Changeset 11578 for NEMO/trunk/doc/latex/NEMO/subfiles/chap_DYN.tex

Timestamp:

2019-09-19T19:44:36+02:00 (5 years ago)

Author:

nicolasmartin

Message:

New LaTeX commands \nam and \np to mention namelist content (step 2)
So far so good, the manual compiles successfully 4 times and everything seems in its right place

File:

• NEMO/trunk/doc/latex/NEMO/subfiles/chap_DYN.tex (modified) (5 diffs)

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

@@ -327 +327 @@
 A key point in \autoref{eq:DYN_een_e3f} is how the averaging in the \textbf{i}- and \textbf{j}- directions is made.
 It uses the sum of masked t-point vertical scale factor divided either by the sum of the four t-point masks
-(\np{nn_een_e3f}{nn\_een\_e3f}\forcode{=1}), or just by $4$ (\np{nn\_een\_e3f}\forcode{=.true.}).
+(\np{nn_een_e3f}{nn\_een\_e3f}\forcode{=1}), or just by $4$ (\np{nn_een_e3f}{nn\_een\_e3f}\forcode{=.true.}).
 The latter case preserves the continuity of $e_{3f}$ when one or more of the neighbouring $e_{3t}$ tends to zero and
 extends by continuity the value of $e_{3f}$ into the land areas.
@@ -904 +904 @@
     In this particular exemple,
     a boxcar averaging window over \np{nn_baro}{nn\_baro} barotropic time steps is used
-    (\np{nn\_bt\_flt}\forcode{=1}) and \np{nn_baro}{nn\_baro}\forcode{=5}.
+    (\np{nn_bt_flt}{nn\_bt\_flt}\forcode{=1}) and \np{nn_baro}{nn\_baro}\forcode{=5}.
     Internal mode time steps (which are also the model time steps) are denoted by
     $t-\rdt$, $t$ and $t+\rdt$.
@@ -1265 +1265 @@
 %-------------------------------------------------------------------------------------------------------------
 
-Options are defined through the \nam{zdf} namelist variables.
+Options are defined through the \nam{zdf}{zdf} namelist variables.
 The large vertical diffusion coefficient found in the surface mixed layer together with high vertical resolution implies that in the case of explicit time stepping there would be too restrictive a constraint on the time step.
 Two time stepping schemes can be used for the vertical diffusion term:
@@ -1409 +1409 @@
 flux is from a cell with water depth greater than \np{rn_wdmin1}{rn\_wdmin1} and 0 otherwise. If the user sets
 \np{ln_wd_dl_ramp}{ln\_wd\_dl\_ramp}\forcode{=.true.} the flux across the face is ramped down as the water depth decreases
-from 2 * \np{rn_wdmin1}{rn\_wdmin1} to \np{rn\_wdmin1}. The use of this ramp reduced grid-scale noise in idealised test cases.
+from 2 * \np{rn_wdmin1}{rn\_wdmin1} to \np{rn_wdmin1}{rn\_wdmin1}. The use of this ramp reduced grid-scale noise in idealised test cases.
 
 At the point where the flux across a $u$-face is multiplied by zuwdmask , we have chosen
@@ -1649 +1649 @@
 %-------------------------------------------------------------------------------------------------------------
 
-Options are defined through the \nam{dom} namelist variables.
+Options are defined through the \nam{dom}{dom} namelist variables.
 The general framework for dynamics time stepping is a leap-frog scheme,
 \ie\ a three level centred time scheme associated with an Asselin time filter (cf. \autoref{chap:TD}).