Environmental Engineering Reference
In-Depth Information
p
d
f
p
d
f
0.6
0.6
a
b
2.5
φ
2.5
φ
2.5
2.5
Figure 5.48. Pdf's of the two fields shown in the first column of the Fig.
5.47
:
(a) refers to
s
gn
=
0
.
025 at
t
=
110 time units, and panel (b) corresponds to the same
time but
s
gn
=
2
.
5. Similar pdf's are obtained for
t
=
195 (corresponding to the third
column in Fig.
5.47
).
of patterns, in model (
5.102
) the coherent arrangement of the high and low values of
φ
(i.e., the dark and light gray pixels in Fig.
5.47
) corresponds to the emergence of
two modes in the distribution of
.
In the previous examples, the periodic forcing was always in the time domain.
However, spatiotemporal stochastic resonance can be also induced by a purely spatial
periodic forcing (
Sagues et al.
,
2007
). For example,
Vilar and Rubi
(
2000
) studied the
case of a Ginzburg-Landau model with an additive diffusive term, a spatially periodic
term, and a noise component. They demonstrated the occurrence of a remarkable
variety of patterns, both when the random driver varies in space and time and when it
varies only in space (so-called
quenched noise
).
φ
5.10 Spatiotemporal stochastic coherence
Similar to the case of stochastic resonance, there is also a spatiotemporal version of
stochastic coherence. In the third chapter we showed that a dynamical system able to
exhibit deterministic excursions characterized by a typical time scale can be excited by
a suitable noise and undergo regular fluctuations. We demonstrated that, when excited
from their steady state (or
rest state
), the deterministic dynamics undergo excursions
with a characteristic time scale. These excursions may have the same dynamical role
as the external periodic forcing in the phenomenon of stochastic resonance.
A classical example of spatiotemporal stochastic coherence can be obtained from
the FitzHugh-Nagumo model presented in Chapter 3 with the addition of diffusive
spatial coupling (
Naiman et al.
,
1999
). The 2D model is
3
1
∂φ
t
=
φ
1
−
φ
1
2
3
−
φ
2
+
D
∇
φ
1
,
(5.103)
∂
2
I
τ
φ
2
ξ
gn
(
r
,
t
)
∂φ
2
t
=
φ
1
+
a
(
r
)
+
,
(5.104)
∂
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