A three-dimensional hydrodynamic model for shallow waters using unstructured Cartesian grids

2010 ◽  
Vol 66 (7) ◽  
pp. 885-905 ◽  
Author(s):  
XinJian Chen
2013 ◽  
Vol 268 ◽  
pp. 93-102 ◽  
Author(s):  
Yongshan Wan ◽  
Chelsea Qiu ◽  
Peter Doering ◽  
Mayra Ashton ◽  
Detong Sun ◽  
...  

2016 ◽  
pp. 1-32
Author(s):  
Igor Stanislavovich Men'shov ◽  
Viacheslav Sergeevich Nikitin ◽  
Victor Victorovich Sheverdin

2009 ◽  
Vol 8 (4) ◽  
pp. 338-342 ◽  
Author(s):  
Zhu Gao ◽  
Xing Li ◽  
Hong-wu Tang ◽  
Zheng-hua Gu

2009 ◽  
Vol 23 (03) ◽  
pp. 277-280
Author(s):  
JIANMING LIU ◽  
NING ZHAO ◽  
OU HU

This paper depicts a ghost cell method to solve the three dimensional compressible time-dependent Euler equations using Cartesian grids for static or moving bodies. In this method, there is no need for special treatment corresponding to cut cells, which complicate other Cartesian mesh methods, and the method avoids the small cell problem. As an application, we present some numerical results for a special moving body using this method, which demonstrates the efficiency of the proposed method.


Author(s):  
Dominique Bonneau ◽  
Aurelian Fatu ◽  
Dominique Souchet

Author(s):  
Behnam Zamani ◽  
Manfred Koch ◽  
Ben R. Hodges

In this study, effects of basin morphology are shown to affect density current hydrodynamics of a large reservoir using a three-dimensional (3D) hydrodynamic model that is validated (but not calibrated) with in situ observational data. The AEM3D hydrodynamic model was applied for 5-month simulations during winter and spring flooding for the Maroon reservoir in southwest Iran, where available observations indicated that large-scale density currents had previously occurred. The model results were validated with near-bottom water temperature measurements that were previously collected at five locations in the reservoir. The Maroon reservoir consists of upper and lower basins that are connected by a deep and narrow canyon. Analyses of simulations show that the canyon strongly affects density current propagation and the resulting differing limnological characteristics of the two basins. The evolution of the Wedderburn Number, Lake Number, and Schmidt stability number are shown to be different in the two basins, and the difference is attributable to the morphological separation by the canyon. Investigation of the background potential energy (BPE) changes along the length of the canyon indicated that a density front passes through the upper section of the canyon but is smoothed into simple filling of the lower basin. The separable dynamics of the basins has implications for the complexity of models needed for representing both water quality and sedimentation.


2019 ◽  
Vol 34 (5) ◽  
pp. 1131-1143 ◽  
Author(s):  
Fei Dong ◽  
Chenxi Mi ◽  
Michael Hupfer ◽  
Karl‐Erich Lindenschmidt ◽  
Wenqi Peng ◽  
...  

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