Changeset 9394 for branches/2017/dev_merge_2017/DOC/tex_sub/chap_SBC.tex
- Timestamp:
- 2018-03-13T21:21:44+01:00 (6 years ago)
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branches/2017/dev_merge_2017/DOC/tex_sub/chap_SBC.tex
r9393 r9394 161 161 162 162 A generic interface has been introduced to manage the way input data (2D or 3D fields, 163 like surface forcing or ocean T and S) are specify in \NEMO. This task is archieved by fldread.F90.163 like surface forcing or ocean T and S) are specify in \NEMO. This task is archieved by \mdl{fldread}. 164 164 The module was design with four main objectives in mind: 165 165 \begin{enumerate} … … 449 449 450 450 \begin{itemize} 451 \item \mdl{nemogcm} : This routine initialises the rest of the model and repeatedly calls the stp time stepping routine ( step.F90)451 \item \mdl{nemogcm} : This routine initialises the rest of the model and repeatedly calls the stp time stepping routine (\mdl{step}) 452 452 Since the ocean state is not calculated all associated initialisations have been removed. 453 453 \item \mdl{step} : The main time stepping routine now only needs to call the sbc routine (and a few utility functions). … … 1272 1272 and CICE CPP keys \textbf{ORCA\_GRID}, \textbf{CICE\_IN\_NEMO} and \textbf{coupled} should be used (seek advice from UKMO 1273 1273 if necessary). Currently the code is only designed to work when using the CORE forcing option for NEMO (with 1274 \textit{calc\_strair ~=~true} and \textit{calc\_Tsfc~=~true} in the CICE name-list), or alternatively when NEMO1275 is coupled to the HadGAM3 atmosphere model (with \textit{calc\_strair ~=~false} and \textit{calc\_Tsfc~=~false}).1274 \textit{calc\_strair}\forcode{ = .true.} and \textit{calc\_Tsfc}\forcode{ = .true.} in the CICE name-list), or alternatively when NEMO 1275 is coupled to the HadGAM3 atmosphere model (with \textit{calc\_strair}\forcode{ = .false.} and \textit{calc\_Tsfc}\forcode{ = false}). 1276 1276 The code is intended to be used with \np{nn\_fsbc} set to 1 (although coupling ocean and ice less frequently 1277 1277 should work, it is possible the calculation of some of the ocean-ice fluxes needs to be modified slightly - the
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