Changes between Version 85 and Version 86 of doc/app/initialization_parameters


Ignore:
Timestamp:
Sep 15, 2010 11:00:07 AM (14 years ago)
Author:
kanani
Comment:

--

Legend:

Unmodified
Added
Removed
Modified
  • doc/app/initialization_parameters

    v85 v86  
    14271427|----------------
    14281428{{{#!td style="vertical-align:top"
     1429[=#pt_surface '''pt_surface''']
     1430}}}
     1431{{{#!td style="vertical-align:top"
     1432R
     1433}}}
     1434{{{#!td style="vertical-align:top"
     1435300.0
     1436}}}
     1437{{{#!td
     1438Surface potential temperature (in K).\\\\
     1439This 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:'''\\
     1441In 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"
     1448R
     1449}}}
     1450{{{#!td style="vertical-align:top"
     14510.0
     1452}}}
     1453{{{#!td
     1454Change in surface temperature to be made at the beginning of the 3d run (in K).\\\\
     1455If '''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"
     1462R(10)
     1463}}}
     1464{{{#!td style="vertical-align:top"
     146510*0.0
     1466}}}
     1467{{{#!td
     1468Temperature gradient(s) of the initial temperature profile (in K / 100 m).\\\\
     1469This 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'',\\\\
     1473That 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:'''\\
     1475In 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"
     1482R(10)
     1483}}}
     1484{{{#!td style="vertical-align:top"
     148510*0.0
     1486}}}
     1487{{{#!td
     1488Height level from which on the temperature gradient defined by [#pt_vertical_gradient pt_vertical_gradient] is effective (in m).\\\\
     1489The 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:'''\\
     1491In 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"
    14291508[=#<insert_parameter_name> '''<insert_parameter_name>''']
    14301509}}}