Changeset 6497 for trunk/DOC/TexFiles/Chapters/Chap_SBC.tex

Timestamp:

2016-04-27T09:33:46+02:00 (8 years ago)

Author:

gm

Message:

#1720 - trunk: add Casimir tidal parameterization

File:

• trunk/DOC/TexFiles/Chapters/Chap_SBC.tex (modified) (5 diffs)

trunk/DOC/TexFiles/Chapters/Chap_SBC.tex

@@ -128 +128 @@
 The ocean model provides, at each time step, to the surface module (\mdl{sbcmod}) 
 the surface currents, temperature and salinity.  
-These variables are averaged over \np{nf\_sbc} time-step (\ref{Tab_ssm}), 
+These variables are averaged over \np{nn\_fsbc} time-step (\ref{Tab_ssm}), 
 and it is these averaged fields which are used to computes the surface fluxes 
-at a frequency of \np{nf\_sbc} time-step.
+at a frequency of \np{nn\_fsbc} time-step.
 
 
@@ -144 +144 @@
 \caption{  \label{Tab_ssm}   
 Ocean variables provided by the ocean to the surface module (SBC). 
-The variable are averaged over nf{\_}sbc time step, $i.e.$ the frequency of 
-computation of surface fluxes.}
+The variable are averaged over nn{\_}fsbc time step, 
+$i.e.$ the frequency of computation of surface fluxes.}
 \end{center}   \end{table}
 %--------------------------------------------------------------------------------------------------------------
@@ -592 +592 @@
 or larger than the one of the input atmospheric fields.
 
+The \np{sn\_wndi}, \np{sn\_wndj}, \np{sn\_qsr}, \np{sn\_qlw}, \np{sn\_tair}, \np{sn\_humi},
+\np{sn\_prec}, \np{sn\_snow}, \np{sn\_tdif} parameters describe the fields 
+and the way they have to be used (spatial and temporal interpolations). 
+
+\np{cn\_dir} is the directory of location of bulk files
+\np{ln\_taudif} is the flag to specify if we use Hight Frequency (HF) tau information (.true.) or not (.false.)
+\np{rn\_zqt}: is the height of humidity and temperature measurements (m)
+\np{rn\_zu}: is the height of wind measurements (m)
+
+Three multiplicative factors are availables : 
+\np{rn\_pfac} and \np{rn\_efac} allows to adjust (if necessary) the global freshwater budget 
+by increasing/reducing the precipitations (total and snow) and or evaporation, respectively.
+The third one,\np{rn\_vfac}, control to which extend the ice/ocean velocities are taken into account 
+in the calculation of surface wind stress. Its range should be between zero and one, 
+and it is recommended to set it to 0.
+
 % -------------------------------------------------------------------------------------------------------------
 %        CLIO Bulk formulea
@@ -926 +942 @@
 \begin{description}
 \item[\np{nn\_isf}~=~1]
-The ice shelf cavity is represented (\np{ln\_isfcav}~=~true needed). The fwf and heat flux are computed. Two different bulk formula are available:
+The ice shelf cavity is represented (\np{ln\_isfcav}~=~true needed). The fwf and heat flux are computed. 
+Two different bulk formula are available:
    \begin{description}
    \item[\np{nn\_isfblk}~=~1]
@@ -988 +1005 @@
 This parameter is only used if \np{nn\_isf}~=~1 or \np{nn\_isf}~=~4
 
-If \np{rn\_hisf\_tbl} = 0.0, the fluxes are put in the top level whatever is its tickness. 
-
-If \np{rn\_hisf\_tbl} $>$ 0.0, the fluxes are spread over the first \np{rn\_hisf\_tbl} m (ie over one or several cells).\\
+If \np{rn\_hisf\_tbl} = 0., the fluxes are put in the top level whatever is its tickness. 
+
+If \np{rn\_hisf\_tbl} $>$ 0., the fluxes are spread over the first \np{rn\_hisf\_tbl} m (ie over one or several cells).\\
 
 The ice shelf melt is implemented as a volume flux with in the same way as for the runoff.