The propagation of magnetohydrodynamic (MHD) disturbances in a solar c
oronal arcade is investigated. The equations of magnetoacoustic fast a
nd slow waves are presented in a very general form: a pair of second-o
rder, two-dimensional partial differential equations in which the two
dependent variables are the components of the velocity perturbation pa
rallel and normal to the magnetic field. In deriving these equations,
a general two-dimensional equilibrium structure with no longitudinal m
agnetic field component has been assumed. Thus, the equations are vali
d for rather general configurations. Alfven waves are decoupled from t
he magnetoacoustic modes and give rise to an Alfven continuous spectru
m.The solutions to the wave equations have been obtained numerically,
and the perturbed restoring forces (plasma pressure gradient, magnetic
pressure gradient, and magnetic tension), responsible for the oscilla
tory modes, have also been computed. These forces give rise to the pro
pagation of MHD waves, and their interaction determines the physical p
roperties of the various modes. Therefore, the spatial structure of th
e forces and their interplay are basic in characterizing fast and slow
modes. Pure fast and pure slow waves do not exist in the present conf
iguration, although for the considered parameter values, all modes pos
sess either fast-mode or slow-mode properties. ''Slow'' modes in these
two-dimensional equilibria can propagate across the magnetic field on
ly with difficulty and so display a structure of bands, centred about
certain field lines, of alternate positive and negative parallel veloc
ity component. On the other hand, ''fast'' modes are isotropic in natu
re, and their spatial structure is not so intimately linked to the sha
pe of field lines. In addition, as a consequence of the distinct chara
cteristic propagation speeds of fast and slow modes, their frequencies
typically differ by an order of magnitude.