scholarly journals Tidal sand ridges on the shelf: A numerical study of their natural morphodynamic evolution and response to interventions

2020 ◽  
Vol 205 ◽  
pp. 104195
Author(s):  
A. Nnafie ◽  
T.B.J. Wolf ◽  
H.E. de Swart
2018 ◽  
Vol 19 (5) ◽  
pp. 1047-1071 ◽  
Author(s):  
Huib E. de Swart ◽  
Bing Yuan
Keyword(s):  

2002 ◽  
Vol 188 (3-4) ◽  
pp. 293-315 ◽  
Author(s):  
Serge Berné ◽  
Pierre Vagner ◽  
François Guichard ◽  
Gilles Lericolais ◽  
Zhenxia Liu ◽  
...  

2014 ◽  
Vol 33 (1) ◽  
pp. 11-18 ◽  
Author(s):  
Xiaohui CHEN ◽  
Xunhua ZHANG ◽  
Rihui LI ◽  
Xianhong LAN

2020 ◽  
Vol 70 (12) ◽  
pp. 1505-1513
Author(s):  
Tjebbe M. Hepkema ◽  
Huib E. de Swart ◽  
Abdel Nnafie ◽  
George P. Schramkowski ◽  
Henk M. Schuttelaars

AbstractThe role of the Coriolis effect in the initial formation of bottom patterns in a tidal channel is studied by means of a linear stability analysis. The key finding is that the mechanism generating oblique tidal sand ridges on the continental shelf is also present in confined tidal channels. As a result, the Coriolis effect causes the fastest growing pattern to be a combination of tidal bars and oblique tidal sand ridges. Similar as on the continental shelf, the Coriolis-induced torques cause anticyclonic residual circulations around the ridges, which lead to the accumulation of sand above the ridges. Furthermore, an asymptotic analysis indicates that the maximum growth rate of the bottom perturbation is slightly increased by the Coriolis effect, while its preferred wavelength is hardly influenced.


2017 ◽  
Vol 137 ◽  
pp. 72-83 ◽  
Author(s):  
Bing Yuan ◽  
Huib E. de Swart ◽  
Carles Panadès

2013 ◽  
Vol 295-298 ◽  
pp. 1968-1974
Author(s):  
Xiao Da Xu ◽  
Zhi Min Cao ◽  
Zhi Xun Zhang

In the Yellow Sea, two large terrains of tidal sand ridges developed, respectively, in the Subei Shoal and the West Korea Bay. Sediment supply, hydrodynamics and bedforms are critical factors to form them. In this paper, sediment composition, morphology of sand ridges, etc. are analyzed in terms of relevant factors and subsequently their formation mechanisms and evolution processes are careful compared.


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