Changes between Version 101 and Version 102 of doc/app/initialization_parameters

Timestamp:

Sep 15, 2010 1:14:14 PM (14 years ago)

Author:

kanani

Comment:

--

doc/app/initialization_parameters

@@ -1610 +1610 @@
 |----------------
 {{{#!td style="vertical-align:top"
+[=#top_heatflux '''top_heatflux''']
+}}}
+{{{#!td style="vertical-align:top"
+R
+}}}
+{{{#!td style="vertical-align:top"
+no prescribed\\
+heatflux
+}}}
+{{{#!td
+Kinematic sensible heat flux at the top boundary (in K m/s).\\\\
+If a value is assigned to this parameter, the internal two-dimensional surface heat flux field {{{tswst}}} is initialized with the value of '''top_heatflux''' as top (horizontally homogeneous) boundary condition for the temperature equation. This additionally requires that a Neumann condition must be used for the potential temperature (see [#bc_pt_t bc_pt_t]), because otherwise the resolved scale may contribute to the top flux so that a constant flux value cannot be guaranteed.\\\\
+'''Note:'''\\
+The application of a top heat flux additionally requires the setting of initial parameter [#use_top_fluxes use_top_fluxes] = ''.T.''.\\\\
+No Prandtl-layer is available at the top boundary so far.\\\\
+See also [#surface_heatflux surface_heatflux].
+}}}
+|----------------
+{{{#!td style="vertical-align:top"
+[=#top_momentumflux_u '''top_momentumflux_u''']
+}}}
+{{{#!td style="vertical-align:top"
+R
+}}}
+{{{#!td style="vertical-align:top"
+no prescribed momentumflux
+}}}
+{{{#!td
+Momentum flux along x at the top boundary (in m^2^/s^2^).\\\\
+If a value is assigned to this parameter, the internal two-dimensional u-momentum flux field {{{uswst}}} is initialized with the value of '''top_momentumflux_u''' as top (horizontally homogeneous) boundary condition for the u-momentum equation.\\\\
+'''Notes:'''\\
+The application of a top momentum flux additionally requires the setting of initial parameter [#use_top_fluxes use_top_fluxes] = ''.T.''. Setting of '''top_momentumflux_u''' requires setting of [#top_momentumflux_v top_momentumflux_v] also.\\\\
+A Neumann condition should be used for the u velocity component (see [#bc_uv_t bc_uv_t]), because otherwise the resolved scale may contribute to the top flux so that a constant flux value cannot be guaranteed.\\\\
+No Prandtl-layer is available at the top boundary so far.\\\\
+The coupled ocean parameter file [../iofiles#PARIN_O PARIN_O] should include dummy REAL value assignments to both '''top_momentumflux_u''' and [#top_momentumflux_v top_momentumflux_v] (e.g. '''top_momentumflux_u''' = ''0.0,'' [#top_momentumflux_v top_momentumflux_v] = ''0.0'') to enable the momentum flux coupling.
+}}}
+|----------------
+{{{#!td style="vertical-align:top"
+[=#top_momentumflux_v '''top_momentumflux_v''']
+}}}
+{{{#!td style="vertical-align:top"
+R
+}}}
+{{{#!td style="vertical-align:top"
+no prescribed momentumflux
+}}}
+{{{#!td
+Momentum flux along y at the top boundary (in m^2^/s^2^).\\\\
+If a value is assigned to this parameter, the internal two-dimensional v-momentum flux field {{{vswst}}} is initialized with the value of '''top_momentumflux_v''' as top (horizontally homogeneous) boundary condition for the v-momentum equation.\\\\
+'''Notes:'''\\
+The application of a top momentum flux additionally requires the setting of initial parameter [#use_top_fluxes use_top_fluxes] = ''.T.''. Setting of '''top_momentumflux_v''' requires setting of [#top_momentumflux_u top_momentumflux_u] also.\\\\
+A Neumann condition should be used for the v velocity component (see [#bc_uv_t bc_uv_t]), because otherwise the resolved scale may contribute to the top flux so that a constant flux value cannot be guaranteed.\\\\
+No Prandtl-layer is available at the top boundary so far.\\\\
+The coupled ocean parameter file [../iofiles#PARIN_O PARIN_O] should include dummy REAL value assignments to both [#top_momentumflux_u top_momentumflux_u] and '''top_momentumflux_v''' (e.g. [#top_momentumflux_u top_momentumflux_u] = ''0.0,'' '''top_momentumflux_'''v = ''0.0'') to enable the momentum flux coupling.
+}}}
+|----------------
+{{{#!td style="vertical-align:top"
+[=#top_salinityflux '''top_salinityflux''']
+}}}
+{{{#!td style="vertical-align:top"
+R
+}}}
+{{{#!td style="vertical-align:top"
+        no prescribed
+salinityflux
+}}}
+{{{#!td
+Kinematic salinity flux at the top boundary, i.e. the sea surface (in psu m/s). 
+
+This parameter only comes into effect for ocean runs (see parameter ocean).
+
+If a value is assigned to this parameter, the internal two-dimensional surface heat flux field saswst is initialized with the value of top_salinityflux as top (horizontally homogeneous) boundary condition for the salinity equation. This additionally requires that a Neumann condition must be used for the salinity (see bc_sa_t), because otherwise the resolved scale may contribute to the top flux so that a constant flux value cannot be guaranteed. 
+
+Note:
+The application of a salinity flux at the model top additionally requires the setting of initial parameter use_top_fluxes = .T..
+
+See also bottom_salinityflux.
+}}}
+|----------------
+{{{#!td style="vertical-align:top"
+[=#turbulent_inflow '''turbulent_inflow''']
+}}}
+{{{#!td style="vertical-align:top"
+L
+}}}
+{{{#!td style="vertical-align:top"
+.F.
+}}}
+{{{#!td
+        Generates a turbulent inflow at side boundaries using a turbulence recycling method.
+
+Turbulent inflow is realized using the turbulence recycling method from Lund et al. (1998, J. Comp. Phys., 140, 233-258) modified by Kataoka and Mizuno (2002, Wind and Structures, 5, 379-392).
+
+A turbulent inflow requires Dirichlet conditions at the respective inflow boundary. So far, a turbulent inflow is realized from the left (west) side only, i.e. bc_lr = 'dirichlet/radiation' is required!
+
+The initial (quasi-stationary) turbulence field should be generated by a precursor run and used by setting initializing_actions = 'cyclic_fill'.
+
+The distance of the recycling plane from the inflow boundary can be set with parameter recycling_width. The heigth above ground above which the turbulence signal is not used for recycling and the width of the layer within the magnitude of the turbulence signal is damped from 100% to 0% can be set with parameters inflow_damping_height and inflow_damping_width.
+
+The detailed setup for a turbulent inflow is described in chapter 3.9.
+}}}
+|----------------
+{{{#!td style="vertical-align:top"
+[=#<insert_parameter_name> '''<insert_parameter_name>''']
+}}}
+{{{#!td style="vertical-align:top"
+<insert type>
+}}}
+{{{#!td style="vertical-align:top"
+<insert value>
+}}}
+{{{#!td
+<insert explanation>
+}}}
+|----------------
+{{{#!td style="vertical-align:top"
 [=#<insert_parameter_name> '''<insert_parameter_name>''']
 }}}