Environmental Engineering Reference
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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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