GFDL to main, 2023-11-13 #1615
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GFDL to main, 2023-11-13 #1615
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The autoconf Python interpreter search was slightly modified to search for Python even if $PYTHON is set to an empty string. This is done by unsetting PYTHON if it is set but empty, then following the usual macro. This was required since `export PYTHON` in a Makefile will create the `PYTHON` variable but will assign it no value (i.e. empty string). This causes issues in some build environments. The backup `configure~` script was also added to the developer `ac-clean` cleanup rule.
Refactored 6 files in the ALE directory to calculate the nominal depth in thickness units in a single place (it is done in regridding_main now) and pass it to the various places where it is used, in a preparatory step to modify how this calculation is done in non-Boussinesq mode. There are new arguments to several publicly visible routines, including: - Add non_depth_H arguments to hybgen_regrid, build_zstar_grid, build_sigma_grid, build_rho_grid, build_grid_HyCOM1, build_grid_adaptive, build_adapt_column and build_grid_arbitrary - Add optional zScale arguments to build_zstar_grid and build_grid_HyCOM1 - Add unit_scale_type arguments to regridding_main, ALE_regrid_accelerated and ALE_offline_inputs Also eliminated an incorrect rescaling GV%Z_to_H facto when calculating the total column thickness from the layer thicknesses when an ice shelf is used with a Hycom grid. This would have caused dimensional consistency testing to fail. Added the new runtime parameters HYBGEN_H_THIN, HYBGEN_FAR_FROM_SURFACE HYBGEN_FAR_FROM_BOTTOM, and HYBGEN_DENSITY_EPSILON to set previously hard-coded dimensional parameters used in the Hybgen regridding code and store these values in new variables in hybgen_regrid_CS. Two of these are no longer passed to hybgen_column_regrid as separate parameters. By default these new runtime parameters recover the previous hard-coded values. Also eliminated an unused block of code in build_rho_column. Several comments documenting variables or their units were also added. All answers are bitwise identical, but there are 4 new runtime parameters that would appear in some MOM_parameter_doc files and there are changes to the arguments to 11 routines.
As described in issue #372, I would like to be able to create restart files that contain information about the particle location. These files will be written at the same time as other restart files. I cannot add these calls directly to the driver, because the driver does not have information about the particle location. We have added save_MOM6_internal_state as a subroutine in MOM.F90, and we added calls to this subroutine from each of the drivers. We hope this will allow for more new packages to write restart files in the future. Co-authored by Spencer Jones <spencerjones@tamu.edu>
Added the integer valid_SpV_halo to the thermo_var_ptrs type to indicate whether the SpV_array has been updated and its valid halo size, to facilitate error detection and debugging in non-Boussinesq mode. Tv%valid_SpV_halo is set to the halo size in calc_derived_thermo or after a halo update is done to tv%SpV_avg, and it is set to a negative value right after calls that change temperatures and salinities (such as by ALE remapping) unless there is a call to calc_derived_thermo. Tests for the validity of tv%SpV_avg are added to the routines behind thickness_to_dz, with fatal errors issued if invalid arrays would be used, but more tests could perhaps be used in any parameterization routines where tv%SpV_avg is used directly. Handling the updates to tv%SpV_avg this way helps to avoid unnecessary calls to calc_derived_thermo, which in turn has equation of state calls that can be expensive, while also providing essential verification of new code related to the non-Boussinesq code. These tests can probably be commented out or removed for efficiency once there is a full suite of regression tests for the fully non-Boussinesq mode of MOM6. In addition, a new optional debug argument was added to calc_derived_thermo which can be used to triggers checksums for the variables used to calculate tv%SpV_avg. One call to calc_derived_thermo was also added just before the initialization call to ALE_regrid that will be needed with the next commit, but does not change answers yet. All answers are bitwise identical, but there is a new element in a transparent and widely used type and a new optional argument to a public interface.
Use RHO_KV_CONVERT instead of RHO_0 to set the non-Boussinesq version of GV%m_to_H, so that there is a mechanism for testing the independence of the fully non-Boussinesq mode from the Boussinesq reference density. With this change, GV%Z_to_H is not guaranteed to be equal to (GV%Z_to_m*GV%m_to_H), with the latter expression preferred when setting parameters. By default the two parameters are the same, and they will probably only ever differ in testing the code. All Boussinesq solutions are bitwise identical, but there are differences in the description of RHO_KV_CONVERT that will appear in MOM_parameter_doc files.
