Initialization parameters (class = I),
run parameters (R), package parameters (P) as well as user-defined
parameters (U) are alphabetically listed in the following table.
Parameter name |
Class |
Type |
Default
|
Explanation |
I |
L |
.F. |
Near-surface adjustment of the mixing length to the Prandtl-layer law. |
|
I |
R |
0.0 |
Inclination of the model domain with respect to the horizontal (in degrees). |
|
R |
R |
0.0 |
Averaging interval for all output of temporally averaged data (in s). |
|
R |
R |
value of averaging_ |
Averaging interval for vertical profiles output to local file DATA_1D_PR_NETCDF and/or PLOT1D_DATA (in s). |
|
P |
R |
value of averaging_ |
Averaging interval for spectra output to local file DATA_1D_SP_NETCDF and/or PLOTSP_X_DATA / PLOTSP_Y_DATA (in s). |
|
I |
C * 20 |
'neumann' |
Bottom boundary condition of the TKE. |
|
I |
C * 20 |
´cyclic´ |
Boundary condition along x (for all quantities). |
|
I |
C * 20 |
'cyclic' |
Boundary condition along y (for all quantities). |
|
I |
C * 20 |
'neumann' |
Bottom boundary condition of the perturbation pressure. |
|
I |
C * 20 |
'dirichlet' |
Top boundary condition of the perturbation pressure. |
|
P |
C*15 |
´reflect´ |
Bottom boundary condition for particle transport. |
|
P |
C*15 |
´cyclic´ |
Lateral boundary condition (x-direction) for particle transport. |
|
P |
C*15 |
´cyclic´ |
Lateral boundary condition (y-direction) for particle transport. |
|
P |
C*15 |
´absorb´ |
Top boundary condition for particle transport. |
|
I |
C * 20 |
'dirichlet' |
Bottom boundary condition of the potential temperature. |
|
I |
C * 20 |
'initial_gradient' |
Top boundary condition of the potential temperature. |
|
I |
C * 20 |
'dirichlet' |
Bottom boundary condition of the specific humidity / total water content. |
|
I |
C * 20 |
'neumann' |
Top boundary condition of the specific humidity / total water content. |
|
I |
C * 20 |
'dirichlet' |
Bottom boundary condition of the scalar concentration. |
|
I |
C * 20 |
´neumann´ |
Top boundary condition of the scalar concentration. |
|
I |
C * 20 |
'neumann' |
Top boundary condition of the salinity. |
|
I |
C * 20 |
'dirichlet' |
Bottom boundary condition of the horizontal wind components u and v. |
|
I |
C * 20 |
'dirichlet' |
Top boundary condition of the horizontal velocity components u and v. |
|
I |
R |
0.0 |
Kinematic salinity flux near the surface (in psu m/s). |
|
I |
R |
50.0 |
Height of a single building in m. |
|
I |
R |
50.0 |
Width of a single building in m. |
|
I |
R |
50.0 |
Depth of a single building in m. |
|
I |
R |
building centered in x-direction |
x-coordinate of the left building wall in m. |
|
I |
R |
building centered in y-direction |
y-coordinate of the South building wall in m. |
|
R |
L |
.T.. |
Switch to steer the call of the pressure solver. |
|
I |
C * 20 |
'block' |
Canopy mode |
|
I |
R |
50.0 |
Street canyon height in m. |
|
I |
R |
9999999.9 |
Street canyon width in x-direction in m. |
|
I |
R |
9999999.9 |
Street canyon width in y-direction in m. |
|
I |
R |
canyon centered in x-direction |
x-coordinate of the left canyon wall in m. |
|
I |
R |
canyon centered in y-direction |
y-coordinate of the South canyon wall in m. |
|
R |
R |
0.1, 0.8 or 0.9 (see parameter description) |
Time step limiting factor. |
|
P |
R |
0.0 |
Left boundary of the displayed domain (in m). |
|
P |
R |
(ny+1)*dy |
North boundary of the displayed domain (in m). |
|
P |
R |
(nx+1)*dx |
Right boundary of the displayed domain (in m). |
|
P |
R |
0.0 |
South boundary of the displayed domain (in m). |
|
I |
L |
.F. |
