In linear quasi-geostrophic approximation, buoyancy and vertical velocity satisfyImpermeability means at and . For a normal mode with nonzero frequency this is equivalent to the Neumann conditionswhere the primes on denote derivatives with respect to . Equivalently, at both rigid boundaries.
Linearizing conservation of three-dimensional quasi-geostrophic potential vorticity about rest givesFor , the plane-wave ansatz yieldsThus the vertical structure equation isThe rigid-boundary eigenfunctions areSubstitution gives the Baroclinic Rossby wave dispersion relationsThe member is the Barotropic Rossby wave; are baroclinic vertical modes.
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