Add new arguments to 7 routines that will be needed for the non-Boussinesq capability, but do not use them yet, so that there will be fewer cross file dependencies as the various changes are being reviewed simultaneously. The impacted interfaces are MEKE_int, vertvisc_coef, sumSWoverBands, KPP_calculate, differential_diffuse_T_S, set_BBL_TKE, and apply_sponge In the three step_MOM_dyn_... routines and in calculateBuoyancyFlux1d, this change includes calls to thickness_to_dz to calculate the new vertical distance arrays that will be passed into vertvisc_coef or sumSWoverBands. The only place where the new arguments are actually used is in sumSWoverBands and set_opacity where the changes are particularly simple. All answers are bitwise identical, but there are new non-optional arguments to seven publicly visible routines.
* Restore functionality for reading slices from 3d volumes in MOM_io - The recent MOM_io modifications in support of FMS2_io accidentally removed support for reading on-grid data (same horizontal grid as model) k-slices. This is needed in some configurations in the model state initialization. * Add FMS1 interfaces * Additional patches to enable reading ongrid state initialization data - read local 3d volume rather than attempting to slice ongrid data vertically. - Related bugfixes in MOM_io
- We were reading KV_ML_INVZ2 without logging, then checking for KVML and finally logging based on a combination of the two. This had the side affect that we get warnings about not using KVML even if KVML was not present. - The fix checks for KVML first, and then changes the default so that when KVML=1e-4 is replaced by KV_ML_INVZ2=1e-4 we end up with no warnings and KVML can be obsoleted safely. Note: this commit alone does not remove all warnings from the MOM6-examples suite because we still need to fix the MOM_input that still use KVML - KVML needs to be unscaled since it is the default for KV_ML_INVZ2 - tc3 used KVML and has been corrected.
Use the new runtime parameter RHO_PGF_REF instead of RHO_0 to set the reference density that is subtracted off from the other densities when calculating the finite volume pressure gradient forces. Although the answers are mathematically equivalent for any value of this parameter, a judicious choice can reduce the impacts of roundoff errors by about 2 orders of magnitude. By default, RHO_PGF_REF is set to RHO_0, and all answers are bitwise identical. However, there is a new runtime parameter that appears in many of the MOM_parameter_doc.all files.
The message that a file is being created was issued as a WARNING when we all agree it should really be a NOTE. Depth_list.nc is read if it is present to avoid recomputing a sorted list, but the absence of the file is not an error and does not warrant a warning. Changes: - Changed WARNING to NOTE. - Removed MOM_mesg from imports since it wasn't being used.
The interpolation scheme for state-dependent diagnostic coordinates was incorrectly registering as the same parameter as the main model. This meant it was never possible to change the interpolation scheme from the default (which was not the same as the main model). Fix registers the generated parameter name which was always computed but not used. A typical example of the generated parameter is "DIAG_COORD_INTERP_SCHEME_RHO2".
Fixed a bug in which wave_speed_init was effectively discarding any values of mono_N2_depth passed to it via the optional argument mono_N2_depth, but also changed the default value of RESOLN_N2_FILTER_DEPTH, which was previously being discarded, to disable the monotonization and replicate the previous results. There were also clarifying additions made to the description how to disable RESOLN_N2_FILTER_DEPTH. This will change some entries in MOM_parameter_doc files, and it will change solutions in cases that set RESOLN_N2_FILTER_DEPTH to a non-default value and have parameter settings that use the resolution function to scale their horizontal mixing. There are, however, no known active simulations where the answers are expected to change.
Revised the calculation of gprime and the coordinate densities (GV%Rlay) in fully non-Boussinesq mode to use the arithmetic mean of adjacent coordinate densities in the denominator of the expression for g_prime in place of RHO_0. Also use LIGHTEST_DENSITY in place of RHO_0 to specify the top-level coordinate density in certain coordinate modes. Also made corresponding changes to the fully non-Boussinesq APE calculation when CALCULATE_APE is true, and eliminated an incorrect calculation of the layer volumes in non-Boussinesq mode using the Boussinesq reference density that was never actually being used when CALCULATE_APE is false. This commit will change answers in some fully non-Boussinesq calculations, and an existing runtime parameter is used and logged in some new cases, changing the MOM_parameter_doc file in those cases.
Refactored thickness_diffuse when in non-Boussinesq mode to avoid any dependencies on the Boussinesq reference density, and to translate the volume streamfunction into the mass streamfunction using an appropriately defined in-situ density averaged to the interfaces at velocity points. This form follows the suggestions of Appendix A.3.2 of Griffies and Greatbatch (Ocean Modelling, 2012) when in non-Boussinesq mode. Thickness_diffuse_full was also revised to work properly in non-Boussinesq mode (and not depend on the Boussinesq reference density) when no equation of state is used. As a part of these changes, the code now uses thickness-based streamfunctions and other thickness-based internal calculations in MOM_thickness_diffuse. For example, the overturning streamfunctions with this change are now in m3/s in Boussinesq mode, but kg/s in non-Boussinesq mode. These changes use a call to thickness_to_dz to set up a separate variable with the vertical distance across layers, and in non-Boussinesq mode they use tv%SpV_avg to estimate in situ densities. Additional debugging checksums were added to thickness_diffuse. The code changes are extensive with 15 new or renamed internal variables, and changes to the units of 9 other internal variables and 3 arguments to the private routine streamfn_solver. After this change, GV%Rho, GV%Z_to_H and GV%H_to_Z are no longer used in any non-Boussinesq calculations (12 such instances having been elimated). Because some calculations have to be redone with the separate thickness and dz variables, this will be more expensive than the original version. No public interfaces are changed, and all answers are bitwise identical in Boussinesq or semiBoussinesq mode, but they will change in non-Boussinesq mode when the isopycnal height diffusion parameterization is used.