Parameter to switch on usage of cloud droplets. |
|
I |
L |
.F. |
Parameter to switch on the condensation scheme. |
|
P |
I |
1 |
Vertex cluster size for polygon reduction of topography. |
|
P |
R(2) |
0.0, 1.0 |
Interval of values used for determining the particle color displayed in the animation. |
|
P |
I (100) |
no level |
Vertical level for which horizontal spectra are to be calculated and output (gridpoints). |
|
I |
L |
.F. |
Conservation of volume flow in x- and y-direction. |
|
I |
C * 16 |
'default' |
Modus of volume flow conservation. |
|
I |
R |
0.0 |
Simulation time of a precursor run. |
|
R |
L |
.T. |
Switch to impose random perturbations to the horizontal velocity field. |
|
R |
C * 10 (100) |
100 * ' ' |
Type of normalization applied to the x-coordinate of vertical profiles to be plotted with profil. |
|
R |
C * 10 |
100 * ' ' |
Type of normalization applied to the y-coordinate of vertical profiles to be plotted with profil. |
|
R |
C * 100 (100) |
see parameter description |
Determines which vertical profiles are to be presented in which coordinate system if the plot software profil is used. |
|
R |
C * 40 |
see parameter description |
x-axis labels of vertical profile coordinate systems to be plotted with profil. |
|
R |
R |
0.0 |
Average heat flux that is prescribed at the top of the plant canopy (in K m/s). |
|
I |
L |
.T. |
Cut off of so-called overshoots, which can occur with the upstream-spline-scheme. |
|
R |
C * 1 |
'w' |
Type of cycle to be used with the multi-grid method. |
|
I |
R |
zu(nz+1) |
Height where the damping layer begins in the 1d-model (in m). |
|
R |
C * 10 (100) |
100 * ´ ´ |
Quantities for which 2d cross section and/or 3d volume data are to be output. |
|
R |
C * 10 (10) |
'netcdf' |
Format of output data. |
|
R |
C * 10 (100) |
100 * ' ' |
Quantities for which vertical profiles (horizontally averaged) are to be output. |
|
U |
C * 10 |
200 * ' ' |
User defined quantities for which horizontally averaged profile data is to be output. |
|
P |
C * 10 (10) |
10 * ' ' |
Quantities for which horizontal spectra are to be calculated and output. |
|
U |
C * 10 (100) |
100 * ' ' |
User defined quantities for which 2d cross section and/or 3d volume data are to be output. |
|
R |
L |
.T. |
Output 2d cross section data by one or all processors. |
|
P |
R (10) |
0.0, 9 * 9999999.9 |
Ratio of the density of the fluid and the density of the particles. |
|
I |
C * 20 |
'as_in_3d_model' |
Calculation method for the energy dissipation term in the TKE equation of the 1d-model. |
|
R |
R |
0.25 |
Maximum perturbation amplitude of the random perturbations imposed to the horizontal velocity field (in m/s). |
|
R |
R |
0.01 |
Upper limit value of the perturbation energy of the velocity field used as a criterion for imposing random perturbations (in m2/s2). |
|
R |
R |
zu(3) or zu(nz*2/3) |
Lower limit of the vertical range for which random perturbations are to be imposed on the horizontal wind field (in m). |
|
R |
R |
zu(nz/3) or zu(nzt-3) |
Upper limit of the vertical range for which random perturbations are to be imposed on the horizontal wind field (in m). |
|
R |
L |
.F. |
Output 2d cross section data by one or all processors. |
|
R |
L |
.F. |
Output of 3d volume data at the beginning of a run. |
|
R |
L |
.F. |
Output of data for 3d plots in compressed form. |
|
R |
C * 7 (100) |
see parameter description |
Significant digits in case of compressed data output. |
|
R |
L |
.F. |
External pressure gradient switch. |
|
R |
L |
.F. |
Vertically smooth the external pressure gradient using a sinusoidal smoothing function. |
