Three dimensional parabolic equation modeling of an internal wave event during Shallow Water 2006.

2010 ◽  
Vol 127 (3) ◽  
pp. 1786-1786
Author(s):  
Georges A. Dossot ◽  
James H. Miller ◽  
Gopu R. Potty ◽  
James F. Lynch ◽  
Ying‐Tsong Lin ◽  
...  
2011 ◽  
Vol 129 (4) ◽  
pp. 2457-2457
Author(s):  
Georges A. Dossot ◽  
James H. Miller ◽  
Gopu R. Potty ◽  
Kevin B. Smith ◽  
Mohsen Badiey ◽  
...  

2019 ◽  
Vol 146 (3) ◽  
pp. 1875-1887 ◽  
Author(s):  
Georges A. Dossot ◽  
Kevin B. Smith ◽  
Mohsen Badiey ◽  
James H. Miller ◽  
Gopu R. Potty

2011 ◽  
Vol 19 (03) ◽  
pp. 221-239 ◽  
Author(s):  
MELANIE E. AUSTIN ◽  
N. ROSS CHAPMAN

A full three-dimensional parabolic equation model (MONM3D) has been developed that incorporates techniques that reduce the required number of model grid points and reduces computation time. The concept of tessellation is implemented in MONM3D, which allows the number of radial paths in the model grid to vary with range from the source, reducing the number of computational points in the horizontal plane. This design establishes a grid layout that is both numerically and computationally desirable. A benchmark test case is used to illustrate the accuracy and efficiency of the model.


2018 ◽  
Vol 144 (2) ◽  
pp. 06017026 ◽  
Author(s):  
Gaurav Savant ◽  
Corey J. Trahan ◽  
Charlie Berger ◽  
Jennifer T. McAlpin ◽  
Tate O. McAlpin

2018 ◽  
Vol 2018 ◽  
pp. 1-6
Author(s):  
Xiao-Wei Guan ◽  
Li-Xin Guo ◽  
Ya-Jiao Wang ◽  
Qing-Liang Li

The parabolic equation method based on digital elevation model (DEM) is applied on propagation predictions over irregular terrains. Starting from a parabolic approximation to the Helmholtz equation, a wide-angle parabolic equation is deduced under the assumption of forward propagation and the split-step Fourier transform algorithm is used to solve it. The application of DEM is extended to the Cartesian coordinate system and expected to provide a precise representation of a three-dimensional surface with high efficiency. In order to validate the accuracy, a perfectly conducting Gaussian terrain profile is simulated and the results are compared with the shift map. As a consequence, a good agreement is observed. Besides, another example is given to provide a theoretical basis and reference for DEM selection. The simulation results demonstrate that the prediction errors will be obvious only when the resolution of the DEM used is much larger than the range step in the PE method.


2020 ◽  
Vol 28 (03) ◽  
pp. 1950013
Author(s):  
Alexey Shmelev ◽  
Ying-Tsong Lin ◽  
James Lynch

Crossing internal wave trains are commonly observed in continental shelf shallow water. In this paper, we study the effects of crossing internal wave structures on three-dimensional acoustic ducts with both theoretical and numerical approaches. We show that, depending on the crossing angle, acoustic energy, which is trapped laterally between internal waves of one train, can be either scattered, cross-ducted or reflected by the internal waves in the crossing train. We describe the governing physics of these effects and illustrate them for selected internal wave scenarios using full-field numerical simulations.


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