* Salt data structures * First steps at brine plume: pass info from SIS2 * The brine plume parameterization, - including now passing the dimensional scaling tests. * Fix problem when running Tidal_bay case with gnu. * Avoiding visc_rem issues inside land mask. Tweaking the brine plume code. * Using the proper MLD in the brine plumes - it now works better on restart * Always including MLD in call to applyBoundary... - I could move it up and make it not optional. * Adding some OpenMP directives to brine plumes
This commit brings the drifters interface up-to-date with the current version of the drifters package, which requires h (layer thickness) to calculate the vertical movement of particles. The interfaces in the code and in config_src/external are updated to pass this information to the drifters package.
Pass dt_kappa_smooth to calc_isoneutral_slopes and vert_fill_TS in units of [H Z ~> m2 or kg m-1] instead of [Z2 ~> m2] for consistency with the units of other diffusivities in the code and to reduce the depenency on the Boussinesq reference density in non-Boussinesq configurations. In addition to the changes to the units of these two arguments, there is a new unit_scale_type argument to vert_fill_TS and MOM_calc_varT and a new verticalGrid_type argument to MOM_stoch_eos_init. The units of 4 vertical diffusivities in the control structures in 4 different modules are also changed accordingly. All answers are bitwise identical in Boussinesq mode, but they can change for some non-Boussinesq configurations. There are new mandatory arguments to three publicly visible routines.
Added a comment justifying the use of a fixed rescaling factor for the diffusivity used in vert_fill_TS. All answers and output are identical.
Added the new public interface find_ustar to extract the friction velocity from either a forcing type argument, or a mech_forcing_type argument, either directly or from tau_mag, and in non-Boussinesq mode by using the time-evolving surface specific volume. Find_ustar is an overloaded interface to find_ustar_fluxes or find_ustar_mech_forcing, which are the same but for the type of one of their arguments. For now, the subroutines bulkmixedlayer, mixedlayer_restrajt_OM4, mixedlayer_restrat_Bodner and mixedlayer_restrat_BML are calling find_ustar to avoid code duplication during the transition to work in fully non-Boussinesq mode, but it will eventually be used in about another half dozen other places. All Boussinesq answers are bitwise identical, but non-Boussinesq answers will change and become less dependent on the Boussinesq reference density, and there is a new publicly visible interface wrapping two subroutines.
Changed the units of the optional mono_N2_depth argument to wave_speed, wave_speed_init and wave_speed_set_param in thickness units instead of height units. Accordingly, the units of one element each in the diagnostics_CS and wave_speed_CS and a local variable in VarMix_init are also changed to thickness units. The unit descriptions of some comments describing diagnostics were also amended to also describe the non-Boussinesq versions. Because this is essentially just changing when the unit conversion occurs, all answers are bitwise identical, but there are changes to the units of an optional argument in 3 publicly visible routines.
Added the new runtime parameter BT_RHO_LINEARIZED to specify the density that is used to convert total water column thicknesses into mass in non-Boussinesq mode with linearized options in the barotropic solver or when estimating the stable barotropic timestep without access to the full baroclinic model state. The default is set to RHO_0 and answers do not change by default. This new parameter is used in non-Boussinesq mode with some options in btcalc and find_face_areas, when LINEARIZED_BT_CORIOLIS = True or BT_NONLIN_STRESS = False, and in the unit conversion of the ice strength with dynamic pressure. Also cancelled out factors of GV%Z_to_H in MOM_barotropic.F90 to simplify the code and reduce the dependence on the value of GV%Rho_0 in non-Boussinesq mode. This involved changing the units of 4 variables in the barotropic_CS type, 3 internal variables in btstep and an internal variable in barotropic_init to use thickness units. The rescaled internal variable mass_to_Z was also replaced with the equivalent GV%RZ_to_H. There are also 4 new debugging messages. Also modified the units of the gtot_est argument to match those of pbce. There is a new element in barotropic_CS. Because GV%Z_to_H is an exact power of 2 in Boussinesq mode, all answers are bitwise identical in that mode, but in non-Boussinesq mode this conversion involves multiplication and division by GV%Rho_0, so while all answers are mathematically equivalent, this change does change answers at roundoff in non-Boussinesq mode. Additionally there is a new runtime parameter that will appear in some MOM_parameter_doc files.
