Changeset 14525

Timestamp:

2021-02-22T17:18:04+01:00 (3 years ago)

Author:

nicolasmartin

Message:

Fix manual compilation...
I guess the last ones who recently modified the file had tested their changes before committing

File:

• NEMO/trunk/doc/latex/NEMO/subfiles/chap_SBC.tex (modified) (11 diffs)

NEMO/trunk/doc/latex/NEMO/subfiles/chap_SBC.tex

@@ -975 +975 @@
 M2, S2, N2, K2, nu2, mu2, 2N2, L2, T2, eps2, lam2, R2, M3, MKS2, MN4, MS4, M4,
 N4, S4, M6, and M8; see file \textit{tide.h90} and \mdl{tide\_mod} for further
-information and references\footnote{As a legacy option \np{ln_tide_var} can be
+information and references\footnote{As a legacy option \np{ln_tide_var}{ln\_tide\_var} can be
   set to \forcode{0}, in which case the 19 tidal constituents (M2, N2, 2N2, S2,
   K2, K1, O1, Q1, P1, M4, Mf, Mm, Msqm, Mtm, S1, MU2, NU2, L2, and T2; see file
@@ -1197 +1197 @@
 
      \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.
+     If \np{ln_isfcav_mlt}{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 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:
      \begin{description}
-        \item[\np{cn_isfcav_mlt}\forcode{ = 'spe'}]:
+        \item[\np{cn_isfcav_mlt}{cn\_isfcav\_mlt}\forcode{ = 'spe'}]:
         The fresh water flux is specified by a forcing fields \np{sn_isfcav_fwf}{sn\_isfcav\_fwf}. Convention of the input file is: positive toward the ocean (i.e. positive for melting and negative for freezing).
         The latent heat fluxes is derived from the fresh water flux. 
         The heat content flux is derived from the fwf flux assuming a temperature set to the freezing point in the top boundary layer (\np{rn_htbl}{rn\_htbl})
 
-        \item[\np{cn_isfcav_mlt}\forcode{ = 'oasis'}]:
+        \item[\np{cn_isfcav_mlt}{cn\_isfcav\_mlt}\forcode{ = 'oasis'}]:
         The \forcode{'oasis'} is a prototype of what could be a method to spread precipitation on Antarctic ice sheet as ice shelf melt inside the cavity when a coupled model Atmosphere/Ocean is used. 
         It has not been tested and therefore the model will stop if you try to use it. 
         Actions will be undertake in 2020 to build a comprehensive interface to do so for Greenland, Antarctic and ice shelf (cav), ice shelf (par), icebergs, subglacial runoff and runoff.
 
-        \item[\np{cn_isfcav_mlt}\forcode{ = '2eq'}]:
+        \item[\np{cn_isfcav_mlt}{cn\_isfcav\_mlt}\forcode{ = '2eq'}]:
         The heat flux and the fresh water flux (negative for melting) resulting from ice shelf melting/freezing are parameterized following \citet{Grosfeld1997}. 
         This formulation is based on a balance between the vertical diffusive heat flux across the ocean top boundary layer (\autoref{eq:ISOMIP1}) 
@@ -1231 +1231 @@
         and $\gamma$ the thermal exchange coefficient.
 
-        \item[\np{cn_isfcav_mlt}\forcode{ = '3eq'}]:
+        \item[\np{cn_isfcav_mlt}{cn\_isfcav\_mlt}\forcode{ = '3eq'}]:
         For realistic studies, the heat and freshwater fluxes are parameterized following \citep{Jenkins2001}. This formulation is based on three equations: 
         a balance between the vertical diffusive heat flux across the boundary layer 
@@ -1287 +1287 @@
      If \np{rn_htbl}{rn\_htbl} smaller than top $e_{3}t$, the top boundary layer thickness is set to the top cell thickness.\\
 
-     Each melt formula (\np{cn_isfcav_mlt}\forcode{ = '3eq'} or \np{cn_isfcav_mlt}\forcode{ = '2eq'}) depends on an exchange coeficient ($\Gamma^{T,S}$) between the ocean and the ice.
+     Each melt formula (\np{cn_isfcav_mlt}{cn\_isfcav\_mlt}\forcode{ = '3eq'} or \np{cn_isfcav_mlt}{cn\_isfcav\_mlt}\forcode{ = '2eq'}) depends on an exchange coeficient ($\Gamma^{T,S}$) between the ocean and the ice.
      Below, the exchange coeficient $\Gamma^{T}$ and $\Gamma^{S}$ are respectively defined by \np{rn_gammat0}{rn\_gammat0} and \np{rn_gammas0}{rn\_gammas0}. 
      There are 3 different ways to compute the exchange velocity:
 
      \begin{description}
-        \item[\np{cn_gammablk}\forcode{='spe'}]:
+        \item[\np{cn_gammablk}{cn\_gammablk}\forcode{='spe'}]:
         The salt and heat exchange coefficients are constant and defined by:
 \[
@@ -1302 +1302 @@
         This is the recommended formulation for ISOMIP.
 
