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Costal Inlets Research Program
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> Fig. 10. Plot of a versus b values for hyperbolic-tangent shape and best-fit line.
RESULTS - cs99-moreno0011
Fig. 11. Hyperbolic-tangent fit to Drakes Bay, California.
cs99-moreno
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Fig.
10.
Plot
of
a
versus
b
values
for
hyperbolic-tangent
shape
and
best-fit
line.
EXAMPLES
OF
FITTING
WITH
HYPERBOLIC
TANGENT
Two
examples of
fittings
of
the
hyperbolic
tangent
shape
to
beaches
in
the
database
are
shown
here.
Values
of obtained
fitting
coefficients
are
listed
in
Appendix
A.
Drakes
Bay,
California,
USA
Drakes
Bay
is a
16.4-km-long
crenulate-shaped
beach
located
north
of
San
Francisco.
Its
shape
is determined by
diffraction
of Pacific-Ocean waves at a
headland
called
Point
Reyes.
The
area
is
tectonically
active
and
lies
on
the
San
Andreas
Fault.
Beach
sediments
consist
of
discontinuous
accumulations
of
well-to-moderately
sorted,
fine-
to
coarse-grained
sand
interspersed
with
pebbles
and
gravel.
Fig.
11 shows
the
nautical
chart
with
56
digitized
data
points
and
the
best-fit
curve.
The
visual
fit
is
very
good
in
the
beach
section
close
to
the
main
headland.
The
curve
deviates
from
the
shoreline
in
the
middle
section
because
of
irregularities
in
beach
plan
form
and
because
of
the
presence
of Drakes Estero (a
river
mouth).
Rosas
Bay,
Girona,
Spain
Rosas
Bay
is
located
on
the
Northeast
coast
of Spain. It is a
2.2-km-long
crenulate-
shaped
beach
with
1 to
1.5
headlands.
Shoreline
shape
is
controlled
in
great
part
by
jetties.
Beach
material
is
fine-
to medium-size
sand
with
median
grain
size
in
the
range
of
0.24
to
0.29
mm.
Fig.
12 shows an aerial
view
of
the
Bay
with
29
digitized
data
points
and
best-fit
hyperbolic
tangent.
Excellent
visual
agreement
is
seen.
Moreno
&
Kraus
12
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