Changeset 9414 for branches/2017/dev_merge_2017/DOC/tex_sub/annex_A.tex

Timestamp:

2018-03-21T15:39:48+01:00 (6 years ago)

Author:

nicolasmartin

Message:

Fix multiple defined references

File:

• branches/2017/dev_merge_2017/DOC/tex_sub/annex_A.tex (modified) (5 diffs)

branches/2017/dev_merge_2017/DOC/tex_sub/annex_A.tex

@@ -16 +16 @@
 % ================================================================
 \section{Chain rule for $s-$coordinates}
-\label{sec:A_continuity}
+\label{sec:A_chain}
 
 In order to establish the set of Primitive Equation in curvilinear $s$-coordinates
@@ -382 +382 @@
 Applying similar manipulation to the second component and replacing 
 $\sigma _1$ and $\sigma _2$ by their expression \autoref{apdx:A_s_slope}, it comes:
-\begin{equation} \label{apdx:A_grad_p}
+\begin{equation} \label{apdx:A_grad_p_1}
 \begin{split}
  -\frac{1}{\rho _o \, e_1 } \left. {\frac{\partial p}{\partial i}} \right|_z
@@ -394 +394 @@
 \end{equation}
 
-An additional term appears in (\autoref{apdx:A_grad_p}) which accounts for the 
+An additional term appears in (\autoref{apdx:A_grad_p_1}) which accounts for the 
 tilt of $s-$surfaces with respect to geopotential $z-$surfaces.
 
@@ -416 +416 @@
 \end{equation*}
 
-Substituing \autoref{apdx:A_pressure} in \autoref{apdx:A_grad_p} and using the definition of 
+Substituing \autoref{apdx:A_pressure} in \autoref{apdx:A_grad_p_1} and using the definition of 
 the density anomaly it comes the expression in two parts:
-\begin{equation} \label{apdx:A_grad_p}
+\begin{equation} \label{apdx:A_grad_p_2}
 \begin{split}
  -\frac{1}{\rho _o \, e_1 } \left. {\frac{\partial p}{\partial i}} \right|_z
@@ -430 +430 @@
 \end{equation}
 This formulation of the pressure gradient is characterised by the appearance of a term depending on the 
-the sea surface height only (last term on the right hand side of expression \autoref{apdx:A_grad_p}).
+the sea surface height only (last term on the right hand side of expression \autoref{apdx:A_grad_p_2}).
 This term will be loosely termed \textit{surface pressure gradient}
 whereas the first term will be termed the