Changeset 9408
 Timestamp:
 20180315T18:00:59+01:00 (6 years ago)
 Location:
 branches/2017/dev_merge_2017/DOC/tex_sub
 Files:

 2 edited
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branches/2017/dev_merge_2017/DOC/tex_sub/annex_A.tex
r9407 r9408 213 213 + w \;\frac{\partial u}{\partial z} \\ 214 214 % 215 \intertext{introducing the chain rule (\ ref{Apdx_A_s_chain_rule}) }215 \intertext{introducing the chain rule (\autoref{apdx:A_s_chain_rule}) } 216 216 % 217 217 &= \left. {\frac{\partial u }{\partial t}} \right_z … … 248 248 \; \frac{\partial u}{\partial s} \\ 249 249 % 250 \intertext{Introducing $\omega$, the diaasurface velocity given by (\ ref{Apdx_A_w_s}) }250 \intertext{Introducing $\omega$, the diaasurface velocity given by (\autoref{apdx:A_w_s}) } 251 251 % 252 252 &= \left. {\frac{\partial u }{\partial t}} \right_z … … 343 343 % 344 344 \intertext {Introducing a more compact form for the divergence of the momentum fluxes, 345 and using (\ ref{Apdx_A_sco_Continuity}), the $s$coordinate continuity equation,345 and using (\autoref{apdx:A_sco_Continuity}), the $s$coordinate continuity equation, 346 346 it becomes : } 347 347 % 
branches/2017/dev_merge_2017/DOC/tex_sub/annex_C.tex
r9407 r9408 612 612 \allowdisplaybreaks 613 613 \intertext{Using successively \autoref{eq:DOM_di_adj}, $i.e.$ the skew symmetry property of 614 the $\delta$ operator, \autoref{eq:wzv}, the continuity equation, \autoref{ dynhpg_sco},614 the $\delta$ operator, \autoref{eq:wzv}, the continuity equation, \autoref{eq:dynhpg_sco}, 615 615 the hydrostatic equation in the $s$coordinate, and $\delta_{k+1/2} \left[ z_t \right] \equiv e_{3w} $, 616 616 which comes from the definition of $z_t$, it becomes: }
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