|
R |
R |
0.0 |
Lower limit of the vertical range for which the external pressure gradient is applied (in m). |
|
R |
R (2) |
2 * 0.0 |
Values of the external pressure gradient applied in x- and y-direction, respectively (in Pa/m). |
|
I |
R |
0.0 |
Drag coefficient used in the plant canopy model. |
|
I/R |
R |
variable |
Time step for the 3d-model (in s). |
|
R |
R |
0.0 |
Temporal interval of data which are subject to temporal averaging (in s). |
|
R |
R |
value of dt_ |
Temporal interval of data which are subject to temporal averaging of vertical profiles and/or spectra (in s). |
|
R |
R |
9999999.9 |
Temporal interval for the data exchange in case of runs with coupled models (e.g. atmosphere - ocean) (in s). |
|
R |
R |
9999999.9 |
Temporal interval at which data (3d volume data (instantaneous or time averaged), cross sections (instantaneous or time averaged), vertical profiles, spectra) shall be output (in s). |
|
R |
R |
value of dt_data_ |
Temporal interval at which time averaged 3d volume data and/or 2d cross section data shall be output (in s). |
|
R |
R |
9999999.9 |
Temporal interval at which random perturbations are to be imposed on the horizontal velocity field (in s). |
|
R |
R |
value of dt_data_ |
Temporal interval at which data of vertical profiles shall be output (to local file DATA_1D_PR_NETCDF or/and PLOT1D_DATA) (in s). |
|
R |
R |
9999999.9 |
Temporal interval at which data of vertical profiles shall be output (output for printouts, local file LIST_PROFIL) (in s). |
|
P |
R |
value of dt_data_ |
Temporal interval at which time series data of particle quantities shall be output (in s). |
|
P |
R |
value of dt_data_ |
Temporal interval at which spectra data shall be output (in s). |
|
R |
R |
see parameter description |
Temporal interval at which time series data shall be output (in s). |
|
R |
R |
value of dt_data_ |
Temporal interval at which horizontal cross section data shall be output (in s). |
|
R |
R |
value of dt_data_ |
Temporal interval at which vertical cross section data (xz) shall be output (in s). |
|
R |
R |
value of dt_data_ |
Temporal interval at which vertical cross section data (yz) shall be output (in s). |
|
R |
R |
value of dt_data_ |
Temporal interval at which 3d volume data shall be output (in s). |
|
P |
R |
9999999.9 |
Temporal interval of scenes to be displayed with the dvrp software (in s). |
|
R |
R |
20.0 |
Maximum allowed value of the timestep (in s). |
|
P |
R |
0.0002 |
Minimum value for the particle timestep when SGS velocities are used (in s). |
|
P |
R |
9999999.9 |
Temporal interval at which particles are to be released from a particle source (in s). |
|
I |
R |
9999999.9 |
Temporal interval of vertical profile output of the 1D-model (in s). |
|
R |
R |
9999999.9 |
Temporal interval at which a new restart run is to be carried out (in s). |
|
R |
R |
60.0 |
Temporal interval at which run control output is to be made (in s). |
|
I |
R |
60.0 |
Temporal interval of runtime control output of the 1d-model (in s). |
|
P |
R |
0.0 |
Temporal interval for sorting particles (in s). |
|
P |
R |
9999999.9 |
Temporal interval for output of particle data (in s). |
|
P |
C * 80 |
'default' |
Name of the directory into which data created by the dvrp software shall be saved. |
|
P |
C * 80 |
'default' |
Name of the file into which data created by the dvrp software shall be output. |
|
P |
C * 80 |
'origin.rvs. |
Name of the computer to which data created by the dvrp software shall be transferred. |
|
P |
C * 10 |
'rtsp' |
Output mode for the dvrp software. |
|
P |
