Modification of edge waves due to Coriolis force is examined in terms of two specific problems: dispersion of an initial deformation of the water surface; the forced wave due to a moving atmospheric pressure disturbance. In both cases the scale of the disturbance is an important factor, and the larger the scale the larger the effect of Coriolis force.
Kajiura, Kinjiro. 1958. "Effect of Coriolis force on edge waves (II) Specific examples of free and forced waves." Journal of Marine Research 16, (2). https://elischolar.library.yale.edu/journal_of_marine_research/889