
Now, in the case of a distributed system whose
initial state is described by functions u
0
= u
0
(x)
depending on the spatial variable x, the evolution
is usually governed by partial differential equations
(PDEs) and the corresponding phase space is some
infinite-dimensional function space (e.g., := L
2
()
or := L
1
() for some domain R
N
.) Such DSs
are usually called infinite dimensional.
The qualitative study of DSs of finite dimensi ons
goes back to the beginning of the twentieth century,
with the pioneering works of Poincare´ on the N-
body problem (one should also acknowledge the
contributions of Lyapunov on the stability and of
Birkhoff on the minimal sets and the ergodic
theorem). One of the most surprising and significant
facts discovered at the very beginning of the theory
is that even relatively simple equations can generate
very complicated chaotic beha viors. Moreover, these
types of systems are extremely sensitive to initial
conditions (the trajectories with close but different
initial data diverge exponentially). Thus, in spite of
the determinis tic nature of the system (we recall that
it is generated by a system of ODEs, for which we
usually have the unique solvability theorem), its
temporal evolution is unpredictable on timescales
larger than some critical time T
0
(which depends
obviously on the error of approximation and on the
rate of divergence of close trajectories) and can
show typical stochastic behaviors. To the best of our
knowledge, one of the first ODEs for which such
types of behaviors were established is the physical
pendulum parametrically perturbed by time-periodic
external forces,
y
00
ðtÞþsinðyðtÞÞð1 þ " sinð!tÞÞ ¼ 0 ½4
where ! and ">0 are physical parameters. We also
mention the more recent (and more relevant for our
topic) famous example of the Lorenz system which is
defined by the following system of ODEs in R
3
:
x
0
¼ ðy xÞ
y
0
¼xy þ rx y
z
0
¼ xy bz
8
>
<
>
:
½5
where , r, and b are some parameters. These
equations are obtained by truncation of the
Navier–Stokes equations and give an approximate
description of a horizontal fluid layer heated from
below. The warmer fluid formed at the bottom
tends to rise, creating convection currents. This is
similar to what happens in the Earth’s atmosphere.
For a sufficiently intense heating, the time evolution
has a sensitive dependence on the initial conditions,
thus repre senting a very irregular and chaotic
convection. This fact was used by Lorenz to justify
the so-called ‘‘butterfly effect,’’ a metaphor for the
imprecision of weather forecast.
The theory of DSs in finite dimensions had been
extensively developed during the twentieth century,
due to the efforts of many famo us mathematicians
(such as Anosov, Arnold, LaSalle, Sinai, Smale, etc.)
and, nowadays, much is known on the chaotic
behaviors in such systems, at least in low dimen-
sions. In particular, it is known that, very often, the
trajectories of a chaotic system are localized, up to a
transient process, in some subset of the phase space
having a very complicated fractal geometric struc-
ture (e.g., locally homeomorphic to the Cartesian
product of R
m
and some Cantor set) which, thus,
accumulates the nontrivial dynamics of the system
(the so-called strange attractor). The chaotic
dynamics on such sets are usually described by
symbolic dynamics generated by Bernoulli shifts on
the space of sequences. We also note that, nowa-
days, a mathematician has a large amount of
different concepts and methods for the extensive
study of concrete chaotic DSs in finite dimensions.
In particular, we mention here different types of
bifurcation theories (including the KAM theory and
the homoclinic bifurcation theory with related
Shilnikov chaos), the theory of hyperbolic sets,
stochastic description of deterministic processes,
Lyapunov exponents and entropy theory, dynamical
analysis of time series, etc.
We now turn to infinite-dimensional DSs gener-
ated by PDEs. A first important difficulty which
arises here is related to the fact that the analytic
structure of a PDE is essentially more complicated
than that of an ODE and, in particular, we do not
have in general the unique solvability theorem as for
ODEs, so that even finding the proper phase space
and the rigorous construction of the associated DS
can be a highly nontrivial problem. In order to
indicate the level of diffic ulties arising here, it
suffices to recall that, for the three-dimensional
Navier–Stokes system (which is one of the most
important equations of mathematical physics), the
required associated DS has not been constructed yet.
Nevertheless, there exists a large number of equa-
tions for which the proble m of the global existence
and uniqueness of a solution has been solved. Thus,
the question of extending the highly developed
finite-dimensional DS theory to infinite dimensions
arises naturally.
One of the first and most significant results in that
direction was the development of the theory of
integrable Hamiltonian systems in infinite dimen-
sions and the explicit resolution (by inverse-scattering
methods) of several important conservative equations
102 Dissipative Dynamical Systems of Infinite Dimension