CESM2.1.3 CISM Namelist Definitions
Model Version: 2.1.3
Change CESM Version
Component Tag:
cism-release-cesm2.1.2_02
HTML Created:
2020-02-13
Variable | Namelist Group | Category | Entry Type | Valid Values | Possible Default Values | Description and out-of-the-box Default |
---|---|---|---|---|---|---|
cism_debug | cism_params | cism | logical | ['.true.', '.false.'] | .false. |
Determines whether extra diagnostics are printed in the cism log file Default: false |
cisminputfile | derived | cism | char*256 | ['any char'] | is glc/cism/gland20.input_c150415.nc for: {'cism_phys': 'cism1', 'glc_grid': 'gland20'} is glc/cism/IceSheetData_UMontana/PresentDayGreenland/Greenland_5km_v1.1_SacksRev_c160720.nc for: {'cism_phys': 'cism1', 'glc_grid': 'gland5UM'} is glc/cism/gland20.input_c150415.nc for: {'cism_phys': 'cism2', 'glc_grid': 'gland20'} is glc/cism/Greenland/glissade/init/greenland_4km_epsg3413_c171126.nc for: {'cism_phys': 'cism2', 'glc_grid': 'gland4'} |
Input file Default: For startup runs or hybrid runs with CISM_OBSERVED_IC=TRUE, a resolution-dependent initial conditions file (e.g., gland20.input_c150415.nc). For branch/hybrid runs with CISM_OBSERVED_IC=FALSE, a restart file name built based on RUN_REFCASE and RUN_REFDATE. |
ice_flux_routing | cism_params | cism | char*64 | ['ocn', 'ice'] | ocn |
Code describing how the solid ice runoff flux (i.e., calving) should be routed. ocn: all solid ice goes to the ocean component ice: all solid ice goes to the sea ice component Default: ocn |
paramfile | cism_params | cism | char*100 | ['any char'] | Name of top-level configuration file for CISM (Determined by scripts -- cannot be set by user) |
|
test_coupling | cism_params | cism | logical | ['.true.', '.false.'] | .false. |
If this is set to true, it sets the mass balance timestep to 1 day. This means the ice dynamics is called after one day of climate simulation. THIS IS ONLY FOR TESTING OF COUPLING PROCEDURES, NOT TO BE USED FOR SCIENCE. |
zero_gcm_fluxes | cism_params | cism | logical | ['.true.', '.false.'] | is .false. for: {'cism_evolve': 'TRUE', 'glc_two_way_coupling': 'TRUE'} is .true. for: {'cism_evolve': 'TRUE', 'glc_two_way_coupling': 'FALSE'} is .true. for: {'cism_evolve': 'FALSE', 'glc_two_way_coupling': 'TRUE'} is .true. for: {'cism_evolve': 'FALSE', 'glc_two_way_coupling': 'FALSE'} |
If true, zero out all fluxes sent to the GCM Default: Depends on GLC_TWO_WAY_COUPLING xml variable |
evolve_ice | cism_config_climate | cism_config_climate | integer | ['0', '1'] | is 1 for: {'cism_evolve': 'TRUE'} is 0 for: {'cism_evolve': 'FALSE'} |
0: Do not let the ice sheet evolve (hold ice state fixed at initial condition) 1: Let the ice sheet evolve Default: 1 |
ice_tstep_multiply | cism_config_climate | cism_config_climate | integer | ['any integer'] | Ice time-step multiplier: allows asynchronous climate-ice coupling Default: (use hard-coded default- currently 1) |
|
dew | cism_config_grid | cism_config_grid | real | ['any real'] | is 20000. for: {'glc_grid': 'gland20'} is 5000. for: {'glc_grid': 'gland5UM'} is 4000. for: {'glc_grid': 'gland4'} |
Node spacing in x-direction (m) Default: resolution-dependent |
dns | cism_config_grid | cism_config_grid | real | ['any real'] | is 20000. for: {'glc_grid': 'gland20'} is 5000. for: {'glc_grid': 'gland5UM'} is 4000. for: {'glc_grid': 'gland4'} |
Node spacing in y-direction (m) Default: resolution-dependent |
ewn | cism_config_grid | cism_config_grid | integer | ['any integer'] | is 76 for: {'glc_grid': 'gland20'} is 301 for: {'glc_grid': 'gland5UM'} is 416 for: {'glc_grid': 'gland4'} |
Number of nodes in x-direction Default: resolution-dependent |
global_bc | cism_config_grid | cism_config_grid | integer | ['0', '1', '2'] | is 0 for: {'cism_phys': 'cism1'} is 1 for: {'cism_phys': 'cism2'} |
Global boundary conditions 0: Doubly periodic 1: Free outflow; scalars in global halo set to zero 2: No penetration; outflow set to zero at global boundaries (only supported for Glissade dycore) Default: 0 for cism1, 1 for cism2 |
nsn | cism_config_grid | cism_config_grid | integer | ['any integer'] | is 141 for: {'glc_grid': 'gland20'} is 561 for: {'glc_grid': 'gland5UM'} is 704 for: {'glc_grid': 'gland4'} |
Number of nodes in y-direction Default: resolution-dependent |
upn | cism_config_grid | cism_config_grid | integer | ['any integer'] | 11 |
Number of nodes in z-direction Default: 11 |
con | cism_config_gthf | cism_config_gthf | real | ['any real'] | thermal conductivity of lithosphere (W m-1 K-1) Only relevant if gthf = 2 Default: (use hard-coded default - currently 3.3) |
|
nlayer | cism_config_gthf | cism_config_gthf | integer | ['any integer'] | Number of vertical layers Only relevant if gthf = 2 Default: (use hard-coded default - currently 20) |
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num_dim | cism_config_gthf | cism_config_gthf | integer | ['1', '3'] | 1: 1D calculations 3: 3D calculations Only relevant if gthf = 2 Default: (use hard-coded default - currently 1) |
|
numt | cism_config_gthf | cism_config_gthf | integer | ['any integer'] | Number of time steps for spinning up GTHF calculations Only relevant if gthf = 2 Default: (use hard-coded default - currently 0) |
|
rho | cism_config_gthf | cism_config_gthf | real | ['any real'] | Density of lithosphere (kg m-3) Only relevant if gthf = 2 Default: (use hard-coded default - currently 3300.) |
|
rock_base | cism_config_gthf | cism_config_gthf | real | ['any real'] | Depth below sea-level at which geothermal heat gradient is applied (m) Only relevant if gthf = 2 Default: (use hard-coded default - currently -5000.) |
|
shc | cism_config_gthf | cism_config_gthf | real | ['any real'] | Specific heat capacity of lithosphere (J kg-1 K-1) Only relevant if gthf = 2 Default: (use hard-coded default - currently 1000.) |
|
