Technical Papers
Apr 20, 2020

Overland Wave Propagation and Load Distribution among Arrays of Elevated Beachfront Structures

Publication: Journal of Waterway, Port, Coastal, and Ocean Engineering
Volume 146, Issue 4

Abstract

A series of laboratory experiments and high-fidelity numerical modeling were conducted to study the effects of the lowest floor elevation on the flow and loading patterns resulting from the overland propagation of a solitary wave among an array of idealized beachfront buildings. Although the uplift force is found to be nearly independent of the building position within the array, it significantly varies with the elevation of the lowest floor. The analyses show that the wave-induced uplift force reaches its peak as the lowest floor elevation is positioned at the still water level. The position of the building within the array and the elevation of the lowest floor are found to be the two most influential factors on the lateral force. The lateral and uplift forces varied with the lowest floor elevation by an inverse linear and a third-order polynomial relationship, respectively. The collective maximum force on the array estimated using the concept of momentum flux demonstrated a confidence level of more than 70%.

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Acknowledgments

This study was funded by The New York State Energy Research and Development Authority (NYSERDA) under Agreement No. 105162. The authors would like to thank the funding agency for the support.

Notation

The following symbols are used in this paper:
Ce
1.048;
Ck
0.094;
c
shallow water wave celerity;
g
gravitational acceleration;
H
offshore incident wave height;
h
still water depth on the berm;
ksgs
subgrid-scale kinetic energy;
L
block dimension;
Mf,i
influx momentum;
Mf,o
outflux momentum;
Mf,t,max
net momentum flux;
Mf,t,max
normalized net momentum flux;
P¯
pressure;
pd,i
dynamic pressures on the seaside of the array;
pd,o
dynamic pressures on the leeside of the array;
S
symmetric component of the velocity tensor;
T
normalized time instants;
t
time;
U
near-surface horizontal current velocity;
u
longitudinal velocity component;
ui
longitudinal velocity on the seaside of the array;
ui¯
filtered flow velocity;
uo
longitudinal velocity on the leeside of the array;
v
lateral velocity component;
w
vertical velocity component;
x
longitudinal axis in the Cartesian coordinate system;
y
lateral axis in the Cartesian coordinate system;
z
vertical axis in the Cartesian coordinate system;
zb
vertical distance of the block’s bottom from the berm;
z*
normalized depth;
Δ
filter length;
Δx
grid size in the x-direction;
Δy
grid size in the y-direction;
Δz
grid size in the z-direction;
η
free surface elevation;
η*
normalized free surface elevation;
ρ
fluid density;
υ
kinematic viscosity of the fluid;
τij
subgrid stress tensor;
υt
turbulence viscosity;
u
velocity tensor;
Ft,max
collective maximum loading on the array;
Ω
antisymmetric component of the velocity tensor;
ωy
vortex in the xz-coordinate plane; and
ωz
out-of-plane vortex.

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Go to Journal of Waterway, Port, Coastal, and Ocean Engineering
Journal of Waterway, Port, Coastal, and Ocean Engineering
Volume 146Issue 4July 2020

History

Received: May 1, 2019
Accepted: Jan 8, 2020
Published online: Apr 20, 2020
Published in print: Jul 1, 2020
Discussion open until: Sep 21, 2020

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Authors

Affiliations

Erdinc Sogut, S.M.ASCE [email protected]
Ph.D. Student, Dept. of Civil Engineering, Stony Brook Univ., Stony Brook, NY 11794-4424. Email: [email protected]
Deniz Velioglu Sogut, Ph.D. [email protected]
Visiting Scholar, Dept. of Civil Engineering, Stony Brook Univ., Stony Brook, NY 11794-4424. Email: [email protected]
Ali Farhadzadeh, Ph.D. [email protected]
P.E.
Assistant Professor, Dept. of Civil Engineering, Stony Brook Univ., Stony Brook, NY 11794-4424 (corresponding author). Email: [email protected]

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