From d66ad7a335ebcc13bcd6e4982e6bce43dcdfc82a Mon Sep 17 00:00:00 2001
From: Sibylle Techene <sibylle.techene@locean-ipsl.upmc.fr>
Date: Fri, 15 Nov 2024 17:14:56 +0000
Subject: [PATCH] Update file chap_DYN.tex
---
latex/NEMO/subfiles/chap_DYN.tex | 2 +-
1 file changed, 1 insertion(+), 1 deletion(-)
diff --git a/latex/NEMO/subfiles/chap_DYN.tex b/latex/NEMO/subfiles/chap_DYN.tex
index ea8a6af..292fdc5 100644
--- a/latex/NEMO/subfiles/chap_DYN.tex
+++ b/latex/NEMO/subfiles/chap_DYN.tex
@@ -78,7 +78,7 @@ The evolution of sea surface height ($\eta$) and vertical velocity ($w$) in ocea
is fundamentally governed by the continuity equation, which ensures the conservation of volume.
Through this equation, we derive expressions for $\eta$ and $w$ that are essential for maintaining
the balance between horizontal and vertical transport in the ocean’s volume-conserving framework.
-Both are deduced from the horizontal divergence $\ksi$ and require the horizontal divergence calculation.
+Both are deduced from the horizontal divergence $\chi$ and require the horizontal divergence calculation.
Because $\eta$ evolution is related to the external mode it is described in \autoref{chap:D2D}
while $w$ evolution is described here after.
--
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