surft | cism_config_gthf | cism_config_gthf | real | ['any real'] | Initial surface temperature (degrees C) Only relevant if gthf = 2 Default: (use hard-coded default - currently 2.) |
|
glissade_maxiter | cism_config_ho_options | cism_config_ho_options | integer | ['any integer'] | 50 |
Maximum number of nonlinear iterations to be used by the Glissade velocity solver Default: 50 |
which_ho_approx | cism_config_ho_options | cism_config_ho_options | integer | ['-1', '0', '1', '2', '3', '4'] | 4 |
Flag that indicates which Stokes approximation to use with the Glissade dycore. Not valid for other dycores. -1: Shallow-ice approximation, Glide-type calculation (uses glissade_velo_sia) 0: Shallow-ice approximation, vertical-shear stresses only (uses glissade_velo_higher) 1: Shallow-shelf approximation, horizontal-plane stresses only (uses glissade_velo_higher) 2: Blatter-Pattyn approximation with both vertical-shear and horizontal-plane stresses (uses glissade_velo_higher) 3: Vertically integrated 'L1L2' approximation with vertical-shear and horizontal-plane stresses (uses glissade_velo_higher) 4: Depth-integrated viscosity approximation based on Goldberg (2011) (uses glissade_velo_higher) Default: 4 |
which_ho_assemble_beta | cism_config_ho_options | cism_config_ho_options | integer | ['0', '1'] | 1 |
Flag that describes how beta terms are assembled in the Glissade finite-element calculation 0: Standard finite-element calculation (which effectively smooths beta) 1: Apply local value of beta at each vertex Default: 1 |
which_ho_assemble_bfric | cism_config_ho_options | cism_config_ho_options | integer | ['0', '1'] | 1 |
Flag that describes how the basal friction heat flux is computed in the Glissade finite-element calculation Not valid for other dycores 0: Standard finite-element calculation summing over quadrature points 1: Apply local value of beta*(u^2 + v^2) at each vertex Default: 1 |
which_ho_assemble_taud | cism_config_ho_options | cism_config_ho_options | integer | ['0', '1'] | 1 |
Flag that describes how driving-stress terms are assembled in the Glissade finite-element calculation Not valid for other dycores 0: Standard finite-element calculation (which effectively smooths the driving stress) 1: Apply local value of driving stress at each vertex Default: 1 |
which_ho_babc | cism_config_ho_options | cism_config_ho_options | integer | ['0', '1', '2', '3', '4', '5', '6', '7', '8', '9', '10', '11', '12', '13', '14'] | 3 |
Basal boundary condition for higher order dynamical core 0: spatially uniform value (low value of 10 Pa yr-1 by default) 1: large value for frozen bed, lower value for bed at pressure melting point 2: treat beta value as a till yield stress (in Pa) using Picard iteration 3: pseudo-plastic basal sliding law; can model linear, power-law or plastic behavior 4: very large value for beta to enforce no slip everywhere 5: beta field passed in from .nc input file as part of standard i/o 6: no slip everywhere (using Dirichlet BC rather than large beta) 7: treat beta value as till yield stress (in Pa) using Newton-type iteration (in development) 8: beta field as prescribed for ISMIP-HOM test C (serial only) 9: power law 10: Coulomb friction law using effective pressure, with flwa from lowest ice layer 11: Coulomb friction law using effective pressure, with constant basal flwa 12: basal stress is the minimum of Coulomb and power-law values, as in Tsai et al. (2015) 13: power law based on effective pressure 14: simple hard-coded pattern (useful for debugging) Default: 3 |
which_ho_bwat | cism_config_ho_options | cism_config_ho_options | integer | ['0', '1', '2'] | 2 |
Basal water depth 0: Set to zero everywhere 1: Set to constant everywhere, to force T = Tpmp. 2: Local basal till model with constant drainage Default: 2 |
which_ho_calving_front | cism_config_ho_options | cism_config_ho_options | integer | ['0', '1'] | 0 |
Flag that indicates whether to use a subgrid calving front parameterization 0: No subgrid calving front parameterization 1: Use subgrid calving front parameterization Default: 0 |
which_ho_disp | cism_config_ho_options | cism_config_ho_options | integer | ['-1', '0', '1'] | 1 |
Method for computing the dissipation during the temperature calculation -1: no dissipation 0: 0-order SIA approx. 1: 1st order solution (e.g., Blatter-Pattyn) Default: 1 |
which_ho_effecpress | cism_config_ho_options | cism_config_ho_options | integer | ['0', '1', '2', '3', '4'] | 4 |
Flag that describes effective pressure calculation for higher order dynamical core 0: N = overburden pressure, rhoi*grav*thck 1: N is reduced where the bed is at or near the pressure melting point 2: N is reduced where there is melting at the bed 3: N is reduced due to the connection of subglacial water to the ocean 4: N is reduced where basal water is present Default: 4 |
which_ho_efvs | cism_config_ho_options | cism_config_ho_options | integer | ['0', '1', '2'] | 2 |
How effective viscosity is computed for higher-order dynamical core 0: constant value 1: multiple of flow factor 2: compute from effective strain rate Default: 2 |
which_ho_gradient | cism_config_ho_options | cism_config_ho_options | integer | ['0', '1', '2'] | 0 |
Which gradient operator to use in the Glissade dycore. Not valid in other dycores. NOTE: Upstream may be better for ice evolution because it damps checkerboard noise. 0: Centered gradient 1: First-order accurate upstream gradient 2: Second-order accurate upstream gradient Default: 0 |
which_ho_gradient_margin | cism_config_ho_options | cism_config_ho_options | integer | ['0', '1', '2'] | 1 |
How to compute the gradient at the ice margin in the Glissade dycore. Not valid for other dycores. Note: Gradients are always computed at edges with ice on both sides. The methods differ in whether gradients are computed when an ice-covered cell lies above an ice-free cell (land or ocean). 0: Compute edge gradient when either cell is ice-covered 1: Compute edge gradient for ice-covered cell above ice-free land (not ocean) 2: Compute edge gradient only when both cells have ice Default: 1 |
