Changeset 11537 for NEMO/trunk/doc/latex/NEMO/subfiles/chap_time_domain.tex

Timestamp:

2019-09-12T10:24:48+02:00 (5 years ago)

Author:

clem

Message:

make sure SI3 doc can be compiled, plus small edits

File:

• NEMO/trunk/doc/latex/NEMO/subfiles/chap_time_domain.tex (modified) (2 diffs)

NEMO/trunk/doc/latex/NEMO/subfiles/chap_time_domain.tex

@@ -86 +86 @@
 where the subscript $F$ denotes filtered values and $\gamma$ is the Asselin coefficient.
 $\gamma$ is initialized as \np{rn\_atfp} (namelist parameter).
-Its default value is \np{rn\_atfp}\forcode{ = 10.e-3} (see \autoref{sec:STP_mLF}),
+Its default value is \np{rn\_atfp}\forcode{=10.e-3} (see \autoref{sec:STP_mLF}),
 causing only a weak dissipation of high frequency motions (\citep{farge-coulombier_phd87}).
 The addition of a time filter degrades the accuracy of the calculation from second to first order.
@@ -172 +172 @@
 
 The leapfrog environment supports a centred in time computation of the surface pressure, \ie\ evaluated
-at \textit{now} time step. This refers to as the explicit free surface case in the code (\np{ln\_dynspg\_exp}\forcode{ = .true.}).
+at \textit{now} time step. This refers to as the explicit free surface case in the code (\np{ln\_dynspg\_exp}\forcode{=.true.}).
 This choice however imposes a strong constraint on the time step which should be small enough to resolve the propagation
 of external gravity waves. As a matter of fact, one rather use in a realistic setup, a split-explicit free surface
-(\np{ln\_dynspg\_ts}\forcode{ = .true.}) in which barotropic and baroclinic dynamical equations are solved separately with ad-hoc
+(\np{ln\_dynspg\_ts}\forcode{=.true.}) in which barotropic and baroclinic dynamical equations are solved separately with ad-hoc
 time steps. The use of the time-splitting (in combination with non-linear free surface) imposes some constraints on the design of
 the overall flowchart, in particular to ensure exact tracer conservation (see \autoref{fig:TimeStep_flowchart}).