| 1429 | [=#pt_surface '''pt_surface'''] |
| 1430 | }}} |
| 1431 | {{{#!td style="vertical-align:top" |
| 1432 | R |
| 1433 | }}} |
| 1434 | {{{#!td style="vertical-align:top" |
| 1435 | 300.0 |
| 1436 | }}} |
| 1437 | {{{#!td |
| 1438 | Surface potential temperature (in K).\\\\ |
| 1439 | This parameter assigns the value of the potential temperature '''pt''' at the surface (k=0). Starting from this value, the initial vertical temperature profile is constructed with [#pt_vertical_gradient pt_vertical_gradient] and [#pt_vertical_gradient_level pt_vertical_gradient_level]. This profile is also used for the [[1d-model]] as a stationary profile.\\\\ |
| 1440 | '''Attention:'''\\ |
| 1441 | In case of ocean runs (see [#ocean ocean]), this parameter gives the temperature value at the sea surface, which is at k=[#nzt nzt]. The profile is then constructed from the surface down to the bottom of the model. |
| 1442 | }}} |
| 1443 | |---------------- |
| 1444 | {{{#!td style="vertical-align:top" |
| 1445 | [=#pt_surface_initial_change '''pt_surface_initial_change'''] |
| 1446 | }}} |
| 1447 | {{{#!td style="vertical-align:top" |
| 1448 | R |
| 1449 | }}} |
| 1450 | {{{#!td style="vertical-align:top" |
| 1451 | 0.0 |
| 1452 | }}} |
| 1453 | {{{#!td |
| 1454 | Change in surface temperature to be made at the beginning of the 3d run (in K).\\\\ |
| 1455 | If '''pt_surface_initial_change''' is set to a non-zero value, the near surface sensible heat flux is not allowed to be given simultaneously (see [#surface_heatflux surface_heatflux]). |
| 1456 | }}} |
| 1457 | |---------------- |
| 1458 | {{{#!td style="vertical-align:top" |
| 1459 | [=#pt_vertical_gradient '''pt_vertical_gradient'''] |
| 1460 | }}} |
| 1461 | {{{#!td style="vertical-align:top" |
| 1462 | R(10) |
| 1463 | }}} |
| 1464 | {{{#!td style="vertical-align:top" |
| 1465 | 10*0.0 |
| 1466 | }}} |
| 1467 | {{{#!td |
| 1468 | Temperature gradient(s) of the initial temperature profile (in K / 100 m).\\\\ |
| 1469 | This temperature gradient holds starting from the height level defined by [#pt_vertical_gradient_level pt_vertical_gradient_level] (precisely: for all uv levels k where zu(k) > pt_vertical_gradient_level, pt_init(k) is set: pt_init(k) = pt_init(k-1) + dzu(k) * '''pt_vertical_gradient''') up to the top boundary or up to the next height level defined by pt_vertical_gradient_level. A total of 10 different gradients for 11 height intervals (10 intervals if pt_vertical_gradient_level(1) = 0.0) can be assigned. The surface temperature is assigned via [#pt_surface pt_surface].\\\\ |
| 1470 | '''Example:'''\\\\ |
| 1471 | '''pt_vertical_gradient''' = ''1.0'', ''0.5'',\\ |
| 1472 | [#pt_vertical_gradient_level pt_vertical_gradient_level] = ''500.0'', ''1000.0'',\\\\ |
| 1473 | That defines the temperature profile to be neutrally stratified up to z = 500.0 m with a temperature given by [#pt_surface pt_surface]. For 500.0 m < z <= 1000.0 m the temperature gradient is 1.0 K / 100 m and for z > 1000.0 m up to the top boundary it is 0.5 K / 100 m (it is assumed that the assigned height levels correspond with uv levels).\\\\ |
| 1474 | '''Attention:'''\\ |
| 1475 | In case of ocean runs (see [#ocean ocean]), the profile is constructed like described above, but starting from the sea surface (k=[#nzt nzt]) down to the bottom boundary of the model. Height levels have then to be given as negative values, e.g. pt_vertical_gradient_level = ''-500.0,'' ''-1000.0.'' |
| 1476 | }}} |
| 1477 | |---------------- |
| 1478 | {{{#!td style="vertical-align:top" |
| 1479 | [=#pt_vertical_gradient_level '''pt_vertical_gradient_level'''] |
| 1480 | }}} |
| 1481 | {{{#!td style="vertical-align:top" |
| 1482 | R(10) |
| 1483 | }}} |
| 1484 | {{{#!td style="vertical-align:top" |
| 1485 | 10*0.0 |
| 1486 | }}} |
| 1487 | {{{#!td |
| 1488 | Height level from which on the temperature gradient defined by [#pt_vertical_gradient pt_vertical_gradient] is effective (in m).\\\\ |
| 1489 | The height levels have to be assigned in ascending order. The default values result in a neutral stratification regardless of the values of pt_vertical_gradient (unless the top boundary of the model is higher than 100000.0 m). For the piecewise construction of temperature profiles see [#pt_vertical_gradient pt_vertical_gradient].\\\\ |
| 1490 | '''Attention:'''\\ |
| 1491 | In case of ocean runs (see [#ocean ocean]), the (negative) height levels have to be assigned in descending order. |
| 1492 | }}} |
| 1493 | |---------------- |
| 1494 | {{{#!td style="vertical-align:top" |
| 1495 | [=#<insert_parameter_name> '''<insert_parameter_name>'''] |
| 1496 | }}} |
| 1497 | {{{#!td style="vertical-align:top" |
| 1498 | <insert type> |
| 1499 | }}} |
| 1500 | {{{#!td style="vertical-align:top" |
| 1501 | <insert value> |
| 1502 | }}} |
| 1503 | {{{#!td |
| 1504 | <insert explanation> |
| 1505 | }}} |
| 1506 | |---------------- |
| 1507 | {{{#!td style="vertical-align:top" |