which_ho_ground | cism_config_ho_options | cism_config_ho_options | integer | ['0', '2'] | 0 |
Flag that indicates how the grounded ice fraction is computed in the Glissade dycore Not valid for other dycores 0: fground = 0 in floating cells (based on flotation condition), else fground = 1 1: [NOT SUPPORTED] fground between 0 and 1 (inclusive), based on a grounding line parameterization 2: fground = 1 in all cells Default: 0 |
which_ho_ground_bmlt | cism_config_ho_options | cism_config_ho_options | integer | ['0', '1'] | 0 |
Flag that indicates how to compute bmlt_float in partly grounded cells 0: Apply bmlt_float in all floating cells, including partly grounded cells 1: Do not apply bmlt_float in partly grounded cells Default: 0 |
which_ho_nonlinear | cism_config_ho_options | cism_config_ho_options | integer | ['0', '1'] | is 1 for: {'dycore': '1'} is 0 for: {'dycore': '2'} |
Method for solving the nonlinear iteration when solving the first-order momentum balance 0: use the standard Picard iteration 1: use Jacobian Free Newton Krylov (JFNK) method [GLAM only] Default: 1 for dycore = 1, 0 for dycore = 2 |
which_ho_precond | cism_config_ho_options | cism_config_ho_options | integer | ['0', '1', '2'] | 1 |
Flag that indicates which Stokes preconditioner to use in the Glissade dycore. Not valid for other dycores. 0: No preconditioner 1: Diagonal preconditioner 2: Physics-based shallow-ice preconditioner Default: 1 |
which_ho_resid | cism_config_ho_options | cism_config_ho_options | integer | ['0', '1', '2', '3', '4'] | 4 |
Method for computing residual in Payne/Price dynamical core 0: maxval 1: maxval ignoring basal velocity 2: mean value 3: L2 norm of system residual, Ax-b=resid 4: L2 norm of system residual relative to rhs, |Ax-b|/|b| Default: 4 |
which_ho_sparse | cism_config_ho_options | cism_config_ho_options | integer | ['-1', '0', '1', '2', '3', '4'] | is 3 for: {'dycore': '2'} is 1 for: {'cism_use_trilinos': 'FALSE', 'dycore': '1'} is 4 for: {'cism_use_trilinos': 'TRUE', 'dycore': '1'} |
Method for solving the sparse linear system that arises from the higher-order solver -1: SLAP (serial) Preconditioned conjugate gradient, incomplete Cholesky preconditioner 0: SLAP (serial) Biconjugate gradient, incomplete LU preconditioner 1: SLAP (serial) GMRES, incomplete LU preconditioner 2: Native PCG, parallel-enabled, standard solver 3: Native PCG, parallel-enabled, Chronopoulos-Gear solver 4: standalone interface to Trilinos The use of trilinos is NOT SUPPORTED in CESM runs. Default: 3 if dycore = 2, 1 if dycore = 1 and cism_use_trilinos = FALSE |
which_ho_thermal_timestep | cism_config_ho_options | cism_config_ho_options | integer | ['0', '1', '2'] | 2 |
0: vertical thermal solve before transport solve 1: vertical thermal solve after transport solve 2: vertical thermal solve split; both before and after transport solve Default: 2 |
asthenosphere | cism_config_isostasy | cism_config_isostasy | integer | ['0', '1'] | 0: fluid mantle, isostatic adjustment happens instantaneously 1: relaxing mantle, mantle is approximated by a half-space Only relevant if isostasy = 1 Default: (use hard-coded default - currently 1) |
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flexural_rigidity | cism_config_isostasy | cism_config_isostasy | real | ['any real'] | Flexural rigidity of the lithosphere Only relevant if 'lithosphere' is set to 1 Default: (use hard-coded default - currently 0.24e25) |
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lithosphere | cism_config_isostasy | cism_config_isostasy | integer | ['0', '1'] | 0: local lithosphere, equilibrium bedrock depression is found using Archimedes' principle 1: elastic lithosphere, flexural rigidity is taken into account Only relevant if isostasy = 1 Default: (use hard-coded default - currently 1) |
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lithosphere_period | cism_config_isostasy | cism_config_isostasy | real | ['any real'] | Lithosphere update period (years) Only relevant if isostasy = 1 Default: (use hard-coded default - currently 100.) |
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relaxed_tau | cism_config_isostasy | cism_config_isostasy | real | ['any real'] | Characteristic time constant of relaxing mantle (years) Only relevant if isostasy = 1 Default: (use hard-coded default - currently 4000.) |
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whichrelaxed | cism_config_isostasy | cism_config_isostasy | integer | ['0', '1', '2'] | 0: relaxed topography is read from a separate variable 1: first time slice of input topography is assumed to be relaxed 2: first time slice of input topography is assumed to be in isostatic equilibrium with ice thickness Default: (use hard-coded default - currently 0) |
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basal_mass_balance | cism_config_options | cism_config_options | integer | ['0', '1'] | 1 |
0: not in continuity equation 1: in continuity equation Default: 1 |
basal_water | cism_config_options | cism_config_options | integer | ['0', '1', '2', '3'] | Determines the treatment of basal water Only valid for Glide dycore (cism1) 0: Set to zero everywhere 1: Calculated from local water balance 2: Compute the basal water flux, then find depth via calculation 3: Set to constant everywhere (10m), to force T = Tpmp Default: (use hard-coded default - currently 0) |
|
bmlt_float | cism_config_options | cism_config_options | integer | ['0', '1', '2', '3', '4'] | 0 |