C * 80 |
'********' |
Password for the computer to which data created by the dvrp software is to be transferred. |
|
P |
R |
0.2 * dx |
Diameter that the particles is given in visualizations with the dvrp software (in m). |
|
P |
R(2) |
0.0, 1.0 |
Interval of values used for determining the particle size displayed in the animation. |
|
P |
C * 80 |
no default value |
User name of a valid account on the computer to which data created by the dvrp software is to be transferred. |
|
I |
R |
1.0 |
Horizontal grid spacing along the x-direction (in m). |
|
I |
R |
1.0 |
Horizontal grid spacing along the y-direction (in m). |
|
I |
R |
no default, see parameter description |
Vertical grid spacing (in m). |
|
I |
R |
9999999.9 |
Allowed maximum vertical grid spacing (in m). |
|
I |
R |
1.08 |
Stretch factor for a vertically stretched grid (see dz_stretch_level). |
|
I |
R |
100000.0 |
Height level above/below which the grid is to be stretched vertically (in m). |
|
I |
R |
0.0 |
Initial TKE in m2s-2. |
|
I |
R |
0.0 |
Minimum TKE in m2s-2. |
|
R |
R |
0.0 |
Simulation time of the 3D model (in s). |
|
P |
R |
9999999.9 |
Time of the last release of particles (in s). |
|
I |
R |
864000.0 |
Time to be simulated for the 1D-model (in s). |
|
I |
C * 20 |
'system specific' |
FFT-method to be used. |
|
R |
L |
.F. |
Steering of header output to the local file RUN_CONTROL. |
|
I |
L |
.F. |
Application of a Galilei-transformation to the coordinate system of the model. |
|
I |
C * 6 |
'strict' |
Variable to adjust the subdomain sizes in parallel runs. |
|
P |
R(3) |
0.0, 0.6, 0.0 |
Color of the ground plate |
|
I |
L |
.F. |
Parameter to switch on the prognostic equation for specific humidity q. |
|
I |
R |
from precursor run |
Height below which the turbulence signal is used for turbulence recycling (in m). |
|
I |
R |
0.1 * inflow_damping_height |
Transition range within which the turbulance signal is damped to zero (in m). |
|
I |
I |
MIN(10, |
Lower limit of the horizontal range for which random perturbations are to be imposed on the horizontal velocity field (gridpoints). |
|
I |
I |
MIN(100, |
Upper limit of the horizontal range for which random perturbations are to be imposed on the horizontal velocity field (gridpoints). |
|
I |
C * 100 |
no default, see parameter description |
Initialization actions to be carried out. |
|
P |
R |
1.0 |
Factor to define the real number of initial droplets in a grid cell. |
|
P |
R(3,10) |
0.9, 0.9, 0.9 |
Color of the isosurface(s). |
|
I |
R |
variable (computed from TKE) |
Constant eddy diffusivities are used (laminar simulations). |
|
I |
R |
0.5*(dx or dy) |
Maximum diffusivity used for filtering the velocity field in the vicinity of the outflow (in m2/s). |
|
I |
R |
0.0 |
Surface value of the leaf area density (in m2/m3) |
|
I |
R (10) |
10 * 0.0 |
Gradient(s) of the leaf area density (in m2/m4) |
|
I |
R (10) |
10 * 0.0 |
Height level from which on the gradient of the leaf area density defined by lad_vertical_gradient_level is effective (in m). |
|
R |
R |
0.0 |
Concentration of a passive scalar at the surface of a leaf (in kg/m3). |
|
I |
R |
0.0 |
Filter factor for the so-called Long-filter. |
|
I |
C * 16 |
see parameter description |
Method used to optimize loops for solving the prognostic equations . |
|
P |
I |
1000 |
Maximum number of particles (on a PE). |
|
P |
I |
100 |
Maximum number of tailpoints that a particle tail can have. |
|
P |
R |
100000.0 |
Maximum age that the end point of a particle tail is allowed to have (in s). |
|
R |
I |
- 1 |
Number of cycles to be used with the multi-grid scheme. |
