Open minghangli-uni opened 9 months ago
Thanks for spotting these differences @minghangli-uni.
The short answer is we didn't test different choices of these parameters in ACCESS-OM2. front_length_const
=5e3 is the default in MOM5. Note that this value is actually a floor because we also use front_length_deform_radius
=true (also the default).
This is a lot larger than the values of mle_front_length
=1000 in MOM6-CICE6_1deg_jra55do_ryf or 500 in mom6-panan/
MOM_input - see this table. Perhaps some difference in the implementation of this scheme in MOM5 vs MOM6 could account for the difference (e.g. maybe there's a different definition of mixed layer depth?)
Both these values are in turn larger than expected from 500m / 250m for 1deg and 0.25deg in the GFDL OM4 paper.
Although MLE_MLD_DECAY_TIME
is just a tuning parameter for the heuristic filter applied to the MLD seen by the mixed-layer restratification scheme, MLE_MLD_DECAY_TIME
= 345600 s = 4 days is an order of magnitude shorter than the 30 days used in the GFDL OM4 paper, so we should use a larger value, e.g. our other MOM6 configs use 2592000.0s = 30 days - see this table.
Some experimentation may be worthwhile once the configuration is running. The GFDL OM4 paper provides examples of the impact of different parameter choices - as expected, increased mixed layer restratification shoals the mixed layer depth, which in turn impacts SST.
Note that we're currently using KPP (unlike the GFDL OM4 paper which uses EPBL) - this might also have an impact.
In MOM6 for the 1deg setup, the frontal-length scale
MLE_FRONT_LENGTH
of MLE is chosen to be 1000.0m and theMLE_MLD_DECAY_TIME
is 345600.0s. Is there any relevant reference for this parameter selection?In the same 1deg setup of OM2, the
MLE_FRONT_LENGTH
was previously 5000m.However, in paper The GFDL Global Ocean and Sea Ice Model OM4.0: Model Description and Simulation Features,
MLE_FRONT_LENGTH
was set to 500m / 250m for 1deg and 0.25deg configurations, whileMLE_MLD_DECAY_TIME
was chosen as 30days, equivalent to 2592000s, the authors demonstrated that, this time filtering,