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Nonlinear Long Wave in Shallow Water
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Contents Two Important Parameters For Waves In Shallow Water Nondimensional Variables Nondimensional Governing Equation & Boundary Conditions Perturbation Series of Potential Depth Average Horizontal Velocity & Wave Elevation Ariy's Approximation Boussenesq's Approximation Steady Kdv Equation Solitary Wave Cnoidal Wave
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Two Important Nonlinear Parameters for Waves in Shallow Water
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Non-dimensional Variables
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Nondimensional Governing Equation & Boundary Conditions
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Perturbation Series for Potential :
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Depth Average Horizontal Velocity & Wave Elevation
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Ariy's Theory For Very Long & Very Steep Waves
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Boussinesq's Approximation
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Steady KdV (Korteweg-de Vries) Equation
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Solitary Waves
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Figure 1. The sketch of a non-dimensional solitary wave train.
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Cnoidal Wave
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Computation Procedure : When water depth h, wave length L (or T) and wave height H are given, we may use a try and error (or iterative) method to determine m based on Equation (50) (or (53)). Once m is obtained, the characteristics of a Cnoidal wave train can be computed using Equations (47), (48), (49), (51) & (52).
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