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- 2020-12-04T20:15:58+01:00 (3 years ago)
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NEMO/trunk/doc/latex/NEMO/subfiles/chap_model_basics_zstar.tex
r11693 r14113 30 30 31 31 In that case, the free surface equation is nonlinear, and the variations of volume are fully taken into account. 32 These coordinates systems is presented in a report \citep{levier.treguier.ea_ rpt07} available on the \NEMO\ web site.32 These coordinates systems is presented in a report \citep{levier.treguier.ea_trpt07} available on the \NEMO\ web site. 33 33 34 34 \colorbox{yellow}{ end of to be updated} … … 170 170 171 171 The split-explicit formulation has a damping effect on external gravity waves, 172 which is weaker than the filtered free surface but still significant as shown by \citet{levier.treguier.ea_ rpt07} in172 which is weaker than the filtered free surface but still significant as shown by \citet{levier.treguier.ea_trpt07} in 173 173 the case of an analytical barotropic Kelvin wave. 174 174 … … 306 306 307 307 In the non-linear free surface formulation, the variations of volume are fully taken into account. 308 This option is presented in a report \citep{levier.treguier.ea_ rpt07} available on the \NEMO\ web site.308 This option is presented in a report \citep{levier.treguier.ea_trpt07} available on the \NEMO\ web site. 309 309 The three time-stepping methods (explicit, split-explicit and filtered) are the same as in 310 310 \autoref{?:DYN_spg_linear?} except that the ocean depth is now time-dependent.
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