Examples, Basic Problems, Peculiar Features of Solutions 11
hydrodynamic equations of perfect incompressible liquid, including quadratic nonlin-
earity, energy conservation, and regularity (phase volume invariance during system
motions). The general description of HTS is given in Sect. 8.3.3, page 200. Here, we
dwell only on the dynamic description of simplest systems.
The simplest system of this type (S
3
) is equivalent to the Euler equations in the
dynamics of solids; it describes the known problem on liquid motions in an ellipsoidal
cavity [24]. Any finite-dimensional approximation of hydrodynamic equations also
belongs to the class of HTS if it possesses the above features.
To model the cascade mechanism of energy transformation in a turbulent flow,
Obukhov [25] suggested a multistage HTS. Each stage of this system consists of
identical-scale triplets; at every next stage, the number of triplets is doubled and the
scale is decreased in geometrical progression with ratio Q & 1. As a result, this model
describes interactions between the motions of different scales.
The first stage consists of a singe triplet whose unstable mode v
01
is excited by an
external force f
0
(t) applied to the system (Fig. 1.4a). The stable modes of this triplet
v
1,1
and v
1,2
are the unstable modes of two triplets of the second stage; their stable
modes v
2,1
, v
2,2
, v
2,3
, and v
2,4
are, in turn, the unstable modes of four triplets of the
third stage; and so on (Fig. 1.4b).
It should be noted however that physical processes described in terms of macro-
scopic equations occur in actuality against the background of processes charac-
terized by shorter scales (noises). Among these processes are, for example, the
molecular noises (in the context of macroscopic hydrodynamics), microturbulence
(against the large-scale motions), and the effect of truncated (small-scale) terms in
the finite-dimensional approximation of hydrodynamic equations. The effect of these
small-scale noises should be analyzed in statistical terms. Such a consideration can be
performed in terms of macroscopic variables. With this goal, one must include exter-
nal random forces with certain statistical characteristics in the corresponding macro-
scopic equations. The models considered here require additionally the inclusion of
dissipative terms in the equations of motion to ensure energy outflow to smaller-scale
modes.
Accordingly, the simplest hydrodynamic models that allow simulating actual pro-
cesses are the HTS with random forces and linear friction.
An important problem which appeared, for example, in the theory of climate con-
sists in the determination of a possibility of significantly different circulation processes
f
0
(t)
v
1,1
(t)
v
1,0
(t)
v
2,1
(t)
v
2,2
(t) v
2,3
(t)
v
1,2
(t)
v
2,4
(t)
(a) (b)
f
0
(t)
v
1,1
(t)
v
1,0
(t)
v
1,2
(t)
Figure 1.4 Diagrams of (a) three- and (b) seven-mode HTS.