|
R |
I |
see parameter description |
Grid level at which data shall be gathered on PE0. |
|
P |
R |
0.0 |
Minimum distance allowed between two adjacent points of a particle tail (in m). |
|
I |
C * 20 |
'as_in_3d_model' |
Mixing length used in the 1d-model. |
|
P |
C * 20 (10) |
10 * ' ' |
Graphical objects (isosurfaces, slicers, particles) which are to be created by the dvrp software. |
|
I |
C * 10 |
'pw-scheme' |
Advection scheme to be used for the momentum equations. |
|
I |
C * 20 (10) |
single precision for all |
Defines the accuracy of the NetCDF output. |
|
R |
L |
.F. |
All NetCDF files - except those containing 3d volume data - will have 64 bit offset format. |
|
R |
L |
.T. |
NetCDF files containing 3d volume data will have 64 bit offset format. |
|
R |
I |
2 |
Grid level at which data shall be gathered on PE0. |
|
R |
I |
0 |
Determines the subdomain from which the normalization quantities are calculated. |
|
R |
I |
no default, see parameter description |
Number of processors along x-direction of the virtual processor net. |
|
R |
I |
no default, see parameter description |
Number of processors along y-direction of the virtual processor net. |
|
R |
I |
20 |
Number of iterations to be used with the SOR-scheme. |
|
I |
I |
100 |
Initial number of iterations with the SOR algorithm |
|
P |
I |
1 |
Number of particle groups to be used. |
|
I |
I |
no default, see parameter description |
Number of grid points in x-direction. |
|
I |
I |
no default, see parameter description |
Number of grid points in y-direction. |
|
I |
I |
no default, see parameter description |
Number of grid points in z-direction. |
|
R |
I |
nz+1 |
Limits the output of 3d volume data along the vertical direction (grid point index k). |
|
I |
L |
.F. |
Parameter to switch on ocean runs. |
|
I |
R |
7.29212E-5 |
Angular velocity of the rotating system (in rad s-1). |
|
R |
R |
1.8 |
Convergence factor to be used with the the SOR-scheme. |
|
I |
I |
MIN(20, nx/2 or ny/2) |
Width of the damping range in the vicinity of the outflow (gridpoints). |
|
I |
R |
0.0 |
Allowed limit for the overshooting of subgrid-scale TKE in case that the upstream-spline scheme is switched on (in m2/s2). |
|
I |
R |
0.0 |
Allowed limit for the overshooting of potential temperature in case that the upstream-spline scheme is switched on (in K). |
|
I |
R |
0.0 |
Allowed limit for the overshooting of the u-component of velocity in case that the upstream-spline scheme is switched on (in m/s). |
|
I |
R |
0.0 |
Allowed limit for the overshooting of the v-component of velocity in case that the upstream-spline scheme is switched on (in m/s). |
|
I |
R |
0.0 |
Allowed limit for the overshooting of the w-component of velocity in case that the upstream-spline scheme is switched on (in m/s). |
|
P |
I |
1 |
Number of particles to be started per point. |
|
P |
R |
0.0 |
Time of the first release of particles (in s). |
|
P |
C*10 |
'none' |
Parameter, which allows to bind the displayed particle color to certain flow quantities. |
|
P |
C*10 |
'none' |
Parameter, which allows to bind the displayed particle size to certain flow quantities. |
|
P |
R |
9999999.9 |
Maximum allowed age of particles (in s). |
|
I |
L |
.F. |
Parameter to switch on the prognostic equation for a passive scalar. |
|
I |
I |
0 |
Grid point index (scalar) of the upper boundary of the plant canopy layer |
|
P |
R (10) |
10 * dx |
Distance along x between particles within a particle source (in m). |
|
P |
R (10) |
10 * dy |
Distance along y between particles within a particle source (in m). |
