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Costal Inlets Research Program
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> Fig. 3. Circulation and momentum balances for idealized inlet II, otherwise same as Fig. 2.
Fig. 2. Circulation and momentum balances for idealized inlet I at maximum flood:
Fig. 4. Circulation and momentum balances for idealized inlet III, otherwise same as Fig. 2.
Hench_et_al_CSR_02
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J.L.
Hench
et
al.
/
Continental
Shelf
Research
22
(2002)
26152631
2620
Fig.
3.
Circulation
and
momentum
balances
for
idealized
inlet
II, otherwise
same
as
Fig.
2.
dominate;
we
will
examine
this
point
in
more
detail
is
similar
to
the
flow
field
since in
the
rotated
in
Section
4.
coordinate
system
the
streamwise
velocity
is
equivalent
to
the
flow
speed. In
the
normal
3.4.
Idealized
inlet
IV
direction
centrifugal
accelerations
balance
the
lateral
pressure
gradients
along
the
entire
inlet
Fig.
5
shows
the
momentum
balances
for
inlet
length,
but
are
confined
to
regions
adjacent
to
the
IV.
Here
the
dynamics
are
a
combination
of
headlands
(Figs.
4i
and
j).
Along
the
center
region
those
found
for
inlets
II
and
III.
Flood
flow
is
of
this
inlet,
it is
not
immediately
obvious
from
driven
by a
strong
favorable
(negative)
pressure
Fig.
4
whether
centrifugal
or
Coriolis
accelerations
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