Changes between Initial Version and Version 1 of doc/app/plant_canopy_parameters


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Timestamp:
Mar 19, 2014 11:51:18 AM (11 years ago)
Author:
kanani
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  • doc/app/plant_canopy_parameters

    v1 v1  
     1== Canopy Parameters ==
     2[[TracNav(doc/app/partoc|nocollapse)]] ----noch ändern?
     3\\\\\\\\\\\\\\\\\\\\\\\\\\\\\\\\
     4'''NAMELIST group name: canopy_par''' \\
     5
     6||='''Parameter Name'''  =||='''[../fortrantypes FORTRAN Type]'''  =||='''Default Value'''  =||='''Explanation'''  =||
     7|----------------
     8{{{#!td style="vertical-align:top;width: 150px"
     9[=#canopy_mode '''canopy_mode''']
     10}}}
     11{{{#!td style="vertical-align:top;width: 50px"
     12C*20
     13}}}
     14{{{#!td style="vertical-align:top;width: 75px"
     15'block'
     16}}}
     17{{{#!td
     18Canopy mode.\\\\
     19Besides using the default value, that will create a horizontally homogeneous plant canopy that extends over the total horizontal extension of the model domain, the user may add code to the user interface (see [#3.5.1 3.5.1]) subroutine {{{user_init_plant_canopy}}} to allow further canopy modes.\\\\
     20The setting of '''canopy_mode''' becomes only active, if [#plant_canopy plant_canopy] has been set ''.T.'' and a non-zero [#drag_coefficient drag_coefficient] has been defined.
     21}}}
     22|----------------
     23{{{#!td style="vertical-align:top"
     24[=#cthf '''cthf''']
     25}}}
     26{{{#!td style="vertical-align:top"
     27R
     28}}}
     29{{{#!td style="vertical-align:top"
     300.0
     31}}}
     32{{{#!td
     33Average heat flux that is prescribed at the top of the plant canopy.\\\\
     34If [#plant_canopy plant_canopy] is set ''.T.'', the user can prescribe a heat flux at the top of the plant canopy.
     35It is assumed that solar radiation penetrates the canopy and warms the foliage which, in turn, warms the air in contact with it.\\\\
     36'''Note:'''\\
     37Instead of using the value prescribed by [#surface_heatflux surface_heatflux], the near surface heat flux is determined from an exponential function that is dependent on the cumulative leaf_area_index (Shaw and Schumann (1992, Boundary Layer Meteorol., 61, 47-64)).
     38}}}
     39|----------------
     40{{{#!td style="vertical-align:top"
     41[=#drag_coefficient '''drag_coefficient''']
     42}}}
     43{{{#!td style="vertical-align:top"
     44R
     45}}}
     46{{{#!td style="vertical-align:top"
     470.0
     48}}}
     49{{{#!td
     50Drag coefficient used in the {{{plant_canopy_model}}}.\\\\
     51This parameter has to be non-zero, if the parameter [#plant_canopy plant_canopy] is set ''.T.''.
     52}}}
     53|----------------
     54{{{#!td style="vertical-align:top"
     55[=#lad_surface '''lad_surface''']
     56}}}
     57{{{#!td style="vertical-align:top"
     58R
     59}}}
     60{{{#!td style="vertical-align:top"
     610.0
     62}}}
     63{{{#!td
     64Surface value of the leaf area density (in m^2^/m^3^).\\\\
     65This parameter assigns the value of the leaf area density '''lad''' at the surface (k=0). Starting from this value, the leaf area density profile is constructed with [#lad_vertical_gradient lad_vertical_gradient] and [#lad_vertical_gradient_level lad_vertical_gradient_level].
     66}}}
     67|----------------
     68{{{#!td style="vertical-align:top"
     69[=#lad_vertical_gradient '''lad_vertical_gradient''']
     70}}}
     71{{{#!td style="vertical-align:top"
     72R(10)
     73}}}
     74{{{#!td style="vertical-align:top"
     7510 * 0.0
     76}}}
     77{{{#!td
     78Gradient(s) of the leaf area density (in m^2^/m^4^).\\\\
     79This leaf area density gradient holds starting from the height level defined by [#lad_vertical_gradient_level lad_vertical_gradient_level] (precisely: for all uv levels k where zu(k) > lad_vertical_gradient_level, lad(k) is set: lad(k) = lad(k-1) + dzu(k) * '''lad_vertical_gradient''') up to the level defined by [#pch_index pch_index]. Above that level lad(k) will automatically be set to 0.0. A total of 10 different gradients for 11 height intervals (10 intervals if lad_vertical_gradient_level(1) = 0.0) can be assigned. The leaf area density at the surface is assigned via [#lad_surface lad_surface]. 
