
• W4205656505 cites W2104448233 @default.
• W4205656505 cites W2108664133 @default.
• W4205656505 cites W2110487068 @default.
• W4205656505 cites W2111286455 @default.
• W4205656505 cites W2125024740 @default.
• W4205656505 cites W2128120064 @default.
• W4205656505 cites W2139851742 @default.
• W4205656505 cites W2169981579 @default.
• W4205656505 cites W2289289499 @default.
• W4205656505 cites W2400222471 @default.
• W4205656505 cites W2504358527 @default.
• W4205656505 cites W2527699765 @default.
• W4205656505 cites W2952654392 @default.
• W4205656505 cites W2959257768 @default.
• W4205656505 cites W2971361373 @default.
• W4205656505 cites W2994976593 @default.
• W4205656505 cites W3146538044 @default.
• W4205656505 doi "https://doi.org/10.1016/j.csr.2022.104645" @default.
• W4205656505 hasPublicationYear "2022" @default.
• W4205656505 type Work @default.
• W4205656505 citedByCount "4" @default.
• W4205656505 countsByYear W42056565052023 @default.
• W4205656505 crossrefType "journal-article" @default.
• W4205656505 hasAuthorship W4205656505A5002468134 @default.
• W4205656505 hasAuthorship W4205656505A5034624355 @default.
• W4205656505 hasAuthorship W4205656505A5050154269 @default.
• W4205656505 hasAuthorship W4205656505A5077259298 @default.
• W4205656505 hasConcept C111368507 @default.
• W4205656505 hasConcept C114793014 @default.
• W4205656505 hasConcept C121332964 @default.
• W4205656505 hasConcept C126645576 @default.
• W4205656505 hasConcept C127313418 @default.
• W4205656505 hasConcept C162284963 @default.
• W4205656505 hasConcept C181654704 @default.
• W4205656505 hasConcept C187320778 @default.
• W4205656505 hasConcept C205649164 @default.
• W4205656505 hasConcept C2816523 @default.
• W4205656505 hasConcept C5072599 @default.
• W4205656505 hasConcept C58640448 @default.
• W4205656505 hasConcept C65589250 @default.
• W4205656505 hasConcept C76886044 @default.
• W4205656505 hasConcept C81660378 @default.
• W4205656505 hasConcept C88160329 @default.
• W4205656505 hasConcept C97355855 @default.
• W4205656505 hasConceptScore W4205656505C111368507 @default.
• W4205656505 hasConceptScore W4205656505C114793014 @default.
• W4205656505 hasConceptScore W4205656505C121332964 @default.
• W4205656505 hasConceptScore W4205656505C126645576 @default.
• W4205656505 hasConceptScore W4205656505C127313418 @default.
• W4205656505 hasConceptScore W4205656505C162284963 @default.
• W4205656505 hasConceptScore W4205656505C181654704 @default.
• W4205656505 hasConceptScore W4205656505C187320778 @default.
• W4205656505 hasConceptScore W4205656505C205649164 @default.
• W4205656505 hasConceptScore W4205656505C2816523 @default.
• W4205656505 hasConceptScore W4205656505C5072599 @default.
• W4205656505 hasConceptScore W4205656505C58640448 @default.
• W4205656505 hasConceptScore W4205656505C65589250 @default.
• W4205656505 hasConceptScore W4205656505C76886044 @default.
• W4205656505 hasConceptScore W4205656505C81660378 @default.
• W4205656505 hasConceptScore W4205656505C88160329 @default.
• W4205656505 hasConceptScore W4205656505C97355855 @default.
• W4205656505 hasLocation W42056565051 @default.
• W4205656505 hasOpenAccess W4205656505 @default.
• W4205656505 hasPrimaryLocation W42056565051 @default.
• W4205656505 hasRelatedWork W1930526758 @default.
• W4205656505 hasRelatedWork W1980896987 @default.
• W4205656505 hasRelatedWork W2381680246 @default.
• W4205656505 hasRelatedWork W2811299054 @default.
• W4205656505 hasRelatedWork W2991060596 @default.
• W4205656505 hasRelatedWork W333129317 @default.
• W4205656505 hasRelatedWork W4206980917 @default.

• next