Changeset 9407 for branches/2017/dev_merge_2017/DOC/tex_sub/chap_ASM.tex

Timestamp:

2018-03-15T17:40:35+01:00 (6 years ago)

Author:

nicolasmartin

Message:

Complete refactoring of cross-referencing

• Use of \autoref instead of simple \ref for contextual text depending on target type
• creation of few prefixes for marker to identify the type reference: apdx|chap|eq|fig|sec|subsec|tab

File:

• branches/2017/dev_merge_2017/DOC/tex_sub/chap_ASM.tex (modified) (6 diffs)

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

@@ -5 +5 @@
 % ================================================================
 \chapter{Apply Assimilation Increments (ASM)}
-\label{ASM}
+\label{chap:ASM}
 
 Authors: D. Lea,  M. Martin, K. Mogensen, A. Weaver, ...   % do we keep
@@ -26 +26 @@
 
 \section{Direct initialization}
-\label{ASM_DI}
+\label{sec:ASM_DI}
 
 Direct initialization (DI) refers to the instantaneous correction
@@ -33 +33 @@
 
 \section{Incremental analysis updates}
-\label{ASM_IAU}
+\label{sec:ASM_IAU}
 
 Rather than updating the model state directly with the analysis increment,
@@ -83 +83 @@
 \end{eqnarray}
 where $\alpha^{-1} = \sum_{i=1}^{M/2} 2i$ and $M$ is assumed to be even. 
-The weights described by \eqref{eq:F2_i} provide a 
+The weights described by \autoref{eq:F2_i} provide a 
 smoother transition of the analysis trajectory from one assimilation cycle 
-to the next than that described by \eqref{eq:F1_i}.
+to the next than that described by \autoref{eq:F1_i}.
 
 %==========================================================================
 % Divergence damping description %%%
 \section{Divergence damping initialisation}
-\label{ASM_details}
+\label{sec:ASM_details}
 
 The velocity increments may be initialized by the iterative application of 
@@ -110 +110 @@
                        +\delta _j \left[ {e_{1v}\,e_{3v}\,v^{n-1}_I} \right]} \right).
 \end{equation}
-By the application of \eqref{eq:asm_dmp} and \eqref{eq:asm_dmp} the divergence is filtered
+By the application of \autoref{eq:asm_dmp} and \autoref{eq:asm_dmp} the divergence is filtered
 in each iteration, and the vorticity is left unchanged. In the presence of coastal boundaries
 with zero velocity increments perpendicular to the coast the divergence is strongly damped.
@@ -125 +125 @@
 
 \section{Implementation details}
-\label{ASM_details}
+\label{sec:ASM_details}
 
 Here we show an example \ngn{namasm} namelist and the header of an example assimilation