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> Figure 2. Examples of solutions to dispersion equation with current present
Wave Action Flux Conservation Equation - TR-02-22-RPT_20022
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TR-02-22-RPT_2
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following
current
produces
an
increase
in
L
,
and
an
opposing
current
a
decrease
in
L
in comparison to
the
case
of no
current
(all
other
factors
held
constant).
0.75
Blocking
current
Opposing
current
E
0.25
A
No
current
D
C
B
Following
current
-0.25
-0.75
0.0
0.1
0.2
0.3
0.4
0.5
Relative
Water
Depth,
d/L
Figure
2.
Examples
of
solutions
to
dispersion
equation
with
current
present
(after
Jonsson
1990)
Wave
Orthogonals
and
Wave
Rays
In
the
presence
of a
current,
the
wave
energy
will
not
be
conserved
along
the
wave
orthogonals,
instead
the
energy
is
conserved
along
the
wave
rays
that
have
the
absolute
group
speed
C
ga
as a
tangent
at
all
locations.
The
wave
ray
direction
β
depends
of
the
relative wave
group
speed
and
the
current
magnitude
and
direction.
Thus,
C
ga
and
β
may
be
obtained
from
geometric
considerations
(Jonsson
1990;
also,
see
Figure 1) to
yield:
C
ga
=
(
C
gr
+
U
2
+ 2
C
gr
U
cos(
δ - α)
)
1/ 2
2
(8)
U
sin(δ - α)
β = α +
arctan
(9)
U
cos(
δ - α) +
C
gr
where
C
gr
is
the
relative
group
speed
and
α
the
direction
of
the
wave
orthogonal.
The
relative
group
speed
is
determined
from
linear wave theory
according
to:
1
2
kd
C
gr
=
C
r
1 +
(10)
2 sinh 2
kd
From
Equation 9, it
may
be
concluded
that
if
U
cos(
δ-α) = -
C
gr
,
the
denominator is zero,
and
the
wave
rays
form
a
90-deg
angle
with
respect
to
14
Chapter
3
Wave
Model
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