344 | | [=#u_bulk '''u_bulk'''] |
345 | | }}} |
346 | | {{{#!td style="vertical-align:top" |
347 | | R |
348 | | }}} |
349 | | {{{#!td style="vertical-align:top" |
350 | | 0.0 |
351 | | }}} |
352 | | {{{#!td |
353 | | u-component of the predefined bulk velocity (in m/s).\\\\ |
354 | | This parameter comes into effect if [#conserve_volume_flow conserve_volume_flow] = ''.T.'' and [#conserve_volume_flow_mode conserve_volume_flow_mode] = '' 'bulk_velocity'.'' |
355 | | }}} |
356 | | |---------------- |
357 | | {{{#!td style="vertical-align:top" |
358 | | [=#use_ug_for_galilei_tr '''use_ug_for_galilei_tr'''] |
359 | | }}} |
360 | | {{{#!td style="vertical-align:top" |
361 | | L |
362 | | }}} |
363 | | {{{#!td style="vertical-align:top" |
364 | | .T. |
365 | | }}} |
366 | | {{{#!td |
367 | | Switch to determine the translation velocity in case that a Galilean transformation is used.\\\\ |
368 | | In case of a Galilean transformation (see [#galilei_transformation galilei_transformation]), '''use_ug_for_galilei_tr''' = ''.T.'' ensures that the coordinate system is translated with the geostrophic windspeed.\\\\ |
369 | | Alternatively, with '''use_ug_for_galilei_tr''' = ''.F.,'' the geostrophic wind can be replaced as translation speed by the (volume) averaged velocity. However, in this case the user must be aware of fast growing gravity waves, so this choice is usually not recommended! |
370 | | }}} |
371 | | |---------------- |
372 | | {{{#!td style="vertical-align:top" |
373 | | [=#v_bulk '''v_bulk'''] |
374 | | }}} |
375 | | {{{#!td style="vertical-align:top" |
376 | | R |
377 | | }}} |
378 | | {{{#!td style="vertical-align:top" |
379 | | 0.0 |
380 | | }}} |
381 | | {{{#!td |
382 | | v-component of the predefined bulk velocity (in m/s).\\\\ |
383 | | This parameter comes into effect if [#conserve_volume_flow conserve_volume_flow] = ''.T.'' and [#conserve_volume_flow_mode conserve_volume_flow_mode] = '' 'bulk_velocity'.'' |
384 | | }}} |
385 | | |---------------- |
386 | | {{{#!td style="vertical-align:top" |
| 376 | }}} |
| 377 | |---------------- |
| 378 | {{{#!td style="vertical-align:top" |
| 379 | [=#u_bulk '''u_bulk'''] |
| 380 | }}} |
| 381 | {{{#!td style="vertical-align:top" |
| 382 | R |
| 383 | }}} |
| 384 | {{{#!td style="vertical-align:top" |
| 385 | 0.0 |
| 386 | }}} |
| 387 | {{{#!td |
| 388 | u-component of the predefined bulk velocity (in m/s).\\\\ |
| 389 | This parameter comes into effect if [#conserve_volume_flow conserve_volume_flow] = ''.T.'' and [#conserve_volume_flow_mode conserve_volume_flow_mode] = '' 'bulk_velocity'.'' |
| 390 | }}} |
| 391 | |---------------- |
| 392 | {{{#!td style="vertical-align:top" |
| 393 | [=#use_ug_for_galilei_tr '''use_ug_for_galilei_tr'''] |
| 394 | }}} |
| 395 | {{{#!td style="vertical-align:top" |
| 396 | L |
| 397 | }}} |
| 398 | {{{#!td style="vertical-align:top" |
| 399 | .T. |
| 400 | }}} |
| 401 | {{{#!td |
| 402 | Switch to determine the translation velocity in case that a Galilean transformation is used.\\\\ |
| 403 | In case of a Galilean transformation (see [#galilei_transformation galilei_transformation]), '''use_ug_for_galilei_tr''' = ''.T.'' ensures that the coordinate system is translated with the geostrophic windspeed.\\\\ |
| 404 | Alternatively, with '''use_ug_for_galilei_tr''' = ''.F.,'' the geostrophic wind can be replaced as translation speed by the (volume) averaged velocity. However, in this case the user must be aware of fast growing gravity waves, so this choice is usually not recommended! |
| 405 | }}} |
| 406 | |---------------- |
| 407 | {{{#!td style="vertical-align:top" |
| 408 | [=#v_bulk '''v_bulk'''] |
| 409 | }}} |
| 410 | {{{#!td style="vertical-align:top" |
| 411 | R |
| 412 | }}} |
| 413 | {{{#!td style="vertical-align:top" |
| 414 | 0.0 |
| 415 | }}} |
| 416 | {{{#!td |
| 417 | v-component of the predefined bulk velocity (in m/s).\\\\ |
| 418 | This parameter comes into effect if [#conserve_volume_flow conserve_volume_flow] = ''.T.'' and [#conserve_volume_flow_mode conserve_volume_flow_mode] = '' 'bulk_velocity'.'' |