Changes between Version 43 and Version 44 of todo

Timestamp:

Oct 23, 2015 11:22:34 AM (9 years ago)

Author:

maronga

Comment:

--

todo

@@ -43 +43 @@
 ||<page>  ||Avoid collecting of 2D data on PE0 (topography data, surface coupling layer) ||  ||
 ||  ||~~Implement flux limiter for Wicker-Skamarock~~ ||~~Matthias, Lennart~~ postponed due to inherent optimization drawbacks  ||
-||<page>  ||Implement RRTM radiation model  ||  ||
+||<page>  ||~~Implement RRTMG radiation model  ||Björn  ||
 ||<page>  ||Subgrid-scale saturation fluctuation for Lagrangian cloud model  ||Fabian  ||
-|| ||Implement new particle data structure in LPM ||Fabian  ||
+|| ||~~Implement new particle data structure in LPM ||Fabian  ||
 || ||~~Implement logarithmic interpolation of particle velocities near the surface~~ ||~~Matthias~~ r1315 ||
 ||  ||Separate equation for passive scalar (multiple scalars?) ||?  ||
@@ -51 +51 @@
 ||  ||implementation of a tracbot, which automatically runs and checks examples in case of any code changes  ||  ||
 ||  ||implement SGS model from Igor Esau  ||  ||
-||  ||implement a soil model (similar to DALES?) ||  ||
+||  ||~~implement a soil model (similar to DALES?) ||Björn ||
 ||~~calc_spectra~~  ||~~check and update the internal calculation of spectra~~ ||~~Matthias (check)~~ ||
-||  ||improve output of standard timeseries: L is defined as Obukhov-length for dry air; should also be defined for moist air; output of buoyancy flux w"vpt"0  ||Björn  ||
+||  ||~~improve output of standard timeseries: L is defined as Obukhov-length for dry air; should also be defined for moist air; output of buoyancy flux w"vpt"0  ||Björn  ||
 ||data_output  ||implement output of hydrostatic pressure ||Björn   ||
 ||data_output  ||implement output of scalar and momentum fluxes calculated by temporal EC ||  ||
-||  ||implement random number generation for ensemble runs ||Helge, Björn   ||
+||  ||~~implement random number generation for ensemble runs ||Helge, Björn   ||
 ||  ||implement new boundary condition for cases where the grid spacing is in the order of the roughness length ||  ||
-||  ||increase limit for some identifier strings (e.g. length of variable names is very limited)||Björn  ||
+||  ||~~increase limit for some identifier strings (e.g. length of variable names is very limited)||Björn  ||
 ||PALM code  ||implement anelastic approximation  ||  ||
 ||  ||implementation of viscous topography  ||  ||
 ||PALM code ||Use NetCDF instead of ASCII for topography data  ||  ||
 ||PALM code ||~~Update GPL~~  ||~~all~~ r1310 ||
-||PALM code  ||Allow runs for >= 10000 cores ||Björn, Siggi  ||
-||PALM code  ||Create temporary job directory via mrun (does not work properly with the FORTRAN system call function)  || ||
+||PALM code  ||~~Allow runs for >= 10000 cores ||Björn, Siggi  ||
+||PALM code  ||~~Create temporary job directory via mrun (does not work properly with the FORTRAN system call function)  || ||
 ||PALM code  ||Discuss the treatment of package parameters, regarding their appearance in {{{read_var_list}}} and {{{write_var_list}}}.  ||all  ||
 || Example runs ||Modify the "building" example run (example_building_p3d), since topography is allowed with WS-scheme ||  ||
@@ -74 +74 @@
 
 == Tools==
-||VAPOR  ||Release final version of nc2vdf  ||  ||
+||~~VAPOR  ||~~Release final version of nc2vdf  ||  ||
 ||<page>  ||<what>  ||<name>  ||