In this paper, we discuss zonally periodic steady quasigeostrophic waves in
a beta-plane channel, by using variational methods. A class of steady quas
igeostrophic waves are determined by the potential vorticity field profile,
g(.), which is a function of the stream function. We show that zonally per
iodic steady quasigeostrophic waves exist when the bottom topography and th
e potential vorticity field are bounded. We also show that these waves are
unique if, in addition, the potential vorticity field profile is increasing
and passes through the origin. Finally, we demonstrate that the zonal peri
odic wave in the case with g(psi)= arctan(psi) is nonlinearly stable in the
sense of Liapunov, under a boundedness condition for the potential vortici
ty field, or equivalently, under suitable conditions on the bottom topograp
hy, beta parameter, and zonal period T. (C) 1999 American Institute of Phys
ics. [S1070-6631(99)00804-1].