From 4bd947b1a4efa0b20a507d44681208a3f725669d Mon Sep 17 00:00:00 2001
From: Sibylle Techene <sibylle.techene@locean-ipsl.upmc.fr>
Date: Tue, 19 Nov 2024 12:35:44 +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 3240876..945d859 100644
--- a/latex/NEMO/subfiles/chap_DYN.tex
+++ b/latex/NEMO/subfiles/chap_DYN.tex
@@ -77,7 +77,7 @@ can be derived from the 3D terms.
 The evolution of sea surface height ($\eta$) and vertical velocity ($w$) in ocean modeling 
 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.
+the balance between horizontal and vertical transport in the ocean's volume-conserving framework.
 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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