Modes of onshore sandbar migration at a single-barred and swell-dominated beach

2020 ◽  
Vol 426 ◽  
pp. 106222
Author(s):  
Jesús Adrián Vidal-Ruiz ◽  
Amaia Ruiz de Alegría-Arzaburu
Keyword(s):  
2017 ◽  
Vol 31 (5) ◽  
pp. 549-558
Author(s):  
Ming-xiao Xie ◽  
Chi Zhang ◽  
Zhi-wen Yang ◽  
Shan Li ◽  
Xin Li ◽  
...  

Author(s):  
Gonzalo Simarro ◽  
Alejandro Orfila ◽  
Phillip L.-F. Liu
Keyword(s):  

2015 ◽  
Vol 12 (05) ◽  
pp. 1550031 ◽  
Author(s):  
Khouane Meftah

In order to model nonlinear breaking waves with moving boundary and coastal sandbar migration; we presented a morphodynamic model, where hydrodynamic equations (free surface flows) and sediment transport equation are solved in a coupled manner. The originality lies in the development of an innovative approach, in which, we project the horizontal velocity onto a basis functions depending only on the variable z and we calculate analytically the vertical velocity and the nonhydrostatic pressure. The choice of basis depends on the problem under consideration. This model is numerically stable because there is no mesh in the vertical direction. This model is accurate because we can directly introduce functions that best fits the physical nature of the flow. Our model is validated through laboratory measurements carried out by Dingemans [1994, J. Comput. Phys. 231, 328–344], Cox and Kobayashi [2000, J. Geophys. Res. 105(c6), 223–236. and Dette et al. [2002, Coast. Eng. 47, 137–177].


2006 ◽  
Vol 53 (10) ◽  
pp. 817-824 ◽  
Author(s):  
Tian-Jian Hsu ◽  
Steve Elgar ◽  
R.T. Guza

2010 ◽  
Vol 26 ◽  
pp. 99-103 ◽  
Author(s):  
E. Ojeda ◽  
J. Guillén ◽  
F. Ribas

Abstract. The morphological changes caused by storm events in two Barcelona beaches were recorded using video monitoring techniques during the period 2001–2006. Changes in shoreline position and configuration and submerged bar position and shape were analyzed during the 25 major storm events that occurred during the study period. Beach responses to storms were grouped into three categories: shoreline advance or retreat (including rotation), sandbar migration and/or configuration change (linear or crescentic shape) and formation of megacusps. This work provides examples of the differential adaptation of both beaches to the same storm and of some unexpected morphological responses of both beaches. The response of the beach to storm events is not straightforward because wave conditions are not the only relevant parameter to be considered. In particular, in such embayed beaches it is crucial to take into account their specific morphodynamic configuration prior to the storm.


2015 ◽  
Vol 42 (8) ◽  
pp. 2869-2877 ◽  
Author(s):  
A. Fernández-Mora ◽  
D. Calvete ◽  
A. Falqués ◽  
H. E. de Swart

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