Basal melt rate for floating ice 0: Basal melt rate = 0 for floating ice 1: Depth-dependent basal melt rate for floating ice as prescribed for MISMIP+ 2: Basal melt rate = constant for floating ice (with option to selectively mask out melting) 3: Depth-dependent basal melt rate for floating ice 4: External basal melt rate field (from input file or coupler) 5: [NOT SUPPORTED] Basal melt rate for floating ice from MISOMIP ocean forcing with plume model Default: 0 |
calving_domain | cism_config_options | cism_config_options | integer | ['0', '1'] | 1 |
0: Calve only at ocean edge 1: Calve wherever the calving criterion is met Default: 1 |
calving_init | cism_config_options | cism_config_options | integer | ['0', '1'] | 1 |
0: Do not calve at initialization 1: Calve at initialization Default: 1 |
cull_calving_front | cism_config_options | cism_config_options | logical | ['.true.', '.false.'] | Expert setting. If true, then cull calving_front cells at initialization. This can make the run more stable by removing long, thin peninsulas. If this is set, then also need to set ncull_calving_front. Default: (use hard-coded default - currently .false.) |
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diag_minthck | cism_config_options | cism_config_options | integer | ['0', '1'] | How to determine minimum thickness for diagnostic 0: global diagnostics include all cell with H > 0 1: global diagnostics include all cells with H > thklim This change only affects log files, not output .nc files Default: (use hard-coded default - currently 1) |
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dm_dt_diag | cism_config_options | cism_config_options | integer | ['0', '1'] | 1 |
Switch units from kg/s to Gt/yr in the log file 0: use kg/s unit in log file 1: use Gt/yr unit in log file This change only affects log files, not output .nc files Default: 1 |
dycore | cism_config_options | cism_config_options | integer | ['0', '2'] | is 0 for: {'cism_phys': 'cism1'} is 2 for: {'cism_phys': 'cism2'} |
Which dycore to use 0: Glide dycore (SIA, serial only) 1: NOT SUPPORTED: glam dycore (HO, FDM, serial or parallel) Note that this option is not allowed within CESM, because it is buggy 2: Glissade dycore (HO, FEM, serial or parallel) Default: 0 for cism1, 2 for cism2 |
evolution | cism_config_options | cism_config_options | integer | ['0', '2', '3', '4', '5'] | is 0 for: {'cism_phys': 'cism1'} is 3 for: {'cism_phys': 'cism2'} |
0: pseudo-diffusion 1: ADI scheme [CANNOT BE USED: RESTARTS ARE NOT EXACT] 2: diffusion 3: remap thickness 4: 1st order upwind 5: no thickness evolution Options 0, 1 and 2 are for Glide dycore only Options 3, 4 and 5 are for Glissade dycore only Default: 0 for cism1, 3 for cism2 |
flow_law | cism_config_options | cism_config_options | integer | ['0', '1', '2', '3'] | 2 |
0: Constant value, taken from default_flwa 1: Uniform value equal to the Paterson-Budd value at -10 deg C 2: Paterson-Budd temperature-dependent relationship 3: Read flwa/flwastag from file Default: 2 |
gthf | cism_config_options | cism_config_options | integer | ['0', '1', '2'] | is 0 for: {'cism_phys': 'cism1'} is 1 for: {'cism_phys': 'cism2'} |
0: prescribed uniform geothermal heat flux 1: read 2D geothermal flux field from input file, if present (if absent, fall back to prescribed uniform geothermal heat flux) 2: calculate geothermal flux using 3d diffusion Default: 0 for cism1, 1 for cism2 |
isostasy | cism_config_options | cism_config_options | integer | ['0', '1'] | 0 |
0: no isostasy 1: compute isostasy Default: 0 |
limit_marine_cliffs | cism_config_options | cism_config_options | logical | ['.true.', '.false.'] | .true. |
If true, then thin marine-based cliffs based on a thickness threshold Default: .true. |
marine_margin | cism_config_options | cism_config_options | integer | ['0', '1', '2', '3', '4', '5', '6', '7', '8', '9'] | 1 |
Calving 0: No calving 1: Set thickness to zero if floating 2: Lose a fraction of floating ice at marine margin 3: Set thickness to zero if relaxed bedrock is more than a certain water depth (marine_limit) 4: Set thickness to zero if present bedrock topography lies below a certain water depth (marine_limit) 5: Set thickness to zero based on grid location (field 'calving_mask') 6: Set thickness to zero if ice at marine margin is thinner than a certain value (calving_minthck) 7: Set thickness to zero based on stress (eigencalving) criterion 8: [NOT SUPPORTED] Calve ice that is sufficiently damaged 9: [NOT SUPPORTED] Huybrechts grounding line scheme for Greenland initialization Default: 1 |
periodic_ew | cism_config_options | cism_config_options | integer | ['0', '1'] | 0: no periodic EW boundary conditions 1: periodic EW boundary conditions (This is a Glimmer serial option. The parallel code enforces periodic EW and NS boundary conditions by default.) Default: (use hard-coded default - currently 0) |
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remove_icebergs | cism_config_options | cism_config_options | logical | ['.true.', '.false.'] | .true. |
If true, then identify and remove icebergs after calving. These are connected regions with zero basal traction and no connection to grounded ice. Safer to make it true (and this is needed for stability when allowing floating ice with more advanced calving options), but not necessary for all applications. Default: .true. |
restart | cism_config_options | cism_config_options | integer | ['0', '1'] | Restart the model if set to 1. This allows for exact restarts from previous initial conditions Default: 0 for startup or hybrid with CISM_OBSERVED_IC=TRUE, 1 for hybrid/branch with CISM_OBSERVED_IC=FALSE |
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sigma | cism_config_options | cism_config_options | integer | ['0', '2', '3', '4'] | 0 |
How to determine sigma values 0: compute standard Glimmer sigma coordinates 1: sigma coordinates are given in external file [NOT ALLOWED WHEN RUNNING CISM IN CESM] 2: read sigma coordinates from config file (from sigma_levels) 3: evenly spaced levels, as required for glam dycore 4: compute Pattyn sigma coordinates Default: 0 |
