From b0bc822ced26e0b1f7852e8a04d25cd548874354 Mon Sep 17 00:00:00 2001
From: Pierre Mathiot <pierre.mathiot@univ-grenoble-alpes.fr>
Date: Wed, 18 Dec 2024 14:41:06 +0100
Subject: [PATCH] minor changes after review
---
latex/NEMO/subfiles/chap_DOM.tex | 7 ++++---
1 file changed, 4 insertions(+), 3 deletions(-)
diff --git a/latex/NEMO/subfiles/chap_DOM.tex b/latex/NEMO/subfiles/chap_DOM.tex
index ab62d7f..97ba989 100644
--- a/latex/NEMO/subfiles/chap_DOM.tex
+++ b/latex/NEMO/subfiles/chap_DOM.tex
@@ -476,7 +476,7 @@ Where $r3t(i,j,t) = \frac{\eta(i,j,t)}{\mathrm{ht\_0}(i,j)}$,
the ratio of sea surface height to reference water column height,
is updated at every time step by \rou{domqco\_r3c} and where
\forcode{e3t_0}, \forcode{ht_0} and \forcode{tmask} are the $T$-point variants of the reference vertical scale
-factor, the reference water height, and the land-sea mask, respectively.
+factor, the reference water column height, and the land-sea mask, respectively.
Similar expressions are applied to the scale factors at $u$/$v$/$f$-points using appropriate interpolation of $\eta$.
In the expressions for the scale factors at $w$-levels, grid point depths and water heights,
the ratio is instead unmasked.
@@ -594,6 +594,7 @@ Unlike in the previous approach, the height of the $T$-points remains unchanged.
This representation is described in \citep{kevlahan_GMD15}, it is
based on Brinkman penalization where a control parameter \ie\ the porosity modifies fluxes though penalized lateral surfaces.
This parameter is encapsulated within vertical scale factors ($e3t^0$, $e3u^0$, $e3v^0$) as illustrated in \autoref{fig:DOM_partial_step_scheme}.
+In case of ocean cavities, partial cells are also applied at the top interface using the same method as for the bottom interface but upside-down.
\begin{figure}
\centering
@@ -639,8 +640,8 @@ Based on variables \forcode{top_level} and \forcode{bottom_level}, the mask vari
Note that, without ice shelves cavities,
masks at $T$- and $w$-points are identical with the numerical indexing used
(see \autoref{subsec:DOM_Num_Index}).
-Nevertheless,
-$wmask$ are required with ocean cavities to deal with the top boundary (ice shelf/ocean interface)
+Nevertheless, with ocean cavities,
+$wmask$ are required to deal with the top boundary (ice shelf/ocean interface)
in exactly the same way as for the bottom boundary.
%% The specification of closed lateral boundaries requires that at least
--
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