IMIS

Publications | Institutes | Persons | Datasets | Projects | Maps | Infrastructure
[ report an error in this record ]basket (0): add | show Print this page

Assessing common downdrift control point and asymmetric double-curvature planform behind multiple detached breakwaters: Simple empirical method
Lee, J.L.; Lim, C.; Pranzini, E.; Yu, M.J.; Chu, J.; Chen, C.; Hsu, J.R.C. (2023). Assessing common downdrift control point and asymmetric double-curvature planform behind multiple detached breakwaters: Simple empirical method. Coast. Eng. 185: 104361. https://dx.doi.org/10.1016/j.coastaleng.2023.104361
In: Coastal Engineering: An International Journal for Coastal, Harbour and Offshore Engineers. Elsevier: Amsterdam; Lausanne; New York; Oxford; Shannon; Tokyo. ISSN 0378-3839; e-ISSN 1872-7379, more
Peer reviewed article  

Available in  Authors 

Keyword
    Marine/Coastal
Author keywords
    Parabolic model; Basic wave angle; Mean wave energy flux method; Asymmetric beach planform; Multiple detached breakwaters

Authors  Top 
  • Lee, J.L.
  • Lim, C.
  • Pranzini, E.
  • Yu, M.J.
  • Chu, J.
  • Chen, C.
  • Hsu, J.R.C.

Abstract
    A system of segmented detached breakwaters (DBWs) with a gap between units or a harbor breakwater with a shore protection structure at downdrift may result in a salient or tombolo, the curved planform of which can be assessed by the parabolic model. Where two adjacent tips of the DBWs are not at equal distance in the cross-shore direction relative to the wave front, it becomes difficult to accurately locate the common downdrift control point (CDCP) for plotting the asymmetric planform in static equilibrium (SEP). In this study, a simple empirical method is proposed to determine the CDCP and the SEP, using the basic wave angle (& beta;0 = 65.75 degrees) derived by differentiating the cross-shore component in the parabolic bay shape equation, from which the apex of the isosceles triangle formed by the wave front line and the & beta;0 line from each wave diffraction point (tip) can be applied to locate the CDCP for plotting the SEP in a double-curvature planform. Following successful benchmark tests with the results calculated by the mean wave energy flux model, many more prototype examples are illustrated to reaffirm the suitability of the simple empirical method for the benefit of coastal scientist, engineer, geomorphologist and manager in the assessment or design of a SEP behind DBWs.

All data in the Integrated Marine Information System (IMIS) is subject to the VLIZ privacy policy Top | Authors