-   \item[\np{cn_gammablk}\forcode{='vel'}]:
+   \item[\np{cn_gammablk}{cn\_gammablk}\forcode{='vel'}]:
         The salt and heat exchange coefficients are velocity dependent and defined as
 \[
@@ -1313 +1313 @@
         See \citet{jenkins.nicholls.ea_JPO10} for all the details on this formulation. It is the recommended formulation for realistic application and ISOMIP+/MISOMIP configuration.
 
-   \item[\np{cn_gammablk}\forcode{'vel\_stab'}]:
+   \item[\np{cn_gammablk}{cn\_gammablk}\forcode{'vel\_stab'}]:
         The salt and heat exchange coefficients are velocity and stability dependent and defined as:
 \[
@@ -1329 +1329 @@
   \begin{description}
 
-     \item[\np{cn_isfpar_mlt}\forcode{ = 'bg03'}]:
+     \item[\np{cn_isfpar_mlt}{cn\_isfpar\_mlt}\forcode{ = 'bg03'}]:
      The ice shelf cavities are not represented.
      The fwf and heat flux are computed using the \citet{beckmann.goosse_OM03} parameterisation of isf melting.
      The fluxes are distributed along the ice shelf edge between the depth of the average grounding line (GL)
      (\np{sn_isfpar_zmax}{sn\_isfpar\_zmax}) and the base of the ice shelf along the calving front
-     (\np{sn_isfpar_zmin}{sn\_isfpar\_zmin}) as in (\np{cn_isfpar_mlt}\forcode{ = 'spe'}).
+     (\np{sn_isfpar_zmin}{sn\_isfpar\_zmin}) as in (\np{cn_isfpar_mlt}{cn\_isfpar\_mlt}\forcode{ = 'spe'}).
      The effective melting length (\np{sn_isfpar_Leff}{sn\_isfpar\_Leff}) is read from a file.
      This parametrisation has not been tested since a while and based on \citet{Favier2019}, 
      this parametrisation should probably not be used.
 
-     \item[\np{cn_isfpar_mlt}\forcode{ = 'spe'}]:
+     \item[\np{cn_isfpar_mlt}{cn\_isfpar\_mlt}\forcode{ = 'spe'}]:
      The ice shelf cavity is not represented.
      The fwf (\np{sn_isfpar_fwf}{sn\_isfpar\_fwf}) is prescribed and distributed along the ice shelf edge between
@@ -1346 +1346 @@
      The heat flux ($Q_h$) is computed as $Q_h = fwf \times L_f$.
 
-     \item[\np{cn_isfpar_mlt}\forcode{ = 'oasis'}]:
+     \item[\np{cn_isfpar_mlt}{cn\_isfpar\_mlt}\forcode{ = 'oasis'}]:
      The \forcode{'oasis'} is a prototype of what could be a method to spread precipitation on Antarctic ice sheet as ice shelf melt inside the cavity when a coupled model Atmosphere/Ocean is used. 
      It has not been tested and therefore the model will stop if you try to use it. 
@@ -1353 +1353 @@
   \end{description}
 
-\np{cn_isfcav_mlt}\forcode{ = '2eq'}, \np{cn_isfcav_mlt}\forcode{ = '3eq'} and \np{cn_isfpar_mlt}\forcode{ = 'bg03'} compute a melt rate based on
+\np{cn_isfcav_mlt}{cn\_isfcav\_mlt}\forcode{ = '2eq'}, \np{cn_isfcav_mlt}{cn\_isfcav\_mlt}\forcode{ = '3eq'} and \np{cn_isfpar_mlt}{cn\_isfpar\_mlt}\forcode{ = 'bg03'} compute a melt rate based on
 the water mass properties, ocean velocities and depth.
 The resulting fluxes are thus highly dependent of the model resolution (horizontal and vertical) and 
 realism of the water masses onto the shelf.\\
 
-\np{cn_isfcav_mlt}\forcode{ = 'spe'} and \np{cn_isfpar_mlt}\forcode{ = 'spe'} read the melt rate from a file.
+\np{cn_isfcav_mlt}{cn\_isfcav\_mlt}\forcode{ = 'spe'} and \np{cn_isfpar_mlt}{cn\_isfpar\_mlt}\forcode{ = 'spe'} read the melt rate from a file.
 You have total control of the fwf forcing.
 This can be useful if the water masses on the shelf are not realistic or
@@ -1437 +1437 @@
 \end{description}
 
-If \np{ln_iscpl}\forcode{ = .true.}, the isf draft is assume to be different at each restart step with
+If \np{ln_iscpl}{ln\_iscpl}\forcode{ = .true.}, the isf draft is assume to be different at each restart step with
 potentially some new wet/dry cells due to the ice sheet dynamics/thermodynamics.
 The wetting and drying scheme, applied on the restart, is very simple. The 6 different possible cases for the tracer and ssh are:
@@ -1482 +1482 @@
 
 In order to remove the trend and keep the conservation level as close to 0 as possible,
-a simple conservation scheme is available with \np{ln_isfcpl_cons}\forcode{ = .true.}.
+a simple conservation scheme is available with \np{ln_isfcpl_cons}{ln\_isfcpl\_cons}\forcode{ = .true.}.
 The heat/salt/vol. gain/loss are diagnosed, as well as the location.
 A correction increment is computed and applied each time step during the model run.