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