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Commit d66ad7a3 authored by Sibylle Techene's avatar Sibylle Techene
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Update file chap_DYN.tex

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    ...@@ -78,7 +78,7 @@ The evolution of sea surface height ($\eta$) and vertical velocity ($w$) in ocea ...@@ -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. 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 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 $\ksi$ 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} Because $\eta$ evolution is related to the external mode it is described in \autoref{chap:D2D}
    while $w$ evolution is described here after. while $w$ evolution is described here after.
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