Equation (1) is Laplace equation for the velocity potential. It expresses incompressibility, , together with . Equation (2) is the linearized dynamic free-surface condition: the unsteady Bernoulli equation and constant atmospheric pressure balance the potential acceleration against the gravitational restoring term . Equation (3), with the printed understood as , is the kinematic free-surface condition: the surface moves with the vertical fluid velocity. Equations (4) and (5) are no-penetration boundary conditions at the rigid bottom and cylindrical sidewall, respectively.
For an axisymmetric separated amplitude , Laplace equation in cylindrical coordinates becomes
The radial equation is
Its solution regular at the axis is the Bessel function . The vertical equation is , and the bottom condition selects
up to an irrelevant constant multiplier. Finally, the sidewall condition gives
Therefore the allowed positive wavenumbers are
and
At , the two free-surface conditions for a normal mode give
Eliminating yields
For the vertical factor found in part (b),
Thus the gravity-wave dispersion relation is
where

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