Use thickness_to_dz to convert layer thicknesses to depths in 4 tracer modules (DOME_tracer, dye_example, ideal_age_example and nw2_tracers) so that this conversion is done correctly in non-Boussineq mode, and there is no longer any dependency on the Boussinesq reference density in that mode. This change includes the addition of a thermo_var_ptrs argument to 5 routines (initialize_DOME_tracer, initialize_dye_tracer, dye_tracer_column_physics ideal_age_tracer_column_physics and count_BL_layers) and changes to the units of some internal variables, and the addition of 6 new 2-d or 3-d arrays with the vertical distance across layers. An unused param_file_type argument to initialize_DOME_tracer was also eliminated. Comments were also added to describe the units of 5 of the variables in the ideal age tracer control structure and 7 internal variables in that same module, and there was some minor cleanup of the formatting cf calls in tracer_flow_control_init. There was some minor refactoring in the ns2_tracers module to use SZK_(GV) instead of SZK_(G) to declare the vertical extent of some arrays, and the vertical indexing convention for interfaces in nw2_tracer_dist was revised from starting at 0 to start at 1 for consistency with all the other code in MOM6. Also moved the code to do halo updates for the physical model state variables and call calc_derived_thermo before calling tracer_flow_control_init, because some routines there are now using the layer average specific volume to convert between thicknesses and heights when in non-Boussinesq mode. All answers in Boussinesq mode are bitwise identical, but these passive tracer modules have slightly different answers in non-Boussinesq mode. There are changes to the non-optional arguments to 4 public interfaces.
Changed a recently added OMP directive for plume_flux from private to firstprivate to reflect how this variable is actually used. This bug was introduced with PR #401, but was causing sporadic failures in some of our pipeline tests with the intel compiler (essentially due to initialized memory when openMP is used) for subsequent commits.
This patch merges the internal `save_restart` function with the new `save_MOM6_internal_state` function into a new general MOM restart function. It also makes an effort to eliminate `MOM_restart` as a driver dependency, narrowing the required MOM API for existing and future drivers. Also removes the `restart_CSp` argument from `MOM_wave_interface_init`, since it appeared to be used for nothing.
MOM simulations typically abort of the restart directory (usually RESTART) are absent. This patch adds POSIX support for mkdir() and creates the directory if it is missing.
Using inquire() to check for directory existence is not possible, since at least one compiler (Intel) does not consider directories to be files. The inquire call is replaced with a C interface to the POSIX stat() function. We do not fully emulate the behavior of stat, but we use its return value to determine existence of directories. This provides a more reliable method for identifying the existence of the directory. This should resolve many of the observed problems with RESTART creation in coupled runs.
Cancelled out factors of GV%Z_to_H in MOM_hor_visc.F90 to simplify the code and reduce the dependence on the value of GV%Rho_0 in non-Boussinesq mode. This involved changing the units of 3 internal variables in horizontal_viscosity and one element in the hor_visc_CS type to use thickness units or their inverse. Because GV%Z_to_H is an exact power of 2 in Boussinesq mode, all answers are bitwise identical in that mode, but in non-Boussinesq mode this conversion involves multiplication and division by GV%Rho_0, so while all answers are mathematically equivalent, this change does change answers at roundoff in non-Boussinesq mode.
Revised the units of 12 vertvisc_type elements to be based on thicknesses, so that vertical viscosities (in [H Z T-1 ~> m2 s-1 or Pa s]) are stored as dynamic viscosites when in non-Boussinesq mode, with analogous changes to the diapycanl diffusivity (now in [H Z T-1 ~> m2 s-1 or kg m-1 s-1]). Similarly changed the units of the 2 Rayleigh drag velocity elements (Ray_u and Ray_v) of the vertvisc_type from vertical velocity units to thickness flux units and to more accurately reflect the nature of these fields. The bottom boundary layer TKE source element (TKE_BBL) was also revised to [H Z2 T-3 ~> m3 s-3 or W m-2]. This commit also adds required changes to the units of the viscosities or shear-driven diffusivities returned from KPP_calculate, calculate_CVMix_shear, calculate_CVMix_conv, Calculate_kappa_shear, Calc_kappa_shear_vertex, calculate_tidal_mixing and calculate_CVMix_tidal. Because GV%Z_to_H is an exact power of 2 in Boussinesq mode, all answers are bitwise identical in that mode, but in non-Boussinesq mode this conversion involves multiplication and division by GV%Rho_0, so while all answers are mathematically equivalent, this change does change answers at roundoff in non-Boussinesq mode unless GV%Rho_0 is chosen to be an integer power of 2.