slip_coeff | cism_config_options | cism_config_options | integer | ['0', '1', '2', '3', '4', '5'] | 0 |
Basal traction parameter Glide or Glissade local SIA (which_ho_approx = -1) only. 0: no basal sliding 1: constant basal traction coefficient 2: constant coefficient where basal water is present, else no sliding 3: constant coefficient where the basal temperature is at the pressure melting point, else no sliding 4: coefficient is proportional to basal melt rate 5: coefficient is a linear function of basal water depth Default: 0 |
temp_init | cism_config_options | cism_config_options | integer | ['0', '1', '2', '3', '4'] | is 2 for: {'cism_phys': 'cism1'} is 3 for: {'cism_phys': 'cism2'} |
Temperature initialization method 0: Initialize temperature to 0 C 1: Initialize temperature to surface air temperature 2: Initialize temperature with a linear profile in each column 3: Initialize temperature with an advective-diffusive balance in each column 4: Initialize temperature from external file Default: 3 for cism2; 2 for cism1 |
temperature | cism_config_options | cism_config_options | integer | ['0', '1', '2', '3'] | 1 |
Determines the temperature solution method 0: isothermal: set column to surface air temperature 1: prognostic temperature solution 2: do NOTHING: hold temperatures steady at initial value 3: prognostic enthalpy solution Default: 1 |
vertical_integration | cism_config_options | cism_config_options | integer | ['0', '1'] | 0 |
Method of integration used to obtain vertical velocity 0: standard vertical integration 1: vertical integration constrained to obey an upper kinematic boundary condition Default: 0 |
basal_tract_const | cism_config_parameters | cism_config_parameters | real | ['any real'] | 1.e-4 |
(m yr-1 Pa-1) Relevant only when slip_coeff is relevant (Glide or Glissade local SIA) Default: 1.e-4 |
basal_tract_max | cism_config_parameters | cism_config_parameters | real | ['any real'] | (m yr-1 Pa-1) (Only used for slip_coeff = BTRC_LINEAR_BMLT) Default: (use hard-coded default - currently 0.) |
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basal_tract_slope | cism_config_parameters | cism_config_parameters | real | ['any real'] | (Pa-1) (Only used for slip_coeff = BTRC_LINEAR_BMLT) Default: (use hard-coded default - currently 0.) |
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basal_tract_tanh | cism_config_parameters | cism_config_parameters | real(5) | ['any real(5)'] | 5-element list of values (Only used for slip_coeff = BTRC_TANH_BWAT) Default: (use hard-coded default - currently 0.2d0, 0.5d0, 0.0d0 ,1.0d-2, 1.0d0) |
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beta_grounded_min | cism_config_parameters | cism_config_parameters | real | ['any real'] | 100. |
Minimum value of beta for grounded ice (Pa yr m-1) (Applies only to Glissade higher-order dycore) Default: 100. |
bmlt_float_depth_frzmax | cism_config_parameters | cism_config_parameters | real | ['any real'] | 0. |
Parameter for bmlt_float=3 (depth-dependent basal melt rate for floating ice): Max freezing rate near surface (m/yr). (Ignored for other bmlt_float options.) Default: 0. |
bmlt_float_depth_meltmax | cism_config_parameters | cism_config_parameters | real | ['any real'] | 10. |
Parameter for bmlt_float=3 (depth-dependent basal melt rate for floating ice): Max melt rate at depth (m/yr). (Ignored for other bmlt_float options.) Default: 10. |
bmlt_float_depth_zfrzmax | cism_config_parameters | cism_config_parameters | real | ['any real'] | -100. |
Parameter for bmlt_float=3 (depth-dependent basal melt rate for floating ice): Depth (m) above which bmlt_float = -frzmax. (Ignored for other bmlt_float options.) Default: -100. |
bmlt_float_depth_zmelt0 | cism_config_parameters | cism_config_parameters | real | ['any real'] | -200. |
Parameter for bmlt_float=3 (depth-dependent basal melt rate for floating ice): Depth (m) where bmlt_float = 0. (Ignored for other bmlt_float options.) Default: -200. |
bmlt_float_depth_zmeltmax | cism_config_parameters | cism_config_parameters | real | ['any real'] | -500. |
Parameter for bmlt_float=3 (depth-dependent basal melt rate for floating ice): Depth (m) below which bmlt_float = meltmax. (Ignored for other bmlt_float options.) Default: -500. |
bmlt_float_h0 | cism_config_parameters | cism_config_parameters | real | ['any real'] | 75. |
Scale for sub-shelf cavity thickness (m) Default: 75. |
bwat_till_max | cism_config_parameters | cism_config_parameters | real | ['any real'] | 2.0 |
Parameter for local till model: Maximum water depth in till (m) Relevant only for which_ho_bwat = 2 Default: 2.0 |
c_drainage | cism_config_parameters | cism_config_parameters | real | ['any real'] | 1.e-3 |
Parameter for local till model: Uniform drainage rate (m/yr) Relevant only for which_ho_bwat = 2 Default: 1.e-3 |
calving_fraction | cism_config_parameters | cism_config_parameters | real | ['any real'] | Fraction of ice lost to calving (marine_margin = 2 only) Default: (use hard-coded default - currently 0.2) |
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calving_minthck | cism_config_parameters | cism_config_parameters | real | ['any real'] | 100. |
Minimum thickness of floating ice at marine edge before it calves (m) Default: 100. |
calving_timescale | cism_config_parameters | cism_config_parameters | real | ['any real'] | 0. |
Timescale for calving (yr) (Glissade only) calving_thck = thck*max(dt/calving_timescale,1) If calving_timescale = 0, then the full column calves at once Default: 0. |
cliff_timescale | cism_config_parameters | cism_config_parameters | real | ['any real'] | 0. |
Time scale (yr) for limiting marine cliffs (Glissade only) Default: 0. |
