ag4680@nyu_edu
New Member
Hi,I am running the finite volume dynamical core with simple physics and analytical initial conditions (HS94 and Polvani-Kushner Stratosphere) using the F19 and F09 horizontal grid and 40 vertical levels. While the f19 grid generates the expected climatology with expected macroturbulence in the midlatitudes, I get an axisymmetric climatology for the f09 grid. In terms of configuration and parameters, all the parameters I am using in the user_nl_cam namelists are the same. Is there some perturbation parameters that should have been there but is not?From what I understand, in some dynamical cores(like the pseudospectral one), axisymmetric forcings (like a flat surface boundary) can generate axisymmetric circulations and some small perturbation is needed. So, I would suspect that might have been the culprit, however then I should have obtained a similar axisymmetric circulation for the f19 grid too.Besides, I noticed that the finite volume is the only dycore for which the temperature perturbation definitions use the analytic_ic_active() logical argument in dyn_comp.F90; the other dycores dont have this clause :if ((pertlim /= 0._r8) .and. (.not. analytic_ic_active()))Why is that? I am not sure if this is causing the problem, because again, it would have created a problem for the f19 resolution as well.
Please find the attached dynamical variables U and T and surface pressure PS from the generated climatology.Any help on this matter is deeply appreciated. Regards,Aman
Please find the attached dynamical variables U and T and surface pressure PS from the generated climatology.Any help on this matter is deeply appreciated. Regards,Aman