Rescaled diapycnal diffusivities passed as arguments in non-Boussinesq mode, to be equivalent to the thermal conductivity divided by the heat capacity, analogously to the difference between a kinematic viscosity and a dynamic viscosity, so that the new units are [H Z T-1 ~> m2 s-1 or kg m-1 s-1]. This includes changing the units of 4 arguments to set_diffusivity; 3 arguments each to calculate_bkgnd_mixing, add_drag_diffusivity, add_LOTW_BBL_diffusivity, user_change_diff, calculate_tidal_mixing and add_int_tide_diffusivity; 2 arguments to KPP_calculate, calculate_CVMix_conv, compute_ddiff_coeffs, differential_diffuse_T_S, entrainment_diffusive, double_diffusion, add_MLrad_diffusivity, and calculate_CVMix_tidal; and one argument to energetic_PBL. The units of 36 internal variables were also changed, as were a total of 29 elements in various opaque types, including 8 elements in bkgnd_mixing_cs, 2 in diabatic_CC, 3 in tidal_mixing_diags type, 1 in user_change_diff_CS, 9 in set_diffusivity_CS type, and 6 elements in diffusivity_diags. Two new internal variables were added, and several redundant GV%H_to_Z conversion factors were also cancelled out, some using that GV%H_to_Z*GV%Rho0 = GV%H_to_RZ. Because GV%Z_to_H is an exact power of 2 in Boussinesq mode, all answers are bitwise identical in that mode, but in non-Boussinesq mode this conversion involves multiplication and division by GV%Rho_0, so while all answers are mathematically equivalent, this change does change answers at roundoff in non-Boussinesq mode unless GV%Rho_0 is chosen to be an integer power of 2.
Changed the units for TKE arguments to [H Z2 T-3 ~> m3 s-3 or W m-2] for find_TKE_to_Kd, add_drag_diffusivity, calculate_tidal_mixing and add_int_tide_diffusivity, with similar changes to the units of 21 diagnostics or internal variables in the same routines and in add_LOTW_BBL_diffusivity and add_MLrad_diffusivity. Dozens of unit conversion factors were also cancelled out with these changes, including using that GV%Z_to_H/GV%Rho_0 = GV%RZ_to_H and that GV%Rho_0*GV%H_to_Z = GV%H_to_RZ for both Boussinesq or non-Boussinesq configurations. Because GV%Z_to_H is an exact power of 2 in Boussinesq mode, all answers are bitwise identical in that mode, but in non-Boussinesq mode this conversion involves multiplication and division by GV%Rho_0, so while all answers are mathematically equivalent, this change does change answers at roundoff in non-Boussinesq mode unless GV%Rho_0 is chosen to be an integer power of 2.
* Added ice shelf Coulomb friction law (Schoof 2005, Gagliardini et al 2007) needed for MISMIP+ experiments (Asay-Davis et al 2016).
* +REMAP_AUX needs at least one more halo update. - This one is for CS%u_av, CS%v_av, which need to be updated coming into step_MOM_dyn_split_RK2. * +Next stab at fixing REMAP_AUX fallout. - This fixes the Bering ORLANSKI OBCs for differing processor counts. - This is either the wrong way to do group_pass for OBLIQUE OBC's or there is more wrong with them. * Adding a group pass, still not solving the problem - Problem is in tangential_vel at tile boundaries. It matches right at the boundary, but needs some halo points to match too. * +Fixing oblique OBCs - Without this, u_av and v_av don't update a wide enough halo to get answers to reproduce across different processor counts with oblique OBCs. * Fixed an oopsie with OBC * Getting rid of extra exchange (that didn't help)
Refactored diapyc_energy_req_test and diapyc_energy_req_calc to remove the dependence on the Boussinesq reference density when in non-Boussinesq mode. This includes changes to the scaled units of the Kd_int argument to diapyc_energy_req_calc and the Kd argument to diapyc_energy_req_calc and the addition of a new argument to diapyc_energy_req_calc. A call to thickness_to_dz is used for the thickness unit conversions. There are 5 new internal variables, and changes to the units of several others. These routines are not actively used in MOM6 solutions, but instead they are used for testing and debugging new code, so there are no changes to solutions, but the results of these routines can differ in fully non-Boussinesq mode.
Modified the MOM_diapyc_energy_req.F90 version of find_PE_chg to align more closely with the version in MOM_energetic_PBL.F90, including making PE_chg into a mandatory argument, changing the name of the ColHt_cor argument to PE_ColHt_cor, and modifying some variable descriptions in units. Also removed find_PE_chg_orig from MOM_diapyc_energy_req.F90 and the old_PE_calc code that calls it. Extra values were also added to Te, Te_a and Te_b and the equivalent salinity variables so that the logical branches at (K==2) and (K=nz) could be simplied out of diapyc_energy_req_calc. Because old_PE_calc had been hard-coded to .false., all answers are bitwise identical.
