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TECHNICAL PAPERS

A Two-Dimensional Numerical Wave Flume—Part 1: Nonlinear Wave Generation, Propagation, and Absorption

[+] Author and Article Information
S. F. Baudic

Deepwater Systems Division, ABB Lummus Global Inc., Houston, TX 77242-2833

A. N. Williams

Department of Civil and Environmental Engineering, University of Houston, Houston, TX 77204-4791e-mail: awilliams@uh.edu

A. Kareem

Department of Civil Engineering and Geological Science, University of Notre Dame, Notre Dame, IN 46556-0767

J. Offshore Mech. Arct. Eng 123(2), 70-75 (Jan 25, 2001) (6 pages) doi:10.1115/1.1365117 History: Received March 31, 2000; Revised January 25, 2001
Copyright © 2001 by ASME
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References

Figures

Grahic Jump Location
Comparison of the dimensionless free-surface elevation at x/ho=11 due to an input linear wave of kAo=0.157, for various smoothing intervals, calculated using Δt=T/90 and Nw=20
Grahic Jump Location
Comparison of the dimensionless free-surface elevation at t/T=44.86 due to an input linear wave of kAo=0.094, for various absorbing beach sizes, β(L/ho), and a constant α value, calculated using Nw=25,Δt=T/140 and smoothing every 10 time steps
Grahic Jump Location
Comparison of the dimensionless free-surface elevation at t/T=44.86 due to an input linear wave of kAo=0.094, for various absorption strengths, α, with a constant β value, calculated using Nw=25,Δt=T/140 and smoothing every 10 times steps
Grahic Jump Location
Comparison of the results of the present model 6 for the dimensionless free-surface elevation at x/ho=11 due to a Stokes fifth-order input wave of kAo=0.157, calculated using Nw=25,Δt=T/90 and smoothing every 17 time steps
Grahic Jump Location
Comparison of the dimensionless free-surface elevation at x/ho=55 due to an input linear wave of kAo=0.094, for various time steps, calculated using Nw=20 and smoothing every 10 time steps
Grahic Jump Location
Comparison of the dimensionless free-surface elevation at x/ho=11 due to an input linear wave of kAo=0.157, for various time steps, calculated using Nw=20 and smoothing every 10 time steps
Grahic Jump Location
Comparison of the dimensionless free-surface elevation at x/ho=55 due to a linear input wave of kAo=0.094, for various mesh sizes, calculated using Δt=T/140 and smoothing every 10 time steps
Grahic Jump Location
Comparison of the dimensionless free-surface elevation at x/ho=11 due to a linear input wave of kAo=0.157, for various mesh sizes, calculated using Δt=T/90 with smoothing every 10 time steps

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