Changeset 11582 for NEMO/trunk/doc/latex/NEMO/subfiles/apdx_triads.tex
- Timestamp:
- 2019-09-20T11:44:31+02:00 (5 years ago)
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NEMO/trunk/doc/latex/NEMO/subfiles/apdx_triads.tex
r11577 r11582 11 11 \newcommand{\rtriadt}[1]{\ensuremath{\triadt{i}{k}{#1}{i_p}{k_p}}} 12 12 13 \onlyinsubfile{\makeindex} 14 13 15 \begin{document} 14 16 % ================================================================ … … 42 44 The options specific to the Griffies scheme include: 43 45 \begin{description} 44 \item[ \np{ln_triad_iso}{ln\_triad\_iso}]46 \item[{\np{ln_triad_iso}{ln\_triad\_iso}}] 45 47 See \autoref{sec:TRIADS_taper}. 46 48 If this is set false (the default), … … 53 55 giving an almost pure horizontal diffusive tracer flux within the mixed layer. 54 56 This is similar to the tapering suggested by \citet{gerdes.koberle.ea_CD91}. See \autoref{subsec:TRIADS_Gerdes-taper} 55 \item[ \np{ln_botmix_triad}{ln\_botmix\_triad}]57 \item[{\np{ln_botmix_triad}{ln\_botmix\_triad}}] 56 58 See \autoref{sec:TRIADS_iso_bdry}. 57 59 If this is set false (the default) then the lateral diffusive fluxes … … 59 61 If it is set true, however, then these lateral diffusive fluxes are applied, 60 62 giving smoother bottom tracer fields at the cost of introducing diapycnal mixing. 61 \item[ \np{rn_sw_triad}{rn\_sw\_triad}]63 \item[{\np{rn_sw_triad}{rn\_sw\_triad}}] 62 64 blah blah to be added.... 63 65 \end{description} 64 66 The options shared with the Standard scheme include: 65 67 \begin{description} 66 \item[ \np{ln_traldf_msc}{ln\_traldf\_msc}] blah blah to be added67 \item[ \np{rn_slpmax}{rn\_slpmax}] blah blah to be added68 \item[{\np{ln_traldf_msc}{ln\_traldf\_msc}}] blah blah to be added 69 \item[{\np{rn_slpmax}{rn\_slpmax}}] blah blah to be added 68 70 \end{description} 69 71 … … 646 648 Note that both near bottom triad slopes \triad{i}{k}{R}{1/2}{1/2} and \triad{i+1}{k}{R}{-1/2}{1/2} are masked when 647 649 either of the $i,k+1$ or $i+1,k+1$ tracer points is masked, \ie\ the $i,k+1$ $u$-point is masked. 648 The associated lateral fluxes (grey-black dashed line) are masked if \np {ln_botmix_triad}{ln\_botmix\_triad}\forcode{ = .false.},649 but left unmasked, giving bottom mixing, if \np {ln_botmix_triad}{ln\_botmix\_triad}\forcode{ = .true.}.650 651 The default option \np {ln_botmix_triad}{ln\_botmix\_triad}\forcode{ = .false.} is suitable when the bbl mixing option is enabled652 (\np {ln_trabbl}{ln\_trabbl}\forcode{ = .true.}, with \np{nn_bbl_ldf}{nn\_bbl\_ldf}\forcode{ = 1}), or for simple idealized problems.653 For setups with topography without bbl mixing, \np {ln_botmix_triad}{ln\_botmix\_triad}\forcode{ = .true.} may be necessary.650 The associated lateral fluxes (grey-black dashed line) are masked if \np[=.false.]{ln_botmix_triad}{ln\_botmix\_triad}, 651 but left unmasked, giving bottom mixing, if \np[=.true.]{ln_botmix_triad}{ln\_botmix\_triad}. 652 653 The default option \np[=.false.]{ln_botmix_triad}{ln\_botmix\_triad} is suitable when the bbl mixing option is enabled 654 (\np[=.true.]{ln_trabbl}{ln\_trabbl}, with \np[=1]{nn_bbl_ldf}{nn\_bbl\_ldf}), or for simple idealized problems. 655 For setups with topography without bbl mixing, \np[=.true.]{ln_botmix_triad}{ln\_botmix\_triad} may be necessary. 654 656 % >>>>>>>>>>>>>>>>>>>>>>>>>>>> 655 657 \begin{figure}[h] … … 672 674 \ie\ the $i,k+1$ $u$-point is masked. 673 675 The associated lateral fluxes (grey-black dashed line) are masked if 674 \protect\np {ln_botmix_triad}{ln\_botmix\_triad}\forcode{ = .false.}, but left unmasked,675 giving bottom mixing, if \protect\np {ln_botmix_triad}{ln\_botmix\_triad}\forcode{ = .true.}}676 \protect\np[=.false.]{ln_botmix_triad}{ln\_botmix\_triad}, but left unmasked, 677 giving bottom mixing, if \protect\np[=.true.]{ln_botmix_triad}{ln\_botmix\_triad}} 676 678 \label{fig:TRIADS_bdry_triads} 677 679 \end{figure} … … 715 717 \label{sec:TRIADS_lintaper} 716 718 717 This is the option activated by the default choice \np {ln_triad_iso}{ln\_triad\_iso}\forcode{ = .false.}.719 This is the option activated by the default choice \np[=.false.]{ln_triad_iso}{ln\_triad\_iso}. 718 720 Slopes $\tilde{r}_i$ relative to geopotentials are tapered linearly from their value immediately below 719 721 the mixed layer to zero at the surface, as described in option (c) of \autoref{fig:LDF_eiv_slp}, to values … … 1145 1147 \label{sec:TRIADS_sfdiag} 1146 1148 1147 Where the namelist parameter \np {ln_traldf_gdia}{ln\_traldf\_gdia}\forcode{ = .true.},1149 Where the namelist parameter \np[=.true.]{ln_traldf_gdia}{ln\_traldf\_gdia}, 1148 1150 diagnosed mean eddy-induced velocities are output. 1149 1151 Each time step, streamfunctions are calculated in the $i$-$k$ and $j$-$k$ planes at … … 1171 1173 \] 1172 1174 1173 \ biblio1174 1175 \ pindex1175 \onlyinsubfile{\bibliography{../main/bibliography}} 1176 1177 \onlyinsubfile{\printindex} 1176 1178 1177 1179 \end{document}
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