| | 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> |