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Costal Inlets Research Program
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Conclusions - CHL-TR-01-200035
References - CHL-TR-01-200037
CHL-TR-01-20
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that
of the adjacent
sea)
and
various
geomorpologic
conditions,
such
as an
inlet
with
a
long
tidally
dominated
channel or a
short
wave-dominated
inlet
channel.
e.
Equilibrium
area
channels
for
tide-only
conditions
retained
their
original
length
and
widened
and
deepened
upon
approaching
equilibrium
cross-
sectional
area.
f.
Equilibrium
area
channels
following
tide-plus-wave
conditions
migrated
bayward
as
they
approached
equilibrium
and
shortened
in
length.
g.
The
equilibrium
area
experimental
results
will
be
useful
in the design of
other
experiments
relating
to
ebb
and
flood
shoals
and
spit
migration
in
the
CIRP
Idealized
Inlet.
28
Chapter
5
Conclusions
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