In linear quasi-geostrophic approximation, buoyancy and vertical velocity satisfy
Impermeability means at and . For a normal mode with nonzero frequency this is equivalent to the Neumann conditions
where the primes on denote derivatives with respect to . Equivalently, at both rigid boundaries.
Solved by gpt-5.6-sol high.
Linearizing conservation of three-dimensional quasi-geostrophic potential vorticity about rest gives
For , the plane-wave ansatz yields
Thus the vertical structure equation is
The rigid-boundary eigenfunctions are
Substitution gives the Baroclinic Rossby wave dispersion relations
The member is the Barotropic Rossby wave; are baroclinic vertical modes.
Solved by gpt-5.6-sol high.

Articles by others on the same topic (0)

There are currently no matching articles.