I have been trying to create a "simpler models" scenario along the lines of the ocean-only "resting" example from MOM6-examples for MOM6 within CESM. I am running into issues with temperature and salinity instabilities forming very rapidly along one boundary (see image of surface layer T and S at 1 hr and 12 hrs into the run below).
The basic setup is as follows:
CESM version: cesm2_3_beta11
compset: 2000_DATM%SIMPLE_SLND_SICE_MOM6_SROF_SGLC_SWAV
ocn model domain: 0.5° x 0.5° x 75m depth
ocn grid: custom, with 100 grid points in each direction in the horizontal (dx~dy~500m), 30 layers
Wind speed is set to 0 over the entire domain (u = v = 0.0 in user_nl_datm) and the air temperature is set to match the initial ocean temperature (5° C).
I am able to run essentially the same scenario, on the same grid, in MOM6 outside of CESM without any issues. I have tried varying a number parameters (e.g., initial TS configuration, equation of state, using a zonally re-entrant model domain), but none of them seem to help. I was hoping someone might have an idea of why things are going wrong, or how best to go about trouble shooting this case.
Thanks!
Paul

The basic setup is as follows:
CESM version: cesm2_3_beta11
compset: 2000_DATM%SIMPLE_SLND_SICE_MOM6_SROF_SGLC_SWAV
ocn model domain: 0.5° x 0.5° x 75m depth
ocn grid: custom, with 100 grid points in each direction in the horizontal (dx~dy~500m), 30 layers
Wind speed is set to 0 over the entire domain (u = v = 0.0 in user_nl_datm) and the air temperature is set to match the initial ocean temperature (5° C).
I am able to run essentially the same scenario, on the same grid, in MOM6 outside of CESM without any issues. I have tried varying a number parameters (e.g., initial TS configuration, equation of state, using a zonally re-entrant model domain), but none of them seem to help. I was hoping someone might have an idea of why things are going wrong, or how best to go about trouble shooting this case.
Thanks!
Paul