damage_constant | cism_config_parameters | cism_config_parameters | real | ['any real'] | Damage rate (1/yr) per unit stress (Pa) [NOT SUPPORTED] Default: (use hard-coded default - currently 1.e-7) |
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damage_threshold | cism_config_parameters | cism_config_parameters | real | ['any real'] | Damage threshold for calving [NOT SUPPORTED] Default: (use hard-coded default - currently 0.75) |
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default_flwa | cism_config_parameters | cism_config_parameters | real | ['any real'] | Glen's A to use in isothermal case, i.e, when temperature = 0 Default: (use hard-coded default - currently 1.e-16) |
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effecpress_bmlt_threshold | cism_config_parameters | cism_config_parameters | real | ['any real'] | Basal melting range over which N ramps from a small value to full overburden (m/yr) Relevant only for which_ho_effecpress = 2 Default: (use hard-coded default - currently 1.0d-3) |
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effecpress_bpmp_threshold | cism_config_parameters | cism_config_parameters | real | ['any real'] | Parameter for reducing the effective pressure where the bed is warm, saturated or connected to the ocean: Temperature range over which N ramps from a small value to full overburden (deg C) Only applies for which_ho_effecpress = 1. Default: (use hard-coded default - currently 0.1) |
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effecpress_delta | cism_config_parameters | cism_config_parameters | real | ['any real'] | 0.02 |
Parameter for reducing the effective pressure where the bed is warm, saturated or connected to the ocean: Multiplier for effective pressure N where the bed is saturated and/or thawed (unitless) Default: 0.02 |
eigen2_weight | cism_config_parameters | cism_config_parameters | real | ['any real'] | Weight that can increase lateral calving rate (eigencalving_constant). Used only with marine_margin = 7 and 8 Default: (use hard-coded default - currently 1.) |
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eigencalving_constant | cism_config_parameters | cism_config_parameters | real | ['any real'] | Lateral calving rate (m/yr) per unit stress (Pa) Used only with marine_margin = 7 and 8 Default: (use hard-coded default - currently 0.01) |
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flow_factor | cism_config_parameters | cism_config_parameters | real | ['any real'] | is 3. for: {'cism_phys': 'cism1'} is 1. for: {'cism_phys': 'cism2'} |
Flow enhancement parameter for the Arrhenius relationship; typically used in SIA model to speed up the ice. Default: 3.0 for cism1, 1.0 for cism2 |
flow_factor_float | cism_config_parameters | cism_config_parameters | real | ['any real'] | 1. |
Flow enhancement parameter for floating ice. Default is 1.0, but for marine simulations a smaller value may be needed to match observed shelf speeds. Default: 1.0 |
geothermal | cism_config_parameters | cism_config_parameters | real | ['any real'] | -5.e-2 |
Constant geothermal heat flux (W m-2; sign convention is positive down) (May be overwritten by a spatially-varying field in input file [bheatflx]) Default: -0.05 |
ho_beta_const | cism_config_parameters | cism_config_parameters | real | ['any real'] | Only relevant for which_ho_babc = 0 Spatially uniform beta for higher-order dycores (Pa yr m-1) Default: (use hard-coded default - currently 1000.) |
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hydro_time | cism_config_parameters | cism_config_parameters | real | ['any real'] | Time scale for basal water to drain (yr-1) Only relevant for cism1 (Glide dycore) (Not relevant for basal_water=2) Default: (use hard-coded default - currently 1000.) |
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ice_limit | cism_config_parameters | cism_config_parameters | real | ['any real'] | is 100. for: {'cism_phys': 'cism1'} is 1. for: {'cism_phys': 'cism2'} |
Thickness below which ice dynamics is ignored (m) Below this limit, ice is only accumulated Default: 100 for cism1, 1 for cism2 |
log_level | cism_config_parameters | cism_config_parameters | integer | ['0', '1', '2', '3', '4', '5', '6'] | 6 |
Set to a value between 0 (no messages) and 6 (all messages) Default: 6 |
marine_limit | cism_config_parameters | cism_config_parameters | real | ['any real'] | All ice is assumed lost once water depths reach this value (for marine_margin=3 or 4) (m) Note that water depth is negative Default: (use hard-coded default - currently -200.) |
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max_slope | cism_config_parameters | cism_config_parameters | real | ['any real'] | 0.1 |
Maximum surface slope used in the Glissade driving-stress calculation (unitless) Not valid for other dycores Default: 0.1 |
ncull_calving_front | cism_config_parameters | cism_config_parameters | integer | ['any integer'] | Number of times to cull calving_front cells at initialization Set to a larger value to remove thicker peninsulas To use this, also set cull_calving_front to .true. Default: (use hard-coded default - currently 0) |
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periodic_offset_ew | cism_config_parameters | cism_config_parameters | real | ['any real'] | Optional periodic offset for ismip-hom and similar tests May be needed to ensure continuous ice geometry at the edges of the global domain Default: (use hard-coded default - currently 0.) |
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periodic_offset_ns | cism_config_parameters | cism_config_parameters | real | ['any real'] | Optional periodic offset for ismip-hom and similar tests May be needed to ensure continuous ice geometry at the edges of the global domain Default: (use hard-coded default - currently 0.) |
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pmp_offset | cism_config_parameters | cism_config_parameters | real | ['any real'] | 5. |
