Google+
Facebook
LinkedIn
Twitter
Digg
StumbleUpon
Home
Download PDF
Order CD-ROM
Order in Print
Home
>
Costal Inlets Research Program
>
> Fig. 3. Seasonal joint probability distributions of wave power vs. direction.
WAVE CLIMATE
Fig. 4. Seasonal joint probability distributions of wave power vs. direction for wave power greater than 8x10 W/m
Zarillo_etal-03
Page Navigation
1
2
3
4
5
6
7
8
9
Spring/Summer
(April
September)
25
20
15
10
0
5
2
4
4
x 10
0
6
140
120
100
8
W a ve
Pow
e
r(W
m
-
1
80
60
40
20
0
10
-20
Fall/Winter
(October
March)
25
20
15
10
0
5
2
4
4
x 10
0
6
140
120
100
8
W a ve
Pow
e
r(W
m
-1
80
60
40
20
0
10
-20
Fig.
3.
Seasonal
joint
probability
distributions
of
wave
power
vs.
direction.
Shorter-term
measurements
of
wave
data
in
the
vicinity
of
Sebastian
Inlet
are
consistent
with
the
interpretation
of
the
WIS
data
(Fig.
5).
The
winter
months
are
characterized
by
episodes
of
high
longshore
energy
flux,
whereas
during
the
summer
months,
higher
energy
events
are
rare,
and
longshore
sand
transport
is
likely
to be
small.
Based
on
analysis
of
wave
power
from
the
nearshore
Sebastian
Inlet
wave
gauge,
net
sand
transport
should
be to
the
south
in
the
winter
and
largely
driven
by
storms.
Transport
in
the
summer
months
is
weaker
and
more
balanced
between
north
and
south-
directed
components.
4
Zarillo
et
al.
Integrated Publishing, Inc. - A (SDVOSB) Service Disabled Veteran Owned Small Business