- Timestamp:
- 2020-12-15T22:18:46+01:00 (3 years ago)
- Location:
- NEMO/trunk/doc/latex/NEMO/subfiles
- Files:
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- 4 edited
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NEMO/trunk/doc/latex/NEMO/subfiles/chap_DYN.tex
r14113 r14177 763 763 which imposes a very small time step when an explicit time stepping is used. 764 764 Two methods are proposed to allow a longer time step for the three-dimensional equations: 765 the filtered free surface, which is a modification of the continuous equations (see \autoref{eq:MB_flt?}),765 the filtered free surface, which is a modification of the continuous equations \iffalse (see \autoref{eq:MB_flt?}) \fi 766 766 and the split-explicit free surface described below. 767 767 The extra term introduced in the filtered method is calculated implicitly, -
NEMO/trunk/doc/latex/NEMO/subfiles/chap_OBS.tex
r11708 r14177 892 892 \subsubsection{Running} 893 893 894 The simplest way to use the executable is to edit and append the \ textbf{sao.nml} namelist to894 The simplest way to use the executable is to edit and append the \nam{sao}{sao} namelist to 895 895 a full \NEMO\ namelist and then to run the executable as if it were nemo.exe. 896 896 … … 914 914 For example, to read the second time counter from a single file the namelist would be. 915 915 916 \begin{forlines} 916 \begin{listing} 917 % \nlst{namsao} 918 \begin{forlines} 917 919 !---------------------------------------------------------------------- 918 920 ! namsao Standalone obs_oper namelist … … 924 926 nn_sao_idx = 2 925 927 / 926 \end{forlines} 928 \end{forlines} 929 \caption{\forcode{&namsao}} 930 \label{lst:namsao} 931 \end{listing} 927 932 928 933 %% ================================================================================================= … … 1119 1124 To plot some data run IDL and then: 1120 1125 1121 \begin{ minted}{idl}1126 \begin{verbatim} 1122 1127 IDL> dataplot, "filename" 1123 \end{ minted}1128 \end{verbatim} 1124 1129 1125 1130 To read multiple files into dataplot, … … 1127 1132 the easiest method is to use the spawn command to generate a list of files which can then be passed to dataplot. 1128 1133 1129 \begin{ minted}{idl}1134 \begin{verbatim} 1130 1135 IDL> spawn, 'ls profb*.nc', files 1131 1136 IDL> dataplot, files 1132 \end{ minted}1137 \end{verbatim} 1133 1138 1134 1139 \autoref{fig:OBS_dataplotmain} shows the main window which is launched when dataplot starts. -
NEMO/trunk/doc/latex/NEMO/subfiles/chap_SBC.tex
r14130 r14177 664 664 For the cool-skin scheme parametrization COARE and ECMWF algorithms share the same 665 665 basis: \citet{fairall.bradley.ea_JGRO96}. With some minor updates based 666 on \citet{zeng.beljaars_GRL05} for ECMWF , and \citet{fairall.ea_19} for COARE666 on \citet{zeng.beljaars_GRL05} for ECMWF \iffalse, and \citet{fairall.ea_19?} for COARE \fi 667 667 3.6. 668 668 … … 671 671 turbulence input from Langmuir circulation). 672 672 673 Importantly, COARE warm-layer scheme \ citep{fairall.ea_19}includes a prognostic673 Importantly, COARE warm-layer scheme \iffalse \citep{fairall.ea_19?} \fi includes a prognostic 674 674 equation for the thickness of the warm-layer, while it is considered as constant 675 675 in the ECWMF algorithm. … … 971 971 and tidal analysis in the model framework. This includes the computation of the gravitational 972 972 surface forcing, as well as support for lateral forcing at open boundaries (see 973 \autoref{subsec:LBC_bdy_tides}) and tidal harmonic analysis (see974 \autoref{subsec:DIA_diamlr } and \autoref{subsec:DIA_diadetide}). The module is973 \autoref{subsec:LBC_bdy_tides}) and tidal harmonic analysis \iffalse (see 974 \autoref{subsec:DIA_diamlr?} and \autoref{subsec:DIA_diadetide?}) \fi . The module is 975 975 activated with \np[=.true.]{ln_tide}{ln\_tide} in namelist 976 976 \nam{_tide}{\_tide}. It provides the same 34 tidal constituents that are -
NEMO/trunk/doc/latex/NEMO/subfiles/chap_ZDF.tex
r14113 r14177 731 731 \subsubsection{Evolution of the boundary layer depth} 732 732 733 The prognostic equation for the depth of the neutral/unstable boundary layer is given by \ citep{grant+etal18},733 The prognostic equation for the depth of the neutral/unstable boundary layer is given by \iffalse \citep{grant+etal18?}, \fi 734 734 735 735 \begin{equation} … … 747 747 equation for the case when the pycnocline has a finite thickness, 748 748 based on the potential energy budget of the OSBL, is the leading term 749 \ citep{grant+etal18}of a generalization of that used in mixed-layer749 \iffalse \citep{grant+etal18?} \fi of a generalization of that used in mixed-layer 750 750 models e.g.\ \citet{kraus.turner_T67}, in which the thickness of the pycnocline is taken to be zero. 751 751
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