Offset of initial Tbed from pressure melting point temperature (deg C) Default: 5. |
pseudo_plastic_bedmax | cism_config_parameters | cism_config_parameters | real | ['any real'] | 700. |
Parameter for pseudo-plasting sliding law: Bed elevation above which phi = phimax (m) Default: 700. |
pseudo_plastic_bedmin | cism_config_parameters | cism_config_parameters | real | ['any real'] | -700. |
Parameter for pseudo-plasting sliding law: Bed elevation below which phi = phimin (m) Default: -700. |
pseudo_plastic_phimax | cism_config_parameters | cism_config_parameters | real | ['any real'] | 40. |
Parameter for pseudo-plasting sliding law: max(phi) in pseudo-plastic law, for topg >= bedmin (degrees) 0 < phi < 90 Default: 40. |
pseudo_plastic_phimin | cism_config_parameters | cism_config_parameters | real | ['any real'] | 5. |
Parameter for pseudo-plasting sliding law: min(phi) in pseudo-plastic law, for topg <= bedmin (degrees) 0 < phi < 90 Default: 5. |
pseudo_plastic_q | cism_config_parameters | cism_config_parameters | real | ['any real'] | 0.5 |
Parameter for pseudo-plasting sliding law: Exponent for pseudo-plastic law (unitless) 0 <= q <= 1 q = 1: linear sliding law q = 0: plastic Intermediate values: power law Default: 0.5 |
pseudo_plastic_u0 | cism_config_parameters | cism_config_parameters | real | ['any real'] | 100. |
Parameter for pseudo-plasting sliding law: Threshold velocity for pseudo-plastic law (m yr-1) Default: 100. |
taumax_cliff | cism_config_parameters | cism_config_parameters | real | ['any real'] | 1.e6 |
Yield stress (Pa) for marine-based ice cliffs (Glissade only) Default: 1.e6 |
thck_gradient_ramp | cism_config_parameters | cism_config_parameters | real | ['any real'] | 50. |
Thickness scale (in meters) over which gradients increase from zero to full value (HO only) This parameter does not exist in CISM1 thus CISM2 only. Default: 50. |
sigma_levels | cism_config_sigma | cism_config_sigma | real(20) | ['any real(20)'] | 0.00 0.15 0.30 0.45 0.60 0.75 0.83 0.90 0.95 0.98 1.00 |
List of sigma levels, in ascending order, separated by spaces These run between 0.0 (at top surface) and 1.0 (at lower surface) Only relevant if sigma = 2 Default: 0.00 0.15 0.30 0.45 0.60 0.75 0.83 0.90 0.95 0.98 1.00 |
adaptive_cfl_threshold | cism_config_time | cism_config_time | real | ['any real'] | is 0.0 for: {'cism_phys': 'cism1'} is 0.5 for: {'cism_phys': 'cism2'} |
Adaptively subcycle the advection when advective CFL exceeds this value (Glissade only) (Zero value means no adaptive subcycling.) A nonzero value makes it possible for CISM to run with large velocities that otherwise would violate the advective CFL limit. Results are generally more accurate and stable, however, if the model is run with a time step short enough to avoid subcycling. Default: 0.5 for cism2 |
dt | cism_config_time | cism_config_time | real | ['any real'] | is 0.1 for: {'cism_phys': 'cism1', 'glc_grid': 'gland20'} is 0.05 for: {'cism_phys': 'cism1', 'glc_grid': 'gland5UM'} is 0.5 for: {'cism_phys': 'cism2', 'glc_grid': 'gland20'} is 0.1 for: {'cism_phys': 'cism2', 'glc_grid': 'gland4'} |
Ice sheet timestep (years) Must translate into an integer number of hours Default: Depends on resolution and physics option |
dt_diag | cism_config_time | cism_config_time | real | ['any real'] | is 0.1 for: {'cism_phys': 'cism1', 'glc_grid': 'gland20'} is 0.05 for: {'cism_phys': 'cism1', 'glc_grid': 'gland5UM'} is 0.5 for: {'cism_phys': 'cism2', 'glc_grid': 'gland20'} is 0.1 for: {'cism_phys': 'cism2', 'glc_grid': 'gland4'} |
Diagnostic frequency (years) Set to 0 for no diagnostic output; set to dt for diagnostic output every time step Default: Same as dt |
idiag | cism_config_time | cism_config_time | integer | ['any integer'] | is 19 for: {'glc_grid': 'gland20'} is 76 for: {'glc_grid': 'gland5UM'} is 134 for: {'glc_grid': 'gland4'} |
x coordinate of point for diagnostic output Default: resolution-dependent |
jdiag | cism_config_time | cism_config_time | integer | ['any integer'] | is 57 for: {'glc_grid': 'gland20'} is 228 for: {'glc_grid': 'gland5UM'} is 280 for: {'glc_grid': 'gland4'} |
y coordinate of point for diagnostic output Default: resolution-dependent |
ntem | cism_config_time | cism_config_time | integer | ['any integer'] | Multiplier of ice sheet timestep, dt (in theory, can be real-valued, but values less than 1 are not handled properly, so restricted to being an integer) Default: (use hard-coded default: 1) |
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profile | cism_config_time | cism_config_time | integer | ['any integer'] | Profile period (number of time steps between profiles) Option for Glide dycore only Default: 100 |
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subcyc | cism_config_time | cism_config_time | integer | ['any integer'] | Subcycling for Glissade Default: 1 |
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cesm_history_vars | cism_history | history | char*1024 | ['any char'] | is 'smb artm thk usurf topg uvel vvel uflx vflx temp bmlt bwat' for: {'cism_phys': 'cism1', 'cism_evolve': 'TRUE'} is 'smb artm thk usurf topg' for: {'cism_phys': 'cism1', 'cism_evolve': 'FALSE'} is 'smb artm thk usurf topg uvel vvel temp bmlt bwat beta_internal floating_mask grounded_mask bpmp acab_applied bmlt_applied calving_rate iareaf iareag imass imass_above_flotation total_smb_flux total_bmb_flux total_calving_flux total_gl_flux' for: {'cism_phys': 'cism2', 'cism_evolve': 'TRUE'} is 'smb artm thk usurf topg' for: {'cism_phys': 'cism2', 'cism_evolve': 'FALSE'} |
Space-delimited list of variables output to history file Default: Depends on physics and ice evolution options |
history_frequency | cism_history | history | integer | ['any integer'] | 1 |
History frequency e.g., if history_option=nyears, then 1 = annual, 2 = every two years, etc. Ignored for history_option = 'coupler' Default: 1 |
