The properties of low-amplitude surface waves propagating in an ice ch
annel are investigated in the shallow-water approximation. The ice cov
er is modelled either by a rigid cap or by a thin elastic plate floati
ng on a liquid surface. It is shown that an ice channel is a waveguide
for surface waves. The dispersive properties of the natural oscillati
ons of the liquid in the channel are investigated. The resonance veloc
ities of the motion of the load on the channel surface, at which the a
mplitude of the forced oscillations of the liquid increases without li
mit in time, are determined. The decay instability of the natural osci
llations of high harmonics with respect to waves of the first mode is
demonstrated. The process is described by the standard equations for n
on-linear three-wave interaction. The investigations lead to the concl
usion that critical modes of motion of a boat are realizable in an ice
channel. (C) 1998 Elsevier Science Ltd. All rights reserved.