Experiments are performed in a 13-m cylindrical tank co study the gene
ration of interfacial internal waves by barotropic sinusoidal waves pa
ssing over a slope. At each tidal cycle, there are two waves generated
, one propagating onshore and the other propagating offshore. The ampl
itude of the waves increases with increasing forcing and evolves as no
nlinear waves if the shelf width is smaller than the wavelength of the
baroclinic tide. Rotation does not modify the generating mechanism bu
t the amplitude of the generated waves decreases with increasing rotat
ion rate; also no internal waves are generated when the forcing period
is larger than the inertial period, and at high rotation rate, there
are only dispersive waves propagating from the shelf break region. The
experiments covered a large range of internal Froude number, Rossby n
umber and temporal Rossby number and compare well with in situ observa
tions. (C) 1998 Elsevier Science B.V. All rights reserved.