Changeset 3218 for branches/2011/dev_NEMO_MERGE_2011/DOC/TexFiles/Chapters/Chap_LDF.tex

Timestamp:

2011-12-13T11:31:24+01:00 (12 years ago)

Author:

agn

Message:

agn: changes to documentation in dev_NEMO_MERGE_2011

--Reordered NEMO_book.tex, changed from 11pt->12pt,

only needs pstricks for logos

--more abbreviations in mathabbrev.sty
--Corrected bug in Abstracts_Foreword.tex that put whole

text into small

--Clarified discussion of LDF operator rotation in
Chap_Model_Basics.tex, Chap_LDF.tex, Annex_B.tex
--Discuss surface tapering of Griffies triads, how they

work in s-coordinates, eddy-induced velocities in
Annex_ISO.tex. Extra ref in Biblio.bib
Extra figures Fig_bdry_triads.pdf, Fig_triad_MLB.pdf
Modified namelist section namtra_ldf

--Minor corrections to Chap_DIA.tex, Chap_CFG.tex,

Chap_SBC.tex, Annex_A.tex, Chap_DOM.tex, Chap_ASM.tex

File:

• branches/2011/dev_NEMO_MERGE_2011/DOC/TexFiles/Chapters/Chap_LDF.tex (modified) (2 diffs)

branches/2011/dev_NEMO_MERGE_2011/DOC/TexFiles/Chapters/Chap_LDF.tex

@@ -220 +220 @@
 and either \np{ln\_traldf\_hor}=True or \np{ln\_dynldf\_hor}=True. 
 
-\subsection{slopes for tracer iso-neutral mixing}
+\subsection{Slopes for tracer iso-neutral mixing}\label{LDF_slp_iso}
 In iso-neutral mixing  $r_1$ and $r_2$ are the slopes between the iso-neutral 
 and computational surfaces. Their formulation does not depend on the vertical 
@@ -369 +369 @@
 
 
-In addition and also for numerical stability reasons \citep{Cox1987, Griffies_Bk04}, 
-the slopes are bounded by $1/100$ everywhere. This limit is decreasing linearly 
-to zero fom $70$ meters depth and the surface (the fact that the eddies "feel" the 
-surface motivates this flattening of isopycnals near the surface).
+% In addition and also for numerical stability reasons \citep{Cox1987, Griffies_Bk04}, 
+% the slopes are bounded by $1/100$ everywhere. This limit is decreasing linearly 
+% to zero fom $70$ meters depth and the surface (the fact that the eddies "feel" the 
+% surface motivates this flattening of isopycnals near the surface).
 
 For numerical stability reasons \citep{Cox1987, Griffies_Bk04}, the slopes must also