Starting from Euler's equations of motion a nonlinear model for intern
al waves in fluids is developed by an appropriate scaling and a vertic
al integration over two layers of different but constant density. The
model allows the barotropic and the first baroclinic mode to be calcul
ated. In addition to the nonlinear advective terms dispersion and Cori
olis force due to the Earth's rotation are taken into account. The mod
el equations are solved numerically by an implicit finite difference s
cheme. In this paper we discuss the results for ideal basins: the effe
cts of nonlinear terms, dispersion and Coriolis force, the mechanism o
f wind forcing, the evolution of Kelvin waves and the corresponding tr
ansport of particles and, finally, wave propagation over variable topo
graphy. First applications to Lake Constance are shown, but a detailed
analysis is deferred to a second paper [Bauer er nl. (1994)].