ONE-DIMENSIONAL (1-D) AND TWO-DIMENSIONAL (2-D) NUMERICAL MODELLING OF WAVE PROPAGATION PHENOMENON PASSING THROUGH VEGETATIONS

In this research, we focus on the development and evaluation of the mathematical model observing wave attenuation phenomenon by porous media. Wave attenuation is a term that refers to the reduction of wave energy as the effect of scattering and absorbing. First, the one-dimensional (1-D) and two-...

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Main Author: Vivianne
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/49459
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:49459
spelling id-itb.:494592020-09-16T13:09:21ZONE-DIMENSIONAL (1-D) AND TWO-DIMENSIONAL (2-D) NUMERICAL MODELLING OF WAVE PROPAGATION PHENOMENON PASSING THROUGH VEGETATIONS Vivianne Indonesia Final Project Shallow Water Equations, reduction, friction, diffusion, transmission coefficient, bathymetry profile INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/49459 In this research, we focus on the development and evaluation of the mathematical model observing wave attenuation phenomenon by porous media. Wave attenuation is a term that refers to the reduction of wave energy as the effect of scattering and absorbing. First, the one-dimensional (1-D) and two-dimensional (2-D) mathematical model that represents the wave propagation phenomenon passing through porous media is governed using Shallow Water Equations (SWEs). Secondly, some modifications towards the SWEs will be applied in order to capture the wave attenuation caused by porous media. The modifications are by adding friction and diffusion factor into the SWEs. Afterwards, the 1-D model will be solved analytically using the characteristics method and numerically using the finite volume method on a staggered grid scheme. Moreover, numerical observation of the wave propagation phenomenon will be conducted on a real bathymetry profile. The 2-D SWEs is discretized using the Arakawa Staggered C-Grid. In this 2-D model, wave shoaling phenomenon is taken into account. Wave shoaling is the change in water height as the effect of change in water depth. Next, the robustness of the 1-D numerical scheme is validated by its convergence to the analytical solution by means of the transmission coefficient. The transmission coefficient represents the wave amplitude reduction caused by the porous media. The results show that the friction coefficient, diffusion coefficient, and vegetation length have a significant effect upon the transmission coefficient. text
institution Institut Teknologi Bandung
building Institut Teknologi Bandung Library
continent Asia
country Indonesia
Indonesia
content_provider Institut Teknologi Bandung
collection Digital ITB
language Indonesia
description In this research, we focus on the development and evaluation of the mathematical model observing wave attenuation phenomenon by porous media. Wave attenuation is a term that refers to the reduction of wave energy as the effect of scattering and absorbing. First, the one-dimensional (1-D) and two-dimensional (2-D) mathematical model that represents the wave propagation phenomenon passing through porous media is governed using Shallow Water Equations (SWEs). Secondly, some modifications towards the SWEs will be applied in order to capture the wave attenuation caused by porous media. The modifications are by adding friction and diffusion factor into the SWEs. Afterwards, the 1-D model will be solved analytically using the characteristics method and numerically using the finite volume method on a staggered grid scheme. Moreover, numerical observation of the wave propagation phenomenon will be conducted on a real bathymetry profile. The 2-D SWEs is discretized using the Arakawa Staggered C-Grid. In this 2-D model, wave shoaling phenomenon is taken into account. Wave shoaling is the change in water height as the effect of change in water depth. Next, the robustness of the 1-D numerical scheme is validated by its convergence to the analytical solution by means of the transmission coefficient. The transmission coefficient represents the wave amplitude reduction caused by the porous media. The results show that the friction coefficient, diffusion coefficient, and vegetation length have a significant effect upon the transmission coefficient.
format Final Project
author Vivianne
spellingShingle Vivianne
ONE-DIMENSIONAL (1-D) AND TWO-DIMENSIONAL (2-D) NUMERICAL MODELLING OF WAVE PROPAGATION PHENOMENON PASSING THROUGH VEGETATIONS
author_facet Vivianne
author_sort Vivianne
title ONE-DIMENSIONAL (1-D) AND TWO-DIMENSIONAL (2-D) NUMERICAL MODELLING OF WAVE PROPAGATION PHENOMENON PASSING THROUGH VEGETATIONS
title_short ONE-DIMENSIONAL (1-D) AND TWO-DIMENSIONAL (2-D) NUMERICAL MODELLING OF WAVE PROPAGATION PHENOMENON PASSING THROUGH VEGETATIONS
title_full ONE-DIMENSIONAL (1-D) AND TWO-DIMENSIONAL (2-D) NUMERICAL MODELLING OF WAVE PROPAGATION PHENOMENON PASSING THROUGH VEGETATIONS
title_fullStr ONE-DIMENSIONAL (1-D) AND TWO-DIMENSIONAL (2-D) NUMERICAL MODELLING OF WAVE PROPAGATION PHENOMENON PASSING THROUGH VEGETATIONS
title_full_unstemmed ONE-DIMENSIONAL (1-D) AND TWO-DIMENSIONAL (2-D) NUMERICAL MODELLING OF WAVE PROPAGATION PHENOMENON PASSING THROUGH VEGETATIONS
title_sort one-dimensional (1-d) and two-dimensional (2-d) numerical modelling of wave propagation phenomenon passing through vegetations
url https://digilib.itb.ac.id/gdl/view/49459
_version_ 1822272044452020224