history_option | cism_history | history | char*64 | ['nyears', 'coupler'] | nyears |
How history frequency is specified nyears: Write history every N years coupler: Get history frequency from coupler (HIST_OPTION/HIST_N xml variables) WARNING: SHOULD NOT BE USED IN PRODUCTION RUNS - frequency metadata not set properly Default: nyears |
decrease_frac | glc_override_nml | overrides | real | ['any real'] | 0.0 |
Fractional decrease in glacier area, per day (should be positive). (days_elapsed * decrease_frac) determines the elevation threshold below which ice_covered is set to 0. When this factor reaches 1, all elevations below 3500 m are set to non-ice-covered. Default: 0 (no decrease) |
decrease_override_delay | glc_override_nml | overrides | integer | ['any integer'] | 0 |
Time delay before beginning decrease_frac overrides (days). Default: 0 (start overrides at beginning of run) |
enable_frac_overrides | glc_override_nml | overrides | logical | ['.true.', '.false.'] | .false. |
Whether to enable overrides of the glc fraction sent to the coupler. If this is false, the other settings in this namelist group are ignored. ONLY MEANT FOR TESTING - SHOULD NOT BE USED FOR SCIENCE RUNS. Default: .false. |
increase_frac | glc_override_nml | overrides | real | ['any real'] | 0.0 |
Fractional increase in glacier area, per day. (days_elapsed * increase_frac) determines the elevation threshold above which ice_covered is set to 1. When this factor reaches 1, all elevations >= 0 m are set to ice-covered. Default: 0 (no increase) |
increase_override_delay | glc_override_nml | overrides | integer | ['any integer'] | 0 |
Time delay before beginning increase_frac overrides (days). Default: 0 (start overrides at beginning of run) |
rearrange_freq | glc_override_nml | overrides | integer | ['any integer'] | 0 |
Frequency (days) at which we rearrange elevation classes. Default: 0 (no flips ever) |
rearrange_override_delay | glc_override_nml | overrides | integer | ['any integer'] | 0 |
Time delay before beginning rearrange_freq overrides (days). Default: 0 (start overrides at beginning of run) |
allow_leapyear | time_manager_nml | time | logical | ['.true.', '.false.'] | .true. is .false. for: {'calendar': 'NO_LEAP'} |
Whether leap years are enabled in the GLC time manager. CAUTION: Leap years don't work correctly with GLC time steps longer than a few months. Default: .false. for NO_LEAP calendar, .true. otherwise |
date_separator | time_manager_nml | time | char*1 | ['any char'] | - |
Character to separate date values Default: '-' |
dt_count | time_manager_nml | time | real | ['any real'] | Time step, in units given by dt_option This generally should not be changed Default: set based on NCPL_BASE_PERIOD and GLC_NCPL in env_run.xml, so that there is one GLC time step per coupling period |
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dt_option | time_manager_nml | time | char*80 | ['steps_per_year', 'steps_per_day', 'seconds', 'hours'] | GLC time-step units This generally should not be changed Valid values: steps_per_year, steps_per_day, seconds, hours Default: set based on NCPL_BASE_PERIOD and GLC_NCPL in env_run.xml, so that there is one GLC time step per coupling period |
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iday0 | time_manager_nml | time | integer | ['1', '2', '3', '4', '5', '6', '7', '8', '9', '10', '11', '12', '13', '14', '15', '16', '17', '18', '19', '20', '21', '22', '23', '24', '25', '26', '27', '28', '29', '30', '31'] | Starting day number in month Default: comes from RUN_STARTDATE or RUN_REFDATE |
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ihour0 | time_manager_nml | time | integer | ['0', '1', '2', '3', '4', '5', '6', '7', '8', '9', '10', '11', '12', '13', '14', '15', '16', '17', '18', '19', '20', '21', '22', '23'] | Starting hour of the day Default: 0 |
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iminute0 | time_manager_nml | time | integer | ['0', '1', '2', '3', '4', '5', '6', '7', '8', '9', '10', '11', '12', '13', '14', '15', '16', '17', '18', '19', '20', '21', '22', '23', '24', '25', '26', '27', '28', '29', '30', '31', '32', '33', '34', '35', '36', '37', '38', '39', '40', '41', '42', '43', '44', '45', '46', '47', '48', '49', '50', '51', '52', '53', '54', '55', '56', '57', '58', '59'] | Starting minute of the day Default: 0 |
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imonth0 | time_manager_nml | time | integer | ['1', '2', '3', '4', '5', '6', '7', '8', '9', '10', '11', '12'] | Starting month number Default: comes from RUN_STARTDATE or RUN_REFDATE |
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isecond0 | time_manager_nml | time | integer | ['0', '1', '2', '3', '4', '5', '6', '7', '8', '9', '10', '11', '12', '13', '14', '15', '16', '17', '18', '19', '20', '21', '22', '23', '24', '25', '26', '27', '28', '29', '30', '31', '32', '33', '34', '35', '36', '37', '38', '39', '40', '41', '42', '43', '44', '45', '46', '47', '48', '49', '50', '51', '52', '53', '54', '55', '56', '57', '58', '59'] | Starting second of the minute Default: 0 |
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iyear0 | time_manager_nml | time | integer | ['any integer'] | Starting year number Default: comes from RUN_STARTDATE or RUN_REFDATE |
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runid | time_manager_nml | time | char*128 | ['any char'] | Simulation identifier (ie case name) Default: case name set by create_newcase |
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stop_option | time_manager_nml | time | char*80 | ['never'] | never |
Stop option -- always let the coupler stop the model so use 'never'. Default: 'never' |
Variable | Namelist Group | Category | Entry Type | Valid Values | Possible Default Values | Description and out-of-the-box Default |