|
P |
R (10) |
10 * ( zu(2) - zu(1) ) |
Distance along z between particles within a particle source (in m). |
|
I |
R |
55.0 |
Geographical latitude (in degrees). |
|
I |
L |
.F. |
Parameter to switch on the plant canopy model |
|
P |
I (100) |
No level |
Vertical level(s) for which horizontal spectra are to be plotted (in gridpoints). |
|
I |
L |
.T. |
Parameter to switch on a Prandtl layer. |
|
R |
R |
1.0 |
Ratio of the eddy diffusivities for momentum and heat (Km/Kh). |
|
I |
L |
.F. |
Parameter to switch on the precipitation scheme. |
|
R |
R |
value of dt_do2d_ |
Temporal interval for which the precipitation amount (in mm) shall be calculated and output (in s). |
|
R |
I |
3 |
Number of coordinate systems to be plotted in one row by profil. |
|
R |
I |
2 |
Number of rows of coordinate systems to be plotted on one page by profil. |
|
P |
R (10) |
10 * zu(nz/2) |
Bottom edge of a particle source (in m). |
|
P |
R (10) |
10 * 0.0 |
Left edge of a particle source (in m). |
|
P |
R (10) |
10 * ( ny * dy ) |
Rear (“north”) edge of a particle source (in m). |
|
R |
C * 10 |
'poisfft' |
Scheme to be used to solve the Poisson equation for the perturbation pressure. |
|
P |
R (10) |
10 * ( nx * dx ) |
Right edge of a particle source (in m). |
|
P |
R (10) |
10 * 0.0 |
Front (“south”) edge of a particle source (in m). |
|
P |
R (10) |
10 * zu(nz/2) |
Top edge of a particle source (in m). |
|
I |
R |
use horizontal average as reference |
Reference temperature to be used in all buoyancy terms (in K). |
|
I |
R |
300.0 |
Surface potential temperature (in K). |
|
I |
R |
0.0 |
Change in surface temperature to be made at the beginning of the 3d run (in K). |
|
I |
R (10) |
10 * 0.0 |
Temperature gradient(s) of the initial temperature profile (in K / 100 m). |
|
I |
R (10) |
10 * 0.0 |
Height level from which on the temperature gradient defined by pt_vertical_gradient is effective (in m). |
|
I |
R |
0.0 |
Surface specific humidity / total water content (kg/kg). |
|
I |
R |
0.0 |
Change in surface specific humidity / total water content to be made at the beginning of the 3d run (kg/kg). |
|
I |
R (10) |
10 * 0.0 |
Humidity gradient(s) of the initial humidity profile (in 1/100 m). |
|
I |
R (10) |
10 * 0.0 |
Height level from which on the humidity gradient defined by q_vertical_gradient is effective (in m). |
|
I |
L |
.F. |
Parameter to switch on longwave radiation cooling at cloud-tops. |
|
P |
R (10) |
0.0, 9* |
Particle radius (in m). |
|
I |
C * 20 |
'numerical recipes' |
Random number generator to be used for creating uniformly distributed random numbers. |
|
I |
L |
.F. |
Parameter to impose random perturbations on the internal two-dimensional near surface heat flux field shf. |
|
P |
L |
.F. |
Initial position of the particles is varied randomly within certain limits. |
|
R |
R |
0.0 and/or 0.01 (see parameter description) |
Factor for Rayleigh damping. |
|
R |
R |
2/3 * zu(nz) |
Height where the Rayleigh damping starts (in m). |
|
P |
L |
.T. |
Read particle data from the previous run. |
|
I |
R |
Distance of the recycling plane from the inflow boundary (in m). |
||
U |
C * 40 (0:9) |
|
Name(s) of the subdomain(s) defined by the user. |
|
R |
R |
1.0E-6 |
Largest residual permitted for the multi-grid scheme (in s-2m-3). |
|
R |
R |
9999999.9 |
Simulated time after which a restart run is to be carried out (in s). |
|
I |
R |
1.0 |
Upper limit of the flux-Richardson number. |
|
I |
R |
- 5.0 |
Lower limit of the flux-Richardson number. |
|
I |
R |
0.1 |
Roughness length (in m). |
|
I |
R |
35.0 |
Surface salinity (in psu). |
