Environmental Engineering Reference
In-Depth Information
(a)
(b)
Figure 6.6. Examples of model-generated patterns (trees or shrubs in black; grass or
bare soil in white). (a) “Pseudo-labyrinthine” pattern (in an 800
×
800 lattice, with
the same parameters as in Fig. 6.5, D
=
0
.
3, uncorrelated random initial condition
with mean 0
350); (b) spot patterns [same
parameters as in Fig. 6.6 (a) but with mean initial condition
.
33, with simulation interrupted at time t
=
=
0
.
28]. Figure taken
from D'Odorico et al. ( 2007b ).
6.6 Random switching between two deterministic dynamics
6.6.1 Swift-Hohenberg process driven by dichotomous noise
A recurrent process of pattern formation in environmental fluid dynamics is associated
with Rayleigh-Benard convection ( Chandrasekhar , 1981 ). This phenomenon leads to
the emergence of organization in atmospheric convection, which is often evidenced
by well-defined cloud patterns (Fig. 6.7 ). The organization results from (symmetry-
breaking) thermoconvective instability typically observed when a fluid overlies a hot
surface ( Chandrasekhar , 1981 ). To study the effect of hydrodynamic fluctuations in
systems exhibiting Rayleigh-Benard convective cells, Swift and Hohenberg ( 1977 )
developed a stochastic model based on a biharmonic equation forced by additive white
noise. The deterministic counterpart of this model is frequently used to investigate
deterministic patterns emerging from symmetry-breaking instability of biharmonic
dynamics ( Cross and Hohenberg , 1993 ).
In Chapter 5 we introduced the Swift-Hohenberg model and discussed the ability
of additive and multiplicative Gaussian noise to generate patterns in Swift-Hohenberg
dynamics. Here we consider the case of a Swift-Hohenberg system driven by DMN
and the emergence of patterns induced by the random switching between two de-
terministic Swift-Hohenberg dynamics. The two dynamics have the same (Swift-
Hohenberg) spatial coupling term and two different local kinetics, f 1 , 2 (
φ
):
∂φ
( r
,
t )
2
k 0 ) 2
=
f 1 , 2 [
φ
( r
,
t )]
D (
+
φ
( r
,
t )
.
(6.11)
t
Buceta and Lindenberg ( 2002a ) considered the case with
A 1 , 2 φ
1
3
2
f 1 , 2 (
φ
)
=−
± φ
φ
(6.12)
Search WWH ::




Custom Search