…equired for NW2 (#484) * Update of Zanna-Bolton-2020 closure: code optimization and features required in NW2 configuration * Resolving compilation errors and doxygen by Alistair * Remove force sync for clock * Change naming of functions according to MOM_Zanna_bolton module
- Several edits to the ice shelf solo driver so that it works with the rest of the current MOM6 - Added capability to initialize a surface mass balance (SMB) that is held contstant over time when running from the ice-shelf solo driver (see new subroutine initialize_ice_SMB). This is required for MISMIP+. A constant SMB can also be used from the MOM driver for coupled ice-shelf/ocean experiments (e.g. MISOMIP). - The new, constant SMB is passed into solo_step_ice_shelf, where change_thickness_using_precip is called - Added capability to save both non-time-stamped and time-stamped restart files when using the ice shelf solo driver. This is useful for debugging. - slight reorganization to when ice shelf post_data calls are made - Added safety checks to diag_mediator_end() so that it works with the ice shelf solo-driver, which now calls it instead of (now removed) solo_ice_shelf_diag_mediator_end() routine. Removed the runtime parameter SAVE_BOTH_RESTARTS from the ice shelf solo-driver, which is no longer needed.
-fixed a bug in change_thickness_using_precip (was missing a division by ice density) -optimized ice shelf pass_var calls with optional complete arguments -corrected the grid area to multiply with ice shelf driving stress before its post_data call -changed some order of operations by adding parentheses, with the hope that it would improve symmetry of the ice shelf solution during MISMIP+. There was no effect, but this version of the code was used for MISMIP+ and MISOMIP.
* allow for assigned ice shelf thickness where hmask==3, but still solve for ice sheet velocity
… a partially-filled cell, add the reference thickness contribution from a neighboring filled cell proportionate to its flux into the partially-filled cell. This is more accurate than simply taking the average thickness of all neighboring filled cells. Also fixed incorrect bounds. (#475)
The directory, time and timestamp variables are needed by the particle code in order to write better restart files. I have changed the particles_save_restart interface to add these variables. I have also removed the option to pass temperature and salinity to particles_save_restart, because these variables are not useful for restart.
the module in now able to read in tidal velocities for different tidal harmonics and distribute the energy and distribute TKE input over the different vertical modes. This involves upsizing dimensions of several arrays and mofiying some API. internal_tide_input_CS is promoted to public to facilitate the passing of energy input to MOM_internal_tides
Removed the unused (and unusable) routine build_grid_arbitrary. This routine could not have been used because it had a hard-coded STOP call, and comments in it indicated that it should have been deleted in July, 2013. The run-time parameter setting that would have triggered a call to this routine has been retained for now, but with a fatal error message explaining that this routine has not been implemented. All answers are bitwise identical in any cases that ran before.
Removed the unused routine rescale_grid_bathymetry. This routine was added in August 2018 as a part of the development of the depth unit conversion and dimensional consistency testing, but it is no longer being called now that this conversion is essentially complete (and it has not been called by the code in several years). For the original commit that first added this code, see github.com/mom-ocean/MOM6/commit/ddc9ed1c33a1b7357b213929118ecaa19ae63f9f. All answers are bitwise identical.
Corrected dimensional rescaling bugs in the spherical harmonics SAL code. An issue with horizontal length scaling was corrected by using G%Rad_Earth_L in place of G%Rad_Earth in spherical_harmonics_init. There are new optional tmp_scale arguments to calc_SAL and spherical_harmonics_forward to allow the rescaling to be undone before calling the reproducing sums. This commit also modifies the call to the reproducing sums in spherical_harmonics_forward so that all real or imaginary components are calculated with a single call, which reduces the cost of the SAL calculation reproducing sums from about 6.7 times the cost with non-reproducing sums to just 5.5 times as much in testing with the tides_025 test case. There is also code added to avoid NaNs arising from a square root operating on a negative argument from a 32-bit integer roll-over when a very large number of harmonics components (more than 1024 x 1024) are unadvisedly being used. While this commit corrects the dimensional scaling when HARMONICS_SAL is true, all answers are bitwise identical when no rescaling is used or when the spherical harmonics SAL is not used. There are new optional arguments to two publicly visible interfaces.
Added standard-format unit descriptions for 31 real variables in comments scattered across 14 modules in the core, tracer, and both parameterizations directories. Only comments are changed and all answers are bitwise identical.
