| 239 | }}} |
| 240 | |---------------- |
| 241 | {{{#!td style="vertical-align:top" |
| 242 | [=#cycle_mg '''cycle_mg'''] |
| 243 | }}} |
| 244 | {{{#!td style="vertical-align:top" |
| 245 | C*1 |
| 246 | }}} |
| 247 | {{{#!td style="vertical-align:top" |
| 248 | 'w' |
| 249 | }}} |
| 250 | {{{#!td |
| 251 | Type of cycle to be used with the multi-grid method.\\\\ |
| 252 | This parameter determines which type of cycle is applied in the multi-grid method used for solving the Poisson equation for perturbation pressure (see [#psolver psolver]). It defines in which way it is switched between the fine and coarse grids. So-called v- and w-cycles are realized (i.e. '''cycle_m'''g may be assigned the values '' 'v' '' or '' 'w' ''). The computational cost of w-cycles is much higher than that of v-cycles, however, w-cycles give a much better convergence. |
| 253 | }}} |
| 254 | |---------------- |
| 255 | {{{#!td style="vertical-align:top" |
| 256 | [=#<insert_parameter_name> '''<insert_parameter_name>'''] |
| 257 | }}} |
| 258 | {{{#!td style="vertical-align:top" |
| 259 | <insert type> |
| 260 | }}} |
| 261 | {{{#!td style="vertical-align:top" |
| 262 | <insert value> |
| 263 | }}} |
| 264 | {{{#!td |
| 265 | <insert explanation> |
| 266 | }}} |
| 267 | |---------------- |
| 268 | {{{#!td style="vertical-align:top" |
| 269 | [=#<insert_parameter_name> '''<insert_parameter_name>'''] |
| 270 | }}} |
| 271 | {{{#!td style="vertical-align:top" |
| 272 | <insert type> |
| 273 | }}} |
| 274 | {{{#!td style="vertical-align:top" |
| 275 | <insert value> |
| 276 | }}} |
| 277 | {{{#!td |
| 278 | <insert explanation> |
| 279 | }}} |
| 280 | |---------------- |
| 281 | {{{#!td style="vertical-align:top" |
| 282 | [=#<insert_parameter_name> '''<insert_parameter_name>'''] |
| 283 | }}} |
| 284 | {{{#!td style="vertical-align:top" |
| 285 | <insert type> |
| 286 | }}} |
| 287 | {{{#!td style="vertical-align:top" |
| 288 | <insert value> |
| 289 | }}} |
| 290 | {{{#!td |
| 291 | <insert explanation> |
| 292 | }}} |
| 293 | |---------------- |
| 294 | {{{#!td style="vertical-align:top" |
| 295 | [=#<insert_parameter_name> '''<insert_parameter_name>'''] |
| 296 | }}} |
| 297 | {{{#!td style="vertical-align:top" |
| 298 | <insert type> |
| 299 | }}} |
| 300 | {{{#!td style="vertical-align:top" |
| 301 | <insert value> |
| 302 | }}} |
| 303 | {{{#!td |
| 304 | <insert explanation> |
546 | | {{{#!td style="vertical-align:top; text-align:left;width: 150px" |
547 | | [=# ''''''] |
548 | | }}} |
549 | | {{{#!td style="vertical-align:top; text-align:left;style="width: 50px" |
550 | | |
551 | | }}} |
552 | | {{{#!td style="vertical-align:top; text-align:left;style="width: 100px" |
553 | | |
554 | | }}} |
555 | | {{{#!td |
556 | | |
| 599 | {{{#!td style="vertical-align:top;width: 150px" |
| 600 | [=#damp_level_1d '''damp_level_1d'''] |
| 601 | }}} |
| 602 | {{{#!td style="vertical-align:top;width: 50px" |
| 603 | R |
| 604 | }}} |
| 605 | {{{#!td style="vertical-align:top;width: 100px" |
| 606 | zu(nz+1) |
| 607 | }}} |
| 608 | {{{#!td |
| 609 | Height where the damping layer begins in the [[1d-model]] (in m).\\\\ |
| 610 | This parameter is used to switch on a damping layer for the 1d-model, which is generally needed for the damping of inertia oscillations. Damping is done by gradually increasing the value of the eddy diffusivities about 10% per vertical grid level (starting with the value at the height given by '''damp_level_1d''', or possibly from the next grid pint above), i.e. K,,m,,(k+1) = 1.1 * K,,m,,(k). The values of K,,m,, are limited to 10 m^2^/s at maximum.\\\\ |
| 611 | This parameter only comes into effect if the 1d-model is switched on for the initialization of the 3d-model using [#initializing_actions initializing_actions] = '' 'set_1d-model_profiles'.'' |
| 863 | }}} |
| 864 | |---------------- |
| 865 | {{{#!td style="vertical-align:top" |
| 866 | [=#<insert_parameter_name> '''<insert_parameter_name>'''] |
| 867 | }}} |
| 868 | {{{#!td style="vertical-align:top" |
| 869 | <insert type> |
| 870 | }}} |
| 871 | {{{#!td style="vertical-align:top" |
| 872 | <insert value> |
| 873 | }}} |
| 874 | {{{#!td |
| 875 | <insert explanation> |
| 876 | }}} |
| 877 | |---------------- |
| 878 | {{{#!td style="vertical-align:top" |
| 879 | [=#<insert_parameter_name> '''<insert_parameter_name>'''] |
| 880 | }}} |
| 881 | {{{#!td style="vertical-align:top" |
| 882 | <insert type> |
| 883 | }}} |
| 884 | {{{#!td style="vertical-align:top" |
| 885 | <insert value> |
| 886 | }}} |
| 887 | {{{#!td |
| 888 | <insert explanation> |
| 889 | }}} |
| 890 | |---------------- |
| 891 | {{{#!td style="vertical-align:top" |
| 892 | [=#<insert_parameter_name> '''<insert_parameter_name>'''] |
| 893 | }}} |
| 894 | {{{#!td style="vertical-align:top" |
| 895 | <insert type> |
| 896 | }}} |
| 897 | {{{#!td style="vertical-align:top" |
| 898 | <insert value> |
| 899 | }}} |
| 900 | {{{#!td |
| 901 | <insert explanation> |
| 902 | }}} |
| 903 | |---------------- |
| 904 | {{{#!td style="vertical-align:top" |
| 905 | [=#<insert_parameter_name> '''<insert_parameter_name>'''] |
| 906 | }}} |
| 907 | {{{#!td style="vertical-align:top" |
| 908 | <insert type> |
| 909 | }}} |
| 910 | {{{#!td style="vertical-align:top" |
| 911 | <insert value> |
| 912 | }}} |
| 913 | {{{#!td |
| 914 | <insert explanation> |
| 915 | }}} |
| 916 | |---------------- |
| 917 | {{{#!td style="vertical-align:top" |
| 918 | [=#<insert_parameter_name> '''<insert_parameter_name>'''] |
| 919 | }}} |
| 920 | {{{#!td style="vertical-align:top" |
| 921 | <insert type> |
| 922 | }}} |
| 923 | {{{#!td style="vertical-align:top" |
| 924 | <insert value> |
| 925 | }}} |
| 926 | {{{#!td |
| 927 | <insert explanation> |