- Timestamp:
- 2018-12-21T15:18:38+01:00 (5 years ago)
- File:
-
- 1 edited
Legend:
- Unmodified
- Added
- Removed
-
NEMO/trunk/doc/latex/NEMO/subfiles/chap_model_basics_zstar.tex
r10414 r10442 6 6 % ================================================================ 7 7 % ================================================================ 8 % Curvilinear z*- s*-coordinate System9 % ================================================================ 10 \chapter{ essai z* s*}11 \section{Curvilinear \ textit{z*}- or \textit{s*}coordinate system}8 % Curvilinear \zstar- \sstar-coordinate System 9 % ================================================================ 10 \chapter{ essai \zstar \sstar} 11 \section{Curvilinear \zstar- or \sstar coordinate system} 12 12 13 13 % ------------------------------------------------------------------------------------------------------------- … … 114 114 and $\rho_w =1,000\,Kg.m^{-3}$ is the volumic mass of pure water. 115 115 The sea-surface height is evaluated using a leapfrog scheme in combination with an Asselin time filter, 116 i.e.the velocity appearing in (\autoref{eq:dynspg_ssh}) is centred in time (\textit{now} velocity).116 (\ie the velocity appearing in (\autoref{eq:dynspg_ssh}) is centred in time (\textit{now} velocity). 117 117 118 118 The surface pressure gradient, also evaluated using a leap-frog scheme, is then simply given by: … … 316 316 \biblio 317 317 318 \pindex 319 318 320 \end{document}
Note: See TracChangeset
for help on using the changeset viewer.