|
I |
R(10) |
10 * 0.0 |
Salinity gradient(s) of the initial salinity profile (in psu / 100 m). |
|
I |
R(10) |
10 * 0.0 |
Height level from which on the salinity gradient defined by sa_vertical_gradient is effective (in m). |
|
I |
C * 10 |
'pw-scheme' |
Advection scheme to be used for the scalar quantities. |
|
R |
R |
0.0 |
Scalar exchange coefficient for a leaf (dimensionless). |
|
R |
I (100) |
no section |
Position of cross section(s) for output of 2d horizontal cross sections (grid point index k). |
|
R |
I (100) |
no section |
Position of cross section(s) for output of 2d (xz) vertical cross sections (grid point index j). |
|
R |
I (100) |
no section |
Position of cross section(s) for output of 2d (yz) vertical cross sections (grid point index i). |
|
P |
I |
100 |
Limit the number of particle tails. |
|
R |
R |
0.0 |
No data output before this interval has passed (in s). |
|
R |
R |
value of skip_time_ |
No output of temporally averaged 2d/3d data before this interval has passed (in s). |
|
R |
R |
value of skip_time_ |
No output of vertical profile data before this interval has passed (in s). |
|
P |
R |
value of skip_time_ |
No output of spectra data before this interval has passed (in s). |
|
R |
R |
value of skip_time_ |
No output of instantaneous horizontal cross section data before this interval has passed (in s). |
|
R |
R |
value of skip_time_ |
No output of instantaneous vertical (xz) cross section data before this interval has passed (in s). |
|
R |
R |
value of skip_time_ |
No output of instantaneous vertical (yz) cross section data before this interval has passed (in s). |
|
R |
R |
value of skip_time_ |
No output of instantaneous 3d volume data before this interval has passed (in s). |
|
P |
R(2,10) |
10 * (-1,1) |
Ranges of values to which a color table has to be mapped (units of the respective quantity). |
|
P |
C * 2 (10) |
10 * ' ' |
Direction(s) along which spectra are to be calculated. |
|
I |
I |
0 |
Number of additional user-defined subdomains for which statistical analysis and corresponding output (profiles, time series) shall be made. |
|
P |
R |
1.0 |
Superelevation factor for the vertical coordinate. |
|
P |
R |
1.0 |
Superelevation factor for the horizontal (x) coordinate. |
|
P |
R |
1.0 |
Superelevation factor for the horizontal (y) coordinate. |
|
I |
R |
no prescribed heatflux |
Kinematic sensible heat flux at the bottom surface (in K m/s). |
|
I |
R |
1013.25 |
Atmospheric pressure at the surface (in hPa) |
|
I |
R |
0.0 |
Scalar flux at the surface (in kg/(m2 s)). |
|
I |
R |
0.0 |
Kinematic water flux near the surface (in m/s). |
|
I |
R |
0.0 |
Surface value of the passive scalar (in kg/m3). |
|
I |
R |
0.0 |
Change in surface scalar concentration to be made at the beginning of the 3d run (in kg/m3). |
|
I |
R(10) |
10 * 0.0 |
Scalar concentration gradient(s) of the initial scalar concentration profile (in kg/m3 / 100 m). |
|
I |
R(10) |
10 * 0.0 |
Height level from which on the scalar gradient defined by s_vertical_gradient is effective (in m). |
|
R |
R |
35.0 |
CPU time needed for terminal actions at the end of a run in batch mode (in s). |
|
P |
R (10) |
0.0 |
Threshold value for which an isosurface is to be created by the dvrp software. |
|
I |
C * 20 |
'runge-kutta-3' |
Time step scheme to be used for integration of the prognostic variables. |
|
I |
C * 40 |
'flat' |
Topography mode. |
|
P |
R(3) |
0.8, 0.7, 0.6 |
Color of the topography. |
|
I |
C * 11 |
default depends on value of topography; see text for details |
Convention for defining the topography grid. |
|
