Forcing and climatology in the shallow water system #151
Labels
forcing 🏋️
Forcing of the momentum equations
parameterizations 🌧️
Parameterizations of unresolved physical processes
That's at the moment no straight forward to say. Most simulations I've run so far just used some initial conditions for vorticity. In that case you get a reasonably developed turbulence in 10-20 days even at higher resolution. However, that's decaying turbulence due to the lack of forcing obviously. Hence there's no actually interesting invariant measure the model converges to.
With #144 I've added some forcing for the shallow water equations, even including a seasonal cycle that you can switch on with
interface_relaxation = true
(default false) and control withinterface_relax_time
andinterface_relax_amplitude
.What's happening there is that one pulls the l=1,m=0 zonal mode of the interface displacement / SSH towards something that mimicks an equatorial heating. Other modes are not affected, so you literally just dump energy into that mode. With the
seasonal_cycle = true
(default true) that equatorial heating moves up and down with the seasons, similar to an ITCZ but actually all the way to the tropic of cancer back to the equator and down to the tropic of capricorn and back.My hope was to get an interesting and stable climate also in the shallow water system. But at the moment it still converges to a steady state (or one that closely follows the seasonal cycle). I probably haven't played around with it enough to get an actually nice setup that produces eddies at all resolutions with a proper energy cascade from some large scale forcing to some small scale dissipation
The text was updated successfully, but these errors were encountered: