Changeset 927
- Timestamp:
- Apr 3, 2013, 2:20:46 PM (12 years ago)
- Location:
- trunk
- Files:
-
- 1 added
- 2 deleted
- 7 edited
Legend:
- Unmodified
- Added
- Removed
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trunk/DOC/documentation/disvert.tex
r124 r927 52 52 \end{itemize} 53 53 54 The Exner function: definition. 54 The Exner function: 55 $pk = C_p \times (p/preff)^\kappa$. 55 56 It corresponds to the pressure levels within the layers. 56 57 Used for the computation of the potential temperature. … … 84 85 of the altitude (in km) of the atmospheric level (one per line of the file). 85 86 87 For planetary applications, the usual way to go is to use \textsf{disvert\_noterre.F} together with \textsf{z2sig.def}. 88 The sigma levels are computed as: 89 \begin{itemize} 90 \item $H$ is the first value in \textsf{z2sig.def}, $zsig$ are the following values in \textsf{z2sig.def} 91 \item $\sigma(1)=1$ 92 \item l=2 to llm: $\sigma(l)= 0.5 \times (\exp(-zsig(l)/H)+\exp(-zsig(l-1)/H))$ 93 \item $\sigma(llm+1)=0$ 94 \end{itemize} 95 The $ap$ and $bp$ values, defining the interface pressure levels, are then computed using these sigma values, the reference pressure $preff$, and the transition pressure $pa$. The values of $preff$ and $pa$ are read in the \textsf{start.nc} file, in the control array. 96 86 97 \item Interface pressures: 87 98 computed in \textsf{caldyn0.F, caldyn.F, integrd.F, leapfrog.F} -
trunk/DOC/documentation/newstart.tex
r819 r927 63 63 \end{itemize} 64 64 65 Currently, this tool is well adapted for Venus and Titan, so the corresponding routine is called \textsf{newstart-VT.F}, located in the \textsf{dyn3d} directory. As for the \textsf{start2archive} tool, it is compiled the same way as the GCM .65 Currently, this tool is well adapted for Venus and Titan, so the corresponding routine is called \textsf{newstart-VT.F}, located in the \textsf{dyn3d} directory. As for the \textsf{start2archive} tool, it is compiled the same way as the GCM (in sequential only). 66 66 67 67 As inputs, it takes the \textsf{start\_archive.nc} file with the initial state to be modified, and the \textsf{traceur.def} and \textsf{z2sig.def} files. -
trunk/DOC/documentation/rcm1d.tex
r892 r927 52 52 The goal of this tool is to initialize the model the same way \textsf{gcm.F} does on 3D, but only on a single column, so that the physics may be tested without any dynamics. 53 53 54 It can be compiled with a command like (e.g. for 50 layers):54 It can be compiled (sequential only) with a command like (e.g. for 50 layers): 55 55 56 56 \textsf{makelmdz -p venus -d 50 rcm1d} -
trunk/LMDZ.VENUS/libf/phyvenus/newstart.F
r849 r927 238 238 ip1jmp1old = (imold+1-1/imold)*(jmold+1-1/jmold) 239 239 240 c dans run.def 241 CALL getin('planet_type',planet_type) 242 call ini_cpdet 243 240 244 c======================================================================= 241 245 c CHANGEMENT DE CONSTANTES CONTENUES DANS tab_cntrl … … 1024 1028 & rlonuold,rlatvold,rlonu,rlatv) 1025 1029 write (*,*) 'T ', T(1,jjp1,1) ! INFO 1030 ! pour info: 1031 ! Si extension verticale, la T est extrapolee constante au-dessus de lmold 1026 1032 1027 1033 c passage grille physique pour restartphy.nc … … 1055 1061 do i=1,iip1 1056 1062 ucov( i,j,l ) = unat( i,j,l ) * cu(i,j) 1057 c ucov( i,j,l ) = 0 1063 ! pour info: 1064 ! Si extension verticale, on impose u=0 au-dessus de lmold 1065 if (l.gt.lmold) ucov( i,j,l ) = 0 1058 1066 end do 1059 1067 end do … … 1065 1073 do i=1,iim 1066 1074 vcov( i,j,l ) = vnat( i,j,l ) * cv(i,j) 1067 c vcov( i,j,l ) = 0 1075 ! pour info: 1076 ! Si extension verticale, on impose v=0 au-dessus de lmold 1077 if (l.gt.lmold) vcov( i,j,l ) = 0 1068 1078 end do 1069 1079 vcov( iip1,j,l ) = vcov( 1,j,l )
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