Changeset 12772 for NEMO/branches/2020/ticket_2444/doc/latex/NEMO/subfiles/chap_SBC.tex

Timestamp:

2020-04-17T18:32:46+02:00 (4 years ago)

Author:

mathiot

Message:

#2444: changes requested by Dave

File:

• NEMO/branches/2020/ticket_2444/doc/latex/NEMO/subfiles/chap_SBC.tex (modified) (5 diffs)

NEMO/branches/2020/ticket_2444/doc/latex/NEMO/subfiles/chap_SBC.tex

@@ -1218 +1218 @@
      \np{ln_isfcav_mlt}{ln\_isfcav\_mlt}\forcode{ = .true.} activates the ocean/ice shelf thermodynamics interactions at the ice shelf/ocean interface. 
      If \np{ln_isfcav_mlt}\forcode{ = .false.}, thermodynamics interactions are desctivated but the ocean dynamics inside the cavity is still active.
-     The logical flag \np{ln_isfcav}{ln\_isfcav} control wether or not the ice shelf cavities are closed. \np{ln_isfcav}{ln\_isfcav} is not defined in the namelist but in the domcfg.nc input file.\\
+     The logical flag \np{ln_isfcav}{ln\_isfcav} control whether or not the ice shelf cavities are closed. \np{ln_isfcav}{ln\_isfcav} is not defined in the namelist but in the domcfg.nc input file.\\
 
      3 options are available to represent to ice-shelf/ocean fluxes at the interface:
@@ -1272 +1272 @@
 
         where $T_b$ is the temperature at the interface, $S_b$ the salinity at the interface, $\gamma_T$ and $\gamma_S$ the exchange coefficients for temperature and salt, respectively, 
-        $S_i$ the salinity of the ice (assumedto be 0), $h_{isf}$ the ice shelf thickness, $\rho_i$ the density of the iceshelf, 
+        $S_i$ the salinity of the ice (assumed to be 0), $h_{isf}$ the ice shelf thickness, $\rho_i$ the density of the iceshelf, 
         $c_{p,i}$ the specific heat capacity of the ice, $\kappa$ the thermal diffusivity of the ice 
         and $T_s$ the atmospheric surface temperature (at the ice/air interface, assumed to be -20C). 
@@ -1303 +1303 @@
      The fluxes and friction velocity are computed using the mean temperature, salinity and velocity in the first \np{rn_htbl}{rn\_htbl} m.
      Then, the fluxes are spread over the same thickness (ie over one or several cells).
-     If \np{rn_htbl}{rn\_htbl} larger than top $e_{3}t$, there is no more direct feedback between the freezing point at the interface and the top cell temperature.
+     If \np{rn_htbl}{rn\_htbl} is larger than top $e_{3}t$, there is no more direct feedback between the freezing point at the interface and the top cell temperature.
      This can lead to super-cool temperature in the top cell under melting condition.
      If \np{rn_htbl}{rn\_htbl} smaller than top $e_{3}t$, the top boundary layer thickness is set to the top cell thickness.\\
@@ -1398 +1398 @@
   \caption[Ice shelf location and fresh water flux definition]{
     Illustration of the location where the fwf is injected and
-    whether or not the fwf is interactif or not.}
+    whether or not the fwf is interactive or not.}
   \label{fig:ISF}
 \end{figure}
@@ -1453 +1453 @@
 \item[Step 2]: a new domcfg.nc file is built using the DOMAINcfg tools.
 \item[Step 3]: NEMO run for a specific period and output the average melt rate over the period.
-\item[Step 4]: the ice sheet model run using the melt rate outputed in step 4.
+\item[Step 4]: the ice sheet model run using the melt rate outputed in step 3.
 \item[Step 5]: go back to 1.
 \end{description}