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Managing Coastal Erosion (1990) / Chapter Skim
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Appendix C: Shore Response Modeling Methods
Pages 151-160

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From page 151...
... The presentation below is organized in terms of "Iongshore" and "cross-shore transport models, consistent with the general pattern of individual model development to represent shore response to one or the other of these transport components. [ONGSHOR1: TRANSPORT MODELS Longshore transport models include analytical models (applicable to limited situations of interest)
From page 152...
... This solution demonstrates that the longevity of a nourishment project varies directly as the square of the project length and inversely as the 2.5 power of the representative wave height. Numerical ModeLs A number of investigators have developed one-~me numerical models to represent beach planform evolution as a result of natural effects or human-~duced alterations (Le Mehaute and Soldate, 1978 and 1980~.
From page 154...
... This is an empirical method that models relationships for the average and maximum expected erosion caused by a storm based on storm tide rise time raised to the 0.8 power and peak storm tide raised to the 1.6 power. Balsillie's approach provides encouraging correlation with numerous field data.
From page 155...
... o c CL s n' a' m ~ S {' ~ O CD ._ 0 _ Z C ._ C~ _ ~ 0 O C c ._ a> o S S ,cn o z a \ cn ~D Ct ~ 0 I oo = 1 1 ~ l l 11 \1 1,, cn COO ~ , ~,,~: ~: 7 _ ~ ~ Z O C~ LU ~ O ()
From page 156...
... The eroded profile is at a 1:50 slope and extends landward from the dune toe defined as the slope transition between the seaward limit of the dune and the milder beach berm. For this case a portion of the eroded sand is considered to be transported landward; thus, there is no basis (or requirement)
From page 157...
... Remove dune above 1 on 50 slope through dune toe 157 \ \ lon40 Slope \ SWFL SWFL Movable I 1 on 12.5 Slope FIGURE C-3 Treatment of sand dune erosion in l00-year event for a coastal good insurance study. SOURCE: Hallermeier and Rhodes, 1988.
From page 158...
... His formulation is based on the concept of an equilibrium profile, defined as an average profile that maintains its form, apart from small fluctuations, at a particular water level. The Bruun rule provides a profile of equilibrium with the material removed during shoreline retreat transferred onto the adjacent shoreface, thus maintaining the original nearshore shallow-water profile relative to the increased water level.
From page 159...
... Technical Report CERC-87-15, U.S. Army Engineer Waterways Experiment Station, Coastal Engineering Research Center.
From page 160...
... 1983. Predictive Computational Modelling for Beach and Dune Erosion During Storm Surges.


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