The baroclinic tide incidence on the sea bottom's unevenness of the type of oceanic ridge is studied within the framework of the linear theory. The fluid is assumed to be stratified, and the effect of the Coriolis force is considered. The characteristics of the wave disturbances caused by incident baroclinic waves in the region of the ridge are determined depending on the bottom's relief parametes and the tide period. It is obtained, in particular, that there exist areas over the ridge, where the internal wave amplitudes are of well over the amplitude of an incident tide, and the area of "shade", where the inverse phenomenon occurs.

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