Magnetohydrodynamic discontinuities in a dissipative medium are consid
ered from the view point of the principle of evolutionarity. For a non
evolutionary discontinuity, the problem of time evolution of a small p
erturbation does not have a unique solution. This means that an infini
tesimal perturbation results in finite variation of the initial flow.
Such a discontinuity cannot exist as a stationary configuration and it
must disintegrate or transform to some other nonsteady flow. Using th
e kinematic properties of weakly damping high-frequency perturbations
of a dissipative medium, the sufficient conditions of nonevolutionarit
y of the dissipative discontinuities are obtained. These conditions ar
e shown to strengthen the known criterion of a discontinuous profile o
f inviscid shocks. It is suggested that time evolution of the nonevolu
tionary shock that contains the nonevolutionary internal discontinuity
is a superposition of two oscillation processes with different charac
teristic times corresponding to internal disintegration and disintegra
tion of the shock as a whole. (C) 1998 American Institute of Physics.
[S1070-664X(98)03506-X]