Changes between Version 240 and Version 241 of doc/app/initialization_parameters

Timestamp:

Apr 23, 2014 2:38:07 PM (11 years ago)

Author:

boeske

Comment:

--

doc/app/initialization_parameters

@@ -264 +264 @@
 }}}
 {{{#!td
-Parameter to choose large scale forcing from an external file. By means of '''large_scale_forcing''' = ''.T.'' the time-dependent surface heat flux '''shf''', surface water flux '''qsws''', surface temperature '''pt_surface''', surface humidity and surface pressure '''surface_pressure''' as well as vertical profiles of the geostrophic wind components '''ug''' and '''vg''', the large scale vertical subsidence profile '''w_subs''', the horizontal large scale advection tendencies of temperature '''td_lsa_lpt''' and humidity '''td_lsa_q''' and the large scale subsidence tendencies of temperature '''td_sub_lpt''' and humidity '''td_sub_q''' are provided in the simulation. An example can be found [../examples/nudging here].\\
+Parameter to choose large scale forcing from an external file. By means of '''large_scale_forcing''' = ''.T.'' the time-dependent surface heat flux '''shf''', surface water flux '''qsws''', surface temperature '''pt_surface''', surface humidity and surface pressure '''surface_pressure''' as well as vertical profiles of the geostrophic wind components '''ug''' and '''vg''', the large scale vertical subsidence profile '''w_subs''', the horizontal large scale advection tendencies of temperature '''td_lsa_lpt''' and humidity '''td_lsa_q''' and the large scale subsidence tendencies of temperature '''td_sub_lpt''' and humidity '''td_sub_q''' are provided in the simulation. An example can be found [../examples/lsf here].\\
 
 '''large_scale_forcing''' = ''.T.'' requires [#humidity humidity] = .T.. It is not implemented for [#ocean ocean] runs and non cyclic lateral boundary conditions. It is possible to drive the simulations either by means of surface fluxes or by means of prescribed surface values for temperature and humidity. \\
@@ -322 +322 @@
 Parameter to choose nudging. Nudging is a relaxation technique which adjusts the large-eddy simulation to a given, larger scale flow situation. It can for example be used to simulate an observed situation. Further information can be found [../../tec/nudging here]. \\\\
 
-With '''nudging''' = ''.T.'', additional tendencies are calculated for the prognostic variable u, v, pt and q. It requires [#humidity humidity] = .T. as well as  [#large_scale_forcing large_scale forcing] = .T.. So far, it is not implemented for [#ocean ocean] runs and non cyclic lateral boundary conditions. An example can be found [../examples/nudging here]. \\\\
+With '''nudging''' = ''.T.'', additional tendencies are calculated for the prognostic variable u, v, pt and q. It requires [#humidity humidity] = .T. as well as  [#large_scale_forcing large_scale forcing] = .T.. So far, it is not implemented for [#ocean ocean] runs and non cyclic lateral boundary conditions. An example can be found [../examples/lsf here]. \\\\
 
 Additionally, this mode requires the input file [../iofiles#NUDGING_DATA NUDGING_DATA]. This file contains profile information at several time steps about the relaxation time scale tau and the prognostic variables u, v, w, pt, q which must be provided by a larger scale model or by measurements.