I |
R |
no prescribed heatflux |
Kinematic sensible heat flux at the top surface (in K m/s). |
|
I |
R |
no prescribed momentumflux |
Momentum flux along x at the top boundary (in m2/s2). |
|
I |
R |
no prescribed momentumflux |
Momentum flux along y at the top boundary (in m2/s2). |
|
I |
R |
no prescribed |
Kinematic salinity flux at the top boundary, i.e. the sea surface (in psu m/s). |
|
I |
L |
.F. |
Generates a turbulent inflow at side boundaries using a turbulence recycling method. |
|
I |
R |
0.0 |
u-component of the predefined bulk velocity (in m/s). |
|
I |
R |
0.0 |
u-component of the geostrophic wind at the surface (in m/s). |
|
I |
R(10) |
10 * 0.0 |
Gradient(s) of the initial profile of the u-component of the geostrophic wind (in 1/100s). |
|
I |
R(10) |
10 * 0.0 |
Height level from which on the gradient defined by ug_vertical_gradient is effective (in m). |
|
I |
R |
0.0 |
Subgrid-scale turbulent kinetic energy difference used as criterion for applying the upstream scheme when upstream-spline advection is switched on (in m2/s2). |
|
I |
R |
0.0 |
Temperature difference used as criterion for applying the upstream scheme when upstream-spline advection is switched on (in K). |
|
I |
R |
0.0 |
Velocity difference (u-component) used as criterion for applying the upstream scheme when upstream-spline advection is switched on (in m/s). |
|
I |
R |
0.0 |
Velocity difference (v-component) used as criterion for applying the upstream scheme when upstream-spline advection is switched on (in m/s). |
|
I |
R |
0.0 |
Velocity difference (w-component) used as criterion for applying the upstream scheme when upstream-spline advection is switched on (in m/s). |
|
P |
L |
.F. |
Give particles a tail. |
|
R |
L |
.F. |
Additional plot of vertical profile data with profil from preceding runs of the job chain. |
|
P |
L |
.F. |
Use subgrid-scale velocities for particle advection. |
|
I |
L |
.F. |
Parameter to steer the treatment of the subgrid-scale vertical fluxes within the diffusion terms at k=1 (bottom boundary). |
|
I |
L |
.F. |
Parameter to steer the treatment of the subgrid-scale vertical fluxes within the diffusion terms at k=nz (top boundary). |
|
I |
L |
.T. |
Switch to determine the translation velocity in case that a Galilean transformation is used. |
|
I |
L |
.F. |
Parameter to choose the advection/timestep scheme to be used for the subgrid-scale TKE. |
|
P |
L |
.T. |
Switch on/off vertical particle transport. |
|
I |
R |
0.0 |
v-component of the predefined bulk velocity (in m/s). |
|
I |
R |
0.0 |
v-component of the geostrophic wind at the surface (in m/s). |
|
I |
R(10) |
10 * 0.0 |
Gradient(s) of the initial profile of the v-component of the geostrophic wind (in 1/100s). |
|
I |
R(10) |
10 * 0.0 |
Height level from which on the gradient defined by vg_vertical_gradient is effective (in m). |
|
I |
L |
.T. |
Parameter to restrict the mixing length in the vicinity of the bottom boundary (and near vertical walls of a non-flat topography). |
|
I |
R(5) |
5 * 0.0 |
Prescribed kinematic sensible heat flux in K m/s at the five topography faces. |
|
P |
L |
.F. |
Switch on/off output of particle informations. |
|
R |
R |
zu(nzt+1) (model top) |
Height level up to which horizontally averaged profiles are to be plotted with profil (in m). |
|
R |
R |
determined by plot |
Normalized height level up to which horizontally averaged profiles are to be plotted with profil. |
|
R |
R |
zu(nz) |
Height level up to which 2d cross sections are to be plotted with iso2d (in m). |
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