 Timestamp:
 20191014T14:53:52+02:00 (13 months ago)
 File:

 1 edited
Legend:
 Unmodified
 Added
 Removed

NEMO/trunk/doc/latex/NEMO/subfiles/chap_model_basics.tex
r11690 r11693 579 579 an explicit computation of vertical advection relative to the moving ssurfaces. 580 580 581 %\gmcomment{ 582 %A key point here is that the $s$coordinate depends on $(i,j)$ ==> horizontal pressure gradient... 581 \cmtgm{A key point here is that the $s$coordinate depends on $(i,j)$ 582 ==> horizontal pressure gradient...} 583 583 The generalized vertical coordinates used in ocean modelling are not orthogonal, 584 584 which contrasts with many other applications in mathematical physics. … … 680 680 and similar expressions are used for mixing and forcing terms. 681 681 682 \ gmcomment{682 \cmtgm{ 683 683 \colorbox{yellow}{ to be updated $= = >$} 684 684 Add a few works on z and zps and s and underlies the differences between all of them … … 1150 1150 Nevertheless it is currently not available in the isoneutral case. 1151 1151 1152 \ onlyinsubfile{\input{../../global/epilogue}}1152 \subinc{\input{../../global/epilogue}} 1153 1153 1154 1154 \end{document}
Note: See TracChangeset
for help on using the changeset viewer.