     80}}}
     81|----------------
     82{{{#!td style="vertical-align:top"
     83[=#lad_vertical_gradient_level '''lad_vertical_gradient_level''']
     84}}}
     85{{{#!td style="vertical-align:top"
     86R(10)
     87}}}
     88{{{#!td style="vertical-align:top"
     8910 * 0.0
     90}}}
     91{{{#!td
     92Height level from which on the gradient of the leaf area density defined by [#lad_vertical_gradient lad_vertical_gradient] is effective (in m).\\\\
     93The height levels have to be assigned in ascending order. The default values result in a leaf area density that is constant with height up to the top of the plant canopy layer defined by [#pch_index pch_index]. For the piecewise construction of temperature profiles see [#lad_vertical_gradient lad_vertical_gradient].
     94}}}
     95|----------------
     96{{{#!td style="vertical-align:top"
     97[=#leaf_surface_concentration '''leaf_surface_concentration''']
     98}}}
     99{{{#!td style="vertical-align:top"
     100R
     101}}}
     102{{{#!td style="vertical-align:top"
     1030.0
     104}}}
     105{{{#!td
     106Concentration of a passive scalar at the surface of a leaf (in K m/s).\\\\
     107This parameter is only of importance in cases in that both, [#plant_canopy plant_canopy] and [#passive_scalar passive_scalar], are set ''.T..'' The value of the concentration of a passive scalar at the surface of a leaf is required for the parametrisation of the sources and sinks of scalar concentration due to the canopy.
     108}}}
     109|----------------
     110{{{#!td style="vertical-align:top"
     111[=#pch_index '''pch_index''']
     112}}}
     113{{{#!td style="vertical-align:top"
     114I
     115}}}
     116{{{#!td style="vertical-align:top"
     1170
     118}}}
     119{{{#!td
     120Grid point index (scalar) of the upper boundary of the plant canopy layer.\\\\
     121Above '''pch_index''' the arrays of leaf area density and [#drag_coeffient drag_coeffient] are automatically set to zero in case of [#plant_canopy plant_canopy] = ''.T.''. Up to '''pch_index''' a leaf area density profile can be prescribed by using the parameters [#lad_surface lad_surface], [#lad_vertical_gradient lad_vertical_gradient] and [#lad_vertical_gradient_level lad_vertical_gradient_level].
     122}}}
     123|----------------
     124{{{#!td style="vertical-align:top"
     125[=#plant_canopy '''plant_canopy''']
     126}}}
     127{{{#!td style="vertical-align:top"
     128L
     129}}}
     130{{{#!td style="vertical-align:top"
     131.F.
     132}}}
     133{{{#!td
     134Switch for the plant canopy model.\\\\
     135If '''plant_canopy''' is set ''.T.'', the plant canopy model of Watanabe (2004, BLM 112, 307-341) is used.\\
     136The impact of a plant canopy on a turbulent flow is considered by an additional drag term in the momentum equations and an additional sink term in the prognostic equation for the subgrid-scale TKE. These additional terms depend on the leaf drag coefficient (see [#drag_coefficient drag_coefficient]), and the leaf area density (see [#lad_surface lad_surface], [#lad_vertical_gradient lad_vertical_gradient], [#lad_vertical_gradient_level lad_vertical_gradient_level]). The top boundary of the plant canopy is determined by the parameter [#pch_index pch_index]. For all heights equal or larger than zw(k=pch_index), the leaf area density is 0 (i.e. there is no canopy at these heights!).\\
     137By default, a horizontally homogeneous plant canopy is prescribed, if  '''plant_canopy''' is set ''.T.''. However, the user can define other types of plant canopies (see [#canopy_mode canopy_mode]).\\\\
     138If '''plant_canopy''' and  [#passive_scalar passive_scalar] are set ''.T.'', the canopy acts as an additional scalar source or sink, respectively. The source/sink strength depends on the scalar concentration at the leaf surface, which generally does not vary with time in PALM, and which can be specified with parameter [#leaf_surface_concentration leaf_surface_concentration].\\\\
     139Additional heating by the plant canopy is taken into account, if the default value of parameter [#cthf cthf] is altered in the parameter file. In that case, the value of [#surface_heatflux surface_heatflux] specified in the parameter file is not used in the model. Instead, the near-surface heat flux is derived from an exponential function that depends on the cumulative leaf area index.\\\\
     140'''plant_canopy''' = ''.T.'' is only allowed with a non-zero [#drag_coefficient drag_coefficient].
     141}}}
     142|----------------
     143{{{#!td style="vertical-align:top"
     144[=#scalar_exchange_coefficient '''scalar_exchange_coefficient''']
     145}}}
     146{{{#!td style="vertical-align:top"
     147R
     148}}}
     149{{{#!td style="vertical-align:top"
     1500.0
     151}}}
     152{{{#!td
     153Scalar exchange coefficient for a leaf (dimensionless).\\\\
     154This parameter is only of importance in cases in that both, [#plant_canopy plant_canopy] and [#passive_scalar passive_scalar], are set ''.T.''. The value of the scalar exchange coefficient is required for the parametrisation of the sources and sinks of scalar concentration due to the canopy.
     155}}}
     156|----------------
     157
     158