CMS-Flow:Features: Difference between revisions
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='''Other Processes'''= | ='''Other Processes'''= | ||
==Eddy Viscosity== | ==Eddy Viscosity== | ||
Eddy Viscosity in CMS-Flow is not a user definable parameter. A description of the advanced cards related to eddy viscosity is shown in the table below. | Eddy Viscosity in CMS-Flow is not a user definable parameter. A description of the advanced cards related to eddy viscosity is shown in the table below. |
Revision as of 16:40, 16 January 2011
Other Processes
Eddy Viscosity
Eddy Viscosity in CMS-Flow is not a user definable parameter. A description of the advanced cards related to eddy viscosity is shown in the table below.
Card | Arguments | Default | Range | Description | Versions |
---|---|---|---|---|---|
TURBULENCE_MODEL | CHARACTER | SUBGRID | SUBGRID |FALCONER| PARABOLIC | MIXING-LENGTH | Specifies the turbulence model used | >=3.5 |
EDDY_VISCOSITY_CONSTANT | REAL | 1.0E-6 | >=1.0E-6 | Constant contribution or base value of eddy viscosity | >=3.5 |
EDDY_VISCOSITY_BOTTOM | REAL | 0.0667 | 0.01-0.2 | Coefficient related to the contribution to eddy viscosity from the bottom shear | >=3.5 |
EDDY_VISCOSITY_HORIZONTAL | REAL | 0.4 | 0.2-0.6 | Coefficient related to the contribution to eddy viscosity from horizontal velocity gradients | >=3.5 |
EDDY_VISCOSITY_WAVE | REAL | 0.5 | 0.2-1.0 | Coefficient related to the wave bottom friction contribution to eddy viscosity | >=4.0 |
EDDY_VISCOSITY_BREAKING | REAL | 0.05 | 0.04-0.08 | Coefficient related to the wave breaking contribution to eddy viscosity | >=4.0 |
More information can be found here.
Other Features
Parallelization with OpenMP
Both Intel and AMD processors now are shipping chips with multiple cores/processors (henceforth referred to as "processors") available. CMS-Flow is now configured to make use of these extra processes that are available on newer machines.
Additional information on using Multiple Processors with CMS-Flow can be found here.
Advanced Output
The following advanced cards have been added to CMS v4.0 and higher for outputting additional output information, ASCII file output, and more.
Card | Arguments | Description | Default value |
---|---|---|---|
XMDF_COMPRESSION | ON | OFF | Compresses the h5 file by a factor of about 7 | OFF |
WAVE_OUT_TIMES_LIST | integer | Output time series id | 0 |
EDDY_OUT_TIMES_LIST | integer | Output time series id | 0 |
VISC_OUT_TIMES_LIST | integer | Output time series id | 0 |
STRESS_OUT_TIMES_LIST | integer | Output time series id | 0 |
BED_SHEAR_STRESS_OUT_TIMES_LIST | integer | Output time series id | 0 |
GLOBAL_TECPLOT_FILES | ON | OFF | Outputs Tecplot ASCII files | OFF |
GLOBAL_SUPER_FILES | ON | OFF | Outputs Tecplot ASCII files | OFF |
GLOBAL_STATISTICS | [t0] [tn] [dt] | Calculates global statistics if specified | none |
FLOW_STATISTICS | [t0] [tn] [dt] | Calculates flow statistics if specified | none |
SEDIMENT_STATISTICS | [t0] [tn] [dt] | Calculates sediment statistics if specified | none |
SALINITY_STATISTICS | [t0] [tn] [dt] | Calculates salinity statistics if specified | none |
Matrix solver
The four different solvers implemented in the implicit model are the Gauss-Seidel, Gauss-Seidel with Successive-Over-Relaxation, BICGSTAB, and GMRES. The same solver is applied to flow, sediment and salinity. The default solver is the GMRES. The solver may be changed using the advanced card in the table below.
Card | Arguments | Description | Default value |
---|---|---|---|
SOLVER_TYPE | GAUSS-SEIDEL | GAUSS-SEIDEL-SOR | BICGSTAB | GMRES | Determines the numerical solver used | GMRES |
HYDRO_MAX_ITER | integer | Maximum number of iterations (outer loop) for the hydrodynamics | 20 |
SEDIMENT_MAX_ITER | integer | Maximum number of iterations (outer loop) for the sediment transport | 20 |
SALINITY_MAX_ITER | integer | Maximum number of iterations (outer loop) for the salinity transport | 20 |
Advection scheme
As in the case of the solver, the same advection scheme is applied for the flow, sediment and salinity transport equations. There are three choices for advection schemes with upwinding in the implicit model: hybrid, exponential and HLPA. The hybrid scheme is fast but is the most diffusive. The exponential scheme is based on the 1D analytical solution to an advection-diffusion equation and produces very stable results. The HLPA is very stable and non-diffusive, but requires slightly more computational time. For most applications, the exponential scheme is recommended and is set as the default. The advection scheme may be change using the advanced card
Card | Arguments | Description | Default value |
---|---|---|---|
ADVECTION_SCHEME | HYBRID | EXPONENTIAL | HLPA | Determines the advection scheme | EXPONENTIAL |
Units of Measurement
Variable | Units | Symbol |
---|---|---|
Water Surface Elevation | meters | |
Current Velocity | meters per second | |
Flow Rate | cubic meters per second | |
Salinity Concentration | parts per thousand | |
Sediment Concentration | kilogram per meter cubed | |
Sediment Transport | meter squared per second | |
Bed Shear Stress | kilogram per meter per second squared |