Changeset 3683 for trunk/DOC/TexFiles/Chapters/Chap_DYN.tex

Timestamp:

2012-11-27T16:21:24+01:00 (11 years ago)

Author:

gm

Message:

trunk: #926 NEMO_book.pdf : references are invisible + error corrections

File:

• trunk/DOC/TexFiles/Chapters/Chap_DYN.tex (modified) (5 diffs)

trunk/DOC/TexFiles/Chapters/Chap_DYN.tex

@@ -127 +127 @@
 This is of paramount importance. Replacing $T$ by the number $1$ in the tracer equation and summing
 over the water column must lead to the sea surface height equation otherwise tracer content
-will not be conserved \ref{Griffies_al_MWR01, LeclairMadec2009}.
+will not be conserved \citep{Griffies_al_MWR01, Leclair_Madec_OM09}.
 
 The vertical velocity is computed by an upward integration of the horizontal 
@@ -189 +189 @@
 the relative vorticity term and horizontal kinetic energy for the planetary vorticity 
 term (MIX scheme) ; or conserving both the potential enstrophy of horizontally non-divergent 
-flow and horizontal kinetic energy (EEN scheme) (see  Appendix~\ref{Apdx_C_vor_zad}). In the 
+flow and horizontal kinetic energy (EEN scheme) (see  Appendix~\ref{Apdx_C_vorEEN}). In the 
 case of ENS, ENE or MIX schemes the land sea mask may be slightly modified to ensure the 
 consistency of vorticity term with analytical equations (\textit{ln\_dynvor\_con}=true).
@@ -331 +331 @@
 This EEN scheme in fact combines the conservation properties of the ENS and ENE schemes. 
 It conserves both total energy and potential enstrophy in the limit of horizontally 
-nondivergent flow ($i.e.$ $\chi$=$0$) (see  Appendix~\ref{Apdx_C_vor_zad}). 
+nondivergent flow ($i.e.$ $\chi$=$0$) (see  Appendix~\ref{Apdx_C_vorEEN}). 
 Applied to a realistic ocean configuration, it has been shown that it leads to a significant 
 reduction of the noise in the vertical velocity field \citep{Le_Sommer_al_OM09}. 
@@ -938 +938 @@
 is the \textit{before} velocity in time, except for the pure vertical component 
 that appears when a tensor of rotation is used. This latter term is solved 
-implicitly together with the vertical diffusion term (see \S\ref{DOM_nxt}) 
+implicitly together with the vertical diffusion term (see \S\ref{STP}) 
 
 At the lateral boundaries either free slip, no slip or partial slip boundary 
@@ -1066 +1066 @@
 scheme (\np{ln\_zdfexp}=true) using a time splitting technique 
 (\np{nn\_zdfexp} $>$ 1) or $(b)$ a backward (or implicit) time differencing scheme 
-(\np{ln\_zdfexp}=false) (see \S\ref{DOM_nxt}). Note that namelist variables 
+(\np{ln\_zdfexp}=false) (see \S\ref{STP}). Note that namelist variables 
 \np{ln\_zdfexp} and \np{nn\_zdfexp} apply to both tracers and dynamics.