Changes between Version 449 and Version 450 of doc/app/initialization_parameters

Timestamp:

Dec 5, 2019 8:29:31 AM (5 years ago)

Author:

oliver.maas

Comment:

--

doc/app/initialization_parameters

@@ -1781 +1781 @@
 |----------------
 {{{#!td style="vertical-align:top"
-[=#recycling_yshift '''recycling_yshift''']
-}}}
-{{{#!td style="vertical-align:top"
-I
-}}}
-{{{#!td style="vertical-align:top"
-0
-}}}
-{{{#!td
-Parameter to define a y-shift for the recycled inflow turbulence, given in multiples of PE (may also be negative).\\\\
-E.g. with recycling_yshift = 3  the turbulent fluctuations, obtained at the recycling plane, will be shifted by 3 processors in positive y-direction before being imposed on the inflow. This method can be used to avoid persistent streaks in the longitudinal wind component, that may form in a neutrally stratified boundary layer (detailed information about this method can be found in Munters 2016, ​http://www.dx.doi.org/10.1063/1.4941912). See also description of parameter [#y_shift y_shift].
-
-Note that '''recycling_yshift''' \= 0 requires [#turbulent_inflow turbulent_inflow] = .T..
-}}}
-|----------------
-{{{#!td style="vertical-align:top"
 [=#roughness_length '''roughness_length''']
 }}}
@@ -2082 +2066 @@
 This parameter introduces a shift by multiples of a subdomain size in y-direction at the left/right domain boundary. The shift is such that a point (coordinate y=yr) on the right domain boundary no longer corresponds with the point with the same y-coordinate on the left boundary, but instead with the point with the coordinate {{{y=yr+y_shift*(ny+1)/npey}}}. Conversely, a point on the left boundary with coordinate {{{y=yl}}} corresponds with the point on the right boundary with the coordinate {{{y=yl-y_shift*(ny+1)/npey}}}.\\
 Negative values and also those that exceed npey are allowed. They are transformed to the range {{{[0,npey-1]}}} internally.\\\\
-This feature has been implemented to alleviate the occurrence of streak-like structures that appear during simulations with neutral stratification, cyclic boundary conditions, and driving velocity with no v-component. For a description of these structures, see Munters (2016; ​http://www.dx.doi.org/10.1063/1.4941912). See also description of parameter [#recycling_yshift recycling_yshift].\\\\\\
+This feature has been implemented to alleviate the occurrence of streak-like structures that appear during simulations with neutral stratification, cyclic boundary conditions, and driving velocity with no v-component. For a description of these structures, see Munters (2016; ​http://www.dx.doi.org/10.1063/1.4941912).\\\\
 '''Schematic of the y_shift method:'''\\
 (Model domain with [../inipar#npex npex] = [../inipar#npey npey] = 5 and y_shift = 1)\\
-[[Image(y_shift_pic.png,260px)]]
-'''In case of [../initialization_parameters#bc_lr bc_lr] = 'cyclic' and [../initialization_parameters#turbulent_inflow turbulent_inflow] = .TRUE.:'''\\
-Parameter to define a y-shift for the recycled inflow turbulence, given in multiples of PE (may also be negative).
-E.g. with recycling_yshift = 3 the turbulent fluctuations, obtained at the recycling plane, will be shifted by 3 processors in positive y-direction before being imposed on the inflow.
-
+[[Image(y_shift_pic.png,260px)]]\\\\
+'''In case of [../initialization_parameters#bc_lr bc_lr] = '''dirichlet/radiation''' and [../initialization_parameters#turbulent_inflow turbulent_inflow] = .TRUE.:'''\\
+Parameter to define a y-shift for the recycled inflow turbulence, given in multiples of PE.
+E.g. with y_shift = 3 the turbulent fluctuations, obtained at the recycling plane, will be shifted by 3 processors in positive y-direction before being imposed on the inflow.
 }}}
 |----------------