Changes between Version 306 and Version 307 of doc/app/initialization_parameters

Timestamp:

Feb 21, 2017 7:59:31 AM (8 years ago)

Author:

raasch

Comment:

--

doc/app/initialization_parameters

@@ -1420 +1420 @@
 {{{#!td
 Top boundary condition of the specific humidity / total water content.\\\\
-Allowed are the values '' 'dirichlet' '' (q(k=nz) and q(k=nz+1) do not change during the run) and '' 'neumann' ''. With the Neumann boundary condition the value of the humidity gradient at the top is calculated from the initial humidity profile (see [#q_surface q_surface], [#q_vertical_gradient q_vertical_gradient]) by: bc_q_t_val = ( q_init(k=nz) - q_init(k=nz-1)) / dzu(nz).
+Allowed are the values '' 'dirichlet' '' (q(k=nz+1) does not change during the run) and '' 'neumann' ''. With the Neumann boundary condition the value of the humidity gradient at the top is calculated from the initial humidity profile (see [#q_surface q_surface], [#q_vertical_gradient q_vertical_gradient]) by: bc_q_t_val = ( q_init(k=nz) - q_init(k=nz-1)) / dzu(nz).
 Using this value (assumed constant during the run) the humidity boundary values are calculated as 
 
       q(k=nz+1) =q(k=nz) + bc_q_t_val * dzu(nz+1)
 
-(up tp k=nz the prognostic equation for q is solved).\\\\
+(up to k=nz the prognostic equation for q is solved).\\\\
 In case of nested run the default value of '''bc_q_t''' in the nest domains is not '' 'neumann' '' but '' 'nested' '' instead. For the root domain of a nested run  the default is '' 'neumann' '' as usually.\\\\
 }}}
@@ -1455 +1455 @@
 {{{#!td
 Top boundary condition of the scalar concentration.\\\\
-Allowed are the values '' 'dirichlet' '' (s(k=nz) and s(k=nz+1) do not change during the run), '' 'neumann' '' (s(k=nz+1) = s(k=nz)), and '' 'initial_gradient' ''. With the '' 'initial_gradient' '' boundary condition the value of the scalar concentration gradient at the top is calculated from the initial scalar concentration profile (see [#s_surface s_surface], [#s_vertical_gradient s_vertical_gradient]) by: bc_s_t_val = (s_init(k=nz) - s_init(k=nz-1)) / dzu(nz).
+Allowed are the values '' 'dirichlet' '' (s(k=nz+1) does not change during the run), '' 'neumann' '' (s(k=nz+1) = s(k=nz)), and '' 'initial_gradient' ''. With the '' 'initial_gradient' '' boundary condition the value of the scalar concentration gradient at the top is calculated from the initial scalar concentration profile (see [#s_surface s_surface], [#s_vertical_gradient s_vertical_gradient]) by: bc_s_t_val = (s_init(k=nz) - s_init(k=nz-1)) / dzu(nz).
 Using this value (assumed constant during the run) the concentration boundary values are calculated as