Save tv%p_surf in the restart file when USE_PSURF_IN_EOS is true so that the diagnosed potential energy written to the ocean.stats files after a restart matches the energy written at the end of the previous run-segment in certain non-Boussinesq configurations, including the Baltic test case. Because p_surf_EOS is a non-mandatory restart field, there is no problem restarting the run from a restart file created by an older version of the model. The solutions themselves are bitwise identical. This change requires that tv%p_surf is treated as an allocatable pointer to its own array rather than being used as a pointer to the p_surf element of the fluxes or forces structures so that it can be registered as a restart field. At some point tv%p_surf could be converted into an allocatable array instead of a pointer, but this would require more extensive code refactoring. All answers are bitwise identical.
…ename specified by new parameter ICE_SHELF_ENERGYFILE). Currently, this file outputs the kinetic energy and mass of the ice sheet according to the smae parameters used to write the ocean.stats file (TIMEUNIT, ENERGYSAVEDAYS, and ENERGYSAVEDAYS_GEOMETRIC).
A few bug fixes so that the GL_couple=.true. option works correctly. Setting GL_couple=.true. will determine the grounding based on ocean column thickness rather than the typical the hydrostatic equilibrium condition. This has the advantage of accounting for changes in sea level, tides, etc. However, it has the disadvantage of not working with the same thoroughly-tested sub-element grounding line parameterization used for the hydrostatic condition. Instead, it accounts for sub-element grounding line movement by, during the SSA solution, using a grounding mask averaged over all ocean (sub)steps that completed since the last SSA solve. Unlike the hydrostatic sub-element parameterization, the dependence of the GL_couple=.true. scheme on grid resolution has not yet been determined. Qualitatively similar grounding line retreat/advance behavior is achieved with both approaches for MISOMIP IceOcean1 on a 2km grid, but GL_couple=.true. results in a rougher grounding line position with less retreat. Note that this commit also fixed a bug in applying the hydrostatic grounding line approach without its sub-element parameterization (though the sub-element parameterization should also be used anyway).
* This commit fixes a bug where restarts were not bitwise identical for coupled ice sheet/ocean runs. This required adding visc%taux and visc%taux (stress on the ocean under ice shelves) to the ocean restart file. Furthermore, ice shelf geometry-related variables needed to be updated and their halo cells filled (within subroutine update_ice_shelf) before (rather than after) calculating shelf fluxes and pressure to the ocean (subroutine add_shelf_flux). Also fixed a bug to calculate ISS%mass_shelf properly in ice-shelf cells that are only partially-filled (ice-shelf area < cell area) due to advection of the ice-shelf front. * Modified the scheme that attempts to enforce a constant sea level in coupled ice-sheet/ocean runs, where balancing fluxes are applied to part/all of the open ocean to offset the sea level effects caused by changes in ice sheet mass on the ocean. The old scheme assumes the entire ice sheet is floating, and is retained here for the case where CS$override_shelf_movement==.true. and CS%mass_from_file (this approach is used for the MISOMIP tests without a dynamic ice sheet). The new scheme (which is needed for the MISOMIP tests with a dynamic ice sheet, e.g. IceOcean1r and IceOcean1a), accounts for the more general case where some of the ice sheet is grounded. In either case, the ocean balancing fluxes are applied over the entirety of the ice-sheet-free ocean by default. However, if the new parameter CONST_SEA_LEVEL_MISOMIP==.true., the balancing flux is only applied where x>=790 km, which is the sponge region for the MISOMIP tests. The new scheme also requires calculation of ice sheet dHdT, which is now calculated and optionally saved as a useful diagnositc field for any ice sheet simulation. * Eliminated array syntax and added inverse dt variables where needed
Makedep can now exclude prescribed directories in the directory tree used to generate the file lists. This is required for projects which may not follow normal development processes, such as the FMS test programs.
The target (regression) configure step did not use a --with-framework flag and would always build with FMS1, even if FRAMEWORK was set to fms2. This patch adds the flag to its configure step. This patch also does some refactoring of the MOM_ENV and MOM_FCFLAGS setup rules. Values common to all rules are set externally, and additional values for individual rules are appended. Variable syntax also follows Makefile format (spaces around =) rather than POSIX shell (no spaces).
The default FMS build in ac/deps is updated to 2023.03. FMS source now includes a suite of test programs which require explicit preprocessing macros, which can complicate out makedep-based build when those macros are not present. To avoid this, the new "skip" flag has been added to the makedep build. The skip flag should not cause errors or other issues in older versions of FMS which do not have the excluded directory (though perhaps that could or should change in the future).
Revised the recently added brine-plume code to avoid using a vertical sum and to use tv%SpV_avg to determine the brine plume mixing thickness instead of GV%Z_to_H when in non-Boussinesq mode. Several internal brine plume expressions now work in units of H instead of Z, and a total of 5 unit conversion factors were eliminated. This will change certain non-Boussinesq calculations to avoid any dependency on the Boussinesq reference density, but some Boussinesq answers may also be changed and made more robust by avoiding the answer-indeterminate sum() function.
