Sediment Transport in Coastal Waters

The interface of 440,000 km long coastline in the world is subject to global change, with an increasing human pressure (land use, buildings, sand mining, dredging) and increasing population. Improving our knowledge on involved mechanisms and sediment transport processes, monitoring the evolution of...

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Bibliographic Details
Format: eBook
Language:English
Published: MDPI - Multidisciplinary Digital Publishing Institute 2019
Subjects:
mud
Online Access:Open Access: DOAB: description of the publication
Open Access: DOAB, download the publication
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520 |a The interface of 440,000 km long coastline in the world is subject to global change, with an increasing human pressure (land use, buildings, sand mining, dredging) and increasing population. Improving our knowledge on involved mechanisms and sediment transport processes, monitoring the evolution of sedimentary stocks and anticipating changes in littoral and coastal zones is essential for this purpose. The special issue of Water on “Sediment transport in coastal waters” gathers thirteen papers which introduce the current revolution in the scientific research related to coastal and littoral hydrosedimentary dynamics, and reflect the diversity of concerns on which research in coastal sediment transport is based, and current trends — topics and preferred methods — to address them. 
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653 |a analysis of variance (ANOVA) 
653 |a bathymetry 
653 |a bed shear stress 
653 |a bedload 
653 |a Bight of Benin 
653 |a biomass 
653 |a climate change 
653 |a Cluster analysis 
653 |a coastal erosion 
653 |a coastal hydraulics 
653 |a coastal management 
653 |a cohesive sediments 
653 |a coral reef 
653 |a delta vulnerability 
653 |a dry season 
653 |a East Coast Low 
653 |a ERA hindcast waves 
653 |a erosion 
653 |a flocculation 
653 |a fresh water runoff 
653 |a geochemical map 
653 |a geochemistry 
653 |a hydrodynamics 
653 |a lagoon 
653 |a Langue de Barbarie spit 
653 |a longshore sediment transport 
653 |a Mahalanobis' generalized distances 
653 |a mathematical model 
653 |a Mekong 
653 |a MODerate Resolution Imaging Spectroradiometer (MODIS) 
653 |a monsoon 
653 |a morphodynamics 
653 |a mud 
653 |a nearshore processes 
653 |a New Caledonia 
653 |a Ni mining 
653 |a non cohesive sediments 
653 |a non-cohesive to cohesive transition 
653 |a North Africa 
653 |a numerical modelling 
653 |a oceanic water intrusion 
653 |a oligotrophic lagoon 
653 |a particle transfer process 
653 |a post-storm recovery 
653 |a recovery 
653 |a reflectance 
653 |a remote sensing reflectance 
653 |a remote-sensing 
653 |a resilience 
653 |a river plume 
653 |a river-mouth migration 
653 |a sand 
653 |a sand-mud mixture erosion 
653 |a seabed colour 
653 |a seagrass beds 
653 |a seasonal cycle 
653 |a sediment 
653 |a sediment transport 
653 |a sediment transport modelling 
653 |a sediment trap 
653 |a sedimentation 
653 |a Senegal River delta 
653 |a Seto Inland Sea 
653 |a shoreline 
653 |a soil erosion 
653 |a South China Sea 
653 |a Southeast Australia 
653 |a spit breaching 
653 |a storminess 
653 |a storms 
653 |a Support Vector Regression (SVR) 
653 |a suspended particulate matter 
653 |a suspended sediment 
653 |a SWAT 
653 |a Tafna catchment 
653 |a tidal current 
653 |a trend 
653 |a turbidity 
653 |a typhoons 
653 |a Vietnam 
653 |a water scarcity 
653 |a waves forcing 
653 |a winter monsoon 
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