From 2d8697419990c4178013add72b35b069f2b91c51 Mon Sep 17 00:00:00 2001
From: Andrew Coward <acc@noc.ac.uk>
Date: Mon, 11 Nov 2024 16:10:33 +0000
Subject: [PATCH] Few more corrections to chap_D2D.tex file
---
latex/NEMO/subfiles/chap_D2D.tex | 11 +++++------
1 file changed, 5 insertions(+), 6 deletions(-)
diff --git a/latex/NEMO/subfiles/chap_D2D.tex b/latex/NEMO/subfiles/chap_D2D.tex
index ca4e727..de7f9e3 100644
--- a/latex/NEMO/subfiles/chap_D2D.tex
+++ b/latex/NEMO/subfiles/chap_D2D.tex
@@ -106,7 +106,7 @@ Note that this option is not yet available with RK3 time-stepping.
%\nlst{namsplit}
The split-explicit free surface formulation used in \NEMO\
-(\np{ln_dynspg_ts}{ln\_dynspg\_ts} set to true), also called the time-splitting
+(\np[=.true.]{ln_dynspg_ts}{ln\_dynspg\_ts}), also called the time-splitting
formulation, follows the one proposed by \citet{shchepetkin.mcwilliams_OM05}. The general
idea is to solve the free surface equation and the associated barotropic velocity
equations with a smaller time step than $\rdt$, the time step used for the three
@@ -140,13 +140,12 @@ hand side of \autoref{eq:D2D_BT_dyn} represents the bottom stress (see section
\autoref{sec:ZDF_drg}), explicitly accounted for at each barotropic iteration.
For 'single 1$^{\mathrm st}$', RK3 time-stepping, barotropic velocities and sea surface
-height are calculated for the {\textit after} timestep from the {\textit before} values
+height are calculated for the \textit{after} timestep from the \textit{before} values
prior to the first stage of the main RK3 timestepping. This occurs in the new module
-\forcode{stp2d.F90} which computes the RHS forcing terms from {\textit before} fields and
+\forcode{stp2d.F90} which computes the RHS forcing terms from \textit{before} fields and
then calls the \forcode{dyn_spg_ts} routine to perform the time-stepping as detailed
below. In the MLF time-stepping case, RHS forcing terms are computed inside
-\forcode{dyn_spg_ts} itself and the time index used will depend on options chosen in
-\forcode{namspgts}.
+\forcode{dyn_spg_ts} itself.
For clarity, in RK3 the RHS forcing terms on momentum are vertically averaged 3D trends of:
\[
@@ -275,7 +274,7 @@ river runoff is taken into account when computing the net freshwater flux.
parameterised contributions from ice-shelf cavities are taken into account when computing
the net freshwater flux.
-(3) When \np[=.true.]{ln_sdw}{ln\_sdw} (see \autoref{sec:SBC_wave_sdw}), the contribution from
+(3) When \np[=.true.]{ln_sdw}{ln\_sdw} (see \autoref{subsec:SBC_wave_sdw}), the contribution from
divergence due to Stoke's drift is taken into account when computing the net freshwater
flux.
--
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