Threshold accelerations necessary to excite surface waves parametrically in a vertically vibrated fluid layer are presented and compared with a linear stability analysis of the full hydrodynamic equations. The effects of viscosity and finite depth are treated rigorously. The case of two-frequency forcing is considered in detail because of its relevance to recently reported pattern forming phenomena. Absolute agreement between theory and experiment, generally to within 2%, is obtained for kinematic viscosities in the range 10--50 cS (1 S=1 cm²/s) and three frequency ratios. A slight discrepancy is noted for single-frequency forcing at high frequencies. {} 1996 The American Physical Society.
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Besson et al. (1996) studied this question.
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