* +Fix for issue #506, tracer OBC bug - it only happens in the advection for certain flow directions, inflow from OBC plus along-boundary flow. * Tracer OBCs need more of an h halo update. - This one should finally fix the processor count issues with OBCs. * Correct the "if" statement. * +Adding more halo points to an exchange - This will change answers if you start with a non-zero velocity. You need three halo points (or maybe cont_stencil) for the continuity solver. - Also trying to put in some initial DEBUG_OBC code. * Fix some DEBUG_OBC logic * Writing to temporary arrays for tres_xy - Way to trick some compiler. * Another fix for DEBUG_OBC * Fixing the whalo troubles for grids that are 2 wide/long. * Exchange all the h_new points. - without this, because we're remapping all the tres points, it dies in debug mode on bad h_new values. * Trying a different exchange - as it was, it was passing my tests, failing the auto-tests. * Fixing the DEBUG_OBC logging * Putting the logging statement back. - Making an error more verbose too.
- Added simple single-thread program to invoke EOS_unit_tests.F90
- Added not-as-simple program to time the cost of calculate_density()
and calculate_spec_vol() for both scalar and array APIs
- Placed in new directory config_src/drivers/timing_tests/
- Renamed MOM_unit_test_driver.F90 to test_MOM_file_parser.F90
- Updated .testing/Makefile
- Added list of programs in config_src/drivers/unit_tests
- These are added to BUILDS if DO_UNIT_TESTS is not blank.
(DO_UNIT_TESTS was an existing macro but it might be uneeded)
- These programs are compiled with code coverage
- Added list of programs in config_src/drivers/timing_tests
- These programs are compiled with optimization and no coverage
- Fixed rule for building UNIT_EXECS (which did not re-build properly
because the central Makefile was trying to model the dependencies
even though those dependencies are in the build/unit/Makefile.dep)
- Added convenient targets build.unit, run.unit, build.timing, run.timing
- Timing tests currently time a loop over 1000 calls (so that the resolution
of the CPU timer is not too large) and 400 samples to collect statistics
on timings. On gaea c5 this takes about 10 seconds.
- The results are written to stdout in json.
- Added placeholder build and run of timing_tests to GH workflow.
- Enabled for [push,pull_request]
- We probably will not be able to use timings from GH but I still want
to exercise the code we know the timing programs aren't broken by a
commit.
- Also added driver for string_functions_unit_tests
Refactored ALE_remap_velocities to separate the code setting the thicknesses at velocity points from the code that actually does the remapping. This includes the creation of the new public routines ALE_remap_set_h_vel and ALE_remap_set_h_vel_via_dz and the replacement the pair of tracer point thickness arguments to ALE_remap_velocities and remap_dyn_split_RK2_aux_vars with a pair of the old and new thicknesses at the velocity points and the elimination of several arguments to these routines that are no longer being used. There are also new internal routines ALE_remap_set_h_vel_partial and ALE_remap_set_h_vel_OBC to apply modifications to the velocity point thicknesses with OBCs and one runtime option. The runtime variable REMAP_UV_USING_OLD_ALG has effectively been moved from MOM_ALE.F90 to MOM.F90, although it is still being read in MOM_ALE_init for use with the accelerated regridding during initialization. All answers are bitwise identical, but there are two new public interfaces and changes to the arguments to two other public interfaces and a run-time parameter was moved between modules resulting in changes to some MOM_parameter_doc files.
This commit fixes a bug to ensure that OBC%debug is always being set when OBCs are in use. After a recent commit, the value of OBC%debug was not being set and was being left in an indeterminate whenever DEBUG_OBC=False or DEBUG=False and DEBUG_OBC was unspecified. This would lead to the model writing out a number of checksums in some cases with open boundary conditions enabled, depending on what value was inherited by the uninitialized OBC%debug. Although this does not change any answers, it will avoid a problem that will write out a large volume of undesired output and greatly slow down configurations with open boundary conditions.
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This PR contains many new features, bugfixes, and overall changes to the MOM6 codebase. In particular, the model now includes a full non-Boussinesq solver alongside the existing Boussinesq and "semi-non-Boussinesq" modes.
Other major features include updates to the ice shelf model, improved particle tracer support, improvements to the computational performance of the Zanna-Bolton parameterization, fixes to the internal tide energetics, brine plume mixing, and self-attraction and loading.
It also includes the usual bundle of bug fixes and code refactors.
Non-Boussinesq
Ice Shelf
Particle Tracers
ZB2020
Internal Tide
Brine Plume Mixing
Self-attraction and Loading
Additional Features
Bugfix
Refactor
save_MOM6_internal_stateNOAA-GFDL/MOM6#403: (@marshallward)Testing
Build
Misc
Contributors