WVBetaPlanePVAdvection
Add beta-plane advection to the balanced QGPV tendency.
Declaration
WVBetaPlanePVAdvection < WVForcingOverview
On a beta plane, material conservation of total quasigeostrophic potential vorticity gives
\[\frac{D}{Dt}(q+\beta y)=0,\]so the right-hand-side tendency contributed by this forcing is
\[\left.\frac{\partial q}{\partial t}\right|_\beta=-\beta v_g.\]QG transforms evaluate this expression directly in physical QGPV
space. Wave-bearing transforms apply the equivalent spectral tendency
only to the geostrophic A0 coefficients; Ap, Am, inertial modes,
and mean-density-anomaly modes receive no direct beta tendency. This
retains beta advection for the balanced flow but is not a full
beta-plane treatment of internal-wave dynamics: wave frequencies and
structures continue to use the transform’s constant Coriolis
parameter.
wvt.addForcing(WVBetaPlanePVAdvection(wvt));
Topics
- Create the forcing
WVBetaPlanePVAdvectionCreate beta-plane QGPV advection for a transform.
Developer Topics
These items document internal implementation details and are not part of the primary public API.
- Forcing persistence
- Forcing internals
betaA0Spectral multiplier mappingA0to its beta-plane tendency.