Changeset 11578 for NEMO/trunk/doc/latex/NEMO/subfiles/chap_SBC.tex
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- 2019-09-19T19:44:36+02:00 (5 years ago)
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NEMO/trunk/doc/latex/NEMO/subfiles/chap_SBC.tex
r11577 r11578 37 37 38 38 Four different ways are available to provide the seven fields to the ocean. They are controlled by 39 namelist \nam{sbc} variables:39 namelist \nam{sbc}{sbc} variables: 40 40 41 41 \begin{itemize} … … 842 842 843 843 The optional atmospheric pressure can be used to force ocean and ice dynamics 844 (\np{ln_apr_dyn}{ln\_apr\_dyn}\forcode{=.true.}, \nam{sbc} namelist).844 (\np{ln_apr_dyn}{ln\_apr\_dyn}\forcode{=.true.}, \nam{sbc}{sbc} namelist). 845 845 The input atmospheric forcing defined via \np{sn_apr}{sn\_apr} structure (\nam{sbc_apr}{sbc\_apr} namelist) 846 846 can be interpolated in time to the model time step, and even in space when the interpolation on-the-fly is used. … … 1070 1070 %-------------------------------------------------------------------------------------------------------- 1071 1071 1072 The namelist variable in \nam{sbc} , \np{nn_isf}{nn\_isf}, controls the ice shelf representation.1072 The namelist variable in \nam{sbc}{sbc}, \np{nn_isf}{nn\_isf}, controls the ice shelf representation. 1073 1073 Description and result of sensitivity test to \np{nn_isf}{nn\_isf} are presented in \citet{mathiot.jenkins.ea_GMD17}. 1074 1074 The different options are illustrated in \autoref{fig:SBC_isf}. … … 1266 1266 (Note that the authors kindly provided a copy of their code to act as a basis for implementation in \NEMO). 1267 1267 Icebergs are initially spawned into one of ten classes which have specific mass and thickness as 1268 described in the \nam{berg} namelist: \np{rn_initial_mass}{rn\_initial\_mass} and \np{rn_initial_thickness}{rn\_initial\_thickness}.1268 described in the \nam{berg}{berg} namelist: \np{rn_initial_mass}{rn\_initial\_mass} and \np{rn_initial_thickness}{rn\_initial\_thickness}. 1269 1269 Each class has an associated scaling (\np{rn_mass_scaling}{rn\_mass\_scaling}), 1270 1270 which is an integer representing how many icebergs of this class are being described as one lagrangian point … … 1343 1343 1344 1344 Physical processes related to ocean surface waves can be accounted by setting the logical variable 1345 \np{ln_wave}{ln\_wave}\forcode{=.true.} in \nam{sbc} namelist. In addition, specific flags accounting for1345 \np{ln_wave}{ln\_wave}\forcode{=.true.} in \nam{sbc}{sbc} namelist. In addition, specific flags accounting for 1346 1346 different processes should be activated as explained in the following sections. 1347 1347 … … 1352 1352 Input Data generic Interface (see \autoref{sec:SBC_input}). 1353 1353 \item[coupled mode]: \NEMO\ and an external wave model can be coupled by setting \np{ln_cpl}{ln\_cpl} \forcode{= .true.} 1354 in \nam{sbc} namelist and filling the \nam{sbc_cpl}{sbc\_cpl} namelist.1354 in \nam{sbc}{sbc} namelist and filling the \nam{sbc_cpl}{sbc\_cpl} namelist. 1355 1355 \end{description} 1356 1356 … … 1364 1364 1365 1365 The neutral surface drag coefficient provided from an external data source (\ie\ a wave model), 1366 can be used by setting the logical variable \np{ln_cdgw}{ln\_cdgw} \forcode{= .true.} in \nam{sbc} namelist.1366 can be used by setting the logical variable \np{ln_cdgw}{ln\_cdgw} \forcode{= .true.} in \nam{sbc}{sbc} namelist. 1367 1367 Then using the routine \rou{sbcblk\_algo\_ncar} and starting from the neutral drag coefficent provided, 1368 1368 the drag coefficient is computed according to the stable/unstable conditions of the … … 1561 1561 assuming that the diurnal cycle of SWF is a scaling of the top of the atmosphere diurnal cycle of incident SWF. 1562 1562 The \cite{bernie.guilyardi.ea_CD07} reconstruction algorithm is available in \NEMO\ by 1563 setting \np{ln_dm2dc}{ln\_dm2dc}\forcode{=.true.} (a \textit{\nam{sbc} } namelist variable) when1563 setting \np{ln_dm2dc}{ln\_dm2dc}\forcode{=.true.} (a \textit{\nam{sbc}{sbc}} namelist variable) when 1564 1564 using a bulk formulation (\np{ln_blk}{ln\_blk}\forcode{=.true.}) or 1565 1565 the flux formulation (\np{ln_flx}{ln\_flx}\forcode{=.true.}). … … 1668 1668 The presence at the sea surface of an ice covered area modifies all the fluxes transmitted to the ocean. 1669 1669 There are several way to handle sea-ice in the system depending on 1670 the value of the \np{nn_ice}{nn\_ice} namelist parameter found in \nam{sbc} namelist.1670 the value of the \np{nn_ice}{nn\_ice} namelist parameter found in \nam{sbc}{sbc} namelist. 1671 1671 \begin{description} 1672 1672 \item[nn\_ice = 0]
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