diff --git a/.testing/tc4/MOM_input b/.testing/tc4/MOM_input index 456783af88..deb496315a 100644 --- a/.testing/tc4/MOM_input +++ b/.testing/tc4/MOM_input @@ -7,10 +7,15 @@ USE_REGRIDDING = True ! [Boolean] default = False ! If True, use the ALE algorithm (regridding/remapping). If False, use the ! layered isopycnal algorithm. -DT = 300.0 ! [s] +DT = 1200.0 ! [s] ! The (baroclinic) dynamics time step. The time-step that is actually used will ! be an integer fraction of the forcing time-step (DT_FORCING in ocean-only mode ! or the coupling timestep in coupled mode.) +DT_THERM = 3600.0 ! [s] default = 300.0 + ! The thermodynamic and tracer advection time step. Ideally DT_THERM should be + ! an integer multiple of DT and less than the forcing or coupling time-step, + ! unless THERMO_SPANS_COUPLING is true, in which case DT_THERM can be an integer + ! multiple of the coupling timestep. By default DT_THERM is set to DT. C_P = 3925.0 ! [J kg-1 K-1] default = 3991.86795711963 ! The heat capacity of sea water, approximated as a constant. This is only used ! if ENABLE_THERMODYNAMICS is true. The default value is from the TEOS-10 @@ -377,7 +382,7 @@ WIND_CONFIG = "zero" ! ! === module MOM_restart === ! === module MOM_main (MOM_driver) === -DAYMAX = 1.0 ! [days] +DAYMAX = 0.25 ! [days] ! The final time of the whole simulation, in units of TIMEUNIT seconds. This ! also sets the potential end time of the present run segment if the end time is ! not set via ocean_solo_nml in input.nml. diff --git a/.testing/tc4/build_data.py b/.testing/tc4/build_data.py index 50f45ce9f1..e060d05cb1 100644 --- a/.testing/tc4/build_data.py +++ b/.testing/tc4/build_data.py @@ -30,7 +30,7 @@ def t_fc(x, y, z, radius=5.0, tmag=1.0): ny, nx = x.shape -nz = 10 +nz = 3 z = (np.arange(nz) * zbot0) / nz temp = t_fc(x, y, z)