Changes between Version 24 and Version 25 of ticket/0663_MLF

Timestamp:

2010-07-09T14:55:36+02:00 (14 years ago)

Author:

mlelod

Comment:

--

ticket/0663_MLF

@@ -229 +229 @@
 • the modifications in trasbc will interfere with the new runoff scheme (see 2009WP/2009Stream3#Substream3.2:fromNEMOteamshort-term)
 
-• Add 'real 3D' treatment of fse3(t/u/v)_b:
-   fse3t_b is not the repartition of sshb. Local conservation implies that the filter correction done on ssh is concentrated in the first level and not distributed on the vertical. => full 3D field is needed. CAUTION: It will slightly alter the Lagrangian treatment of barotropic vertical motions.
-   fse3(u/v)_b are deduced from fse3t_b by a surface averaging (as ssh(u/v) from ssh)
-
-   Add a non corrected before ssh field, sshbnc, in the restart file in order to compute fse3ub. This variable won't be used in the code, just for the restart.
-   NO!!! It doesn't work. The whole 3D fse3t_b field has to be in the restart file.
-
-• Computation of ub and vb
-   Devide the filtered transport by the correct scale factor (the fture fse3(u/v)b) in dynnxt
-
 • Caution: Vertical mass transport is only the baroclinic mas transport in the vvl case. only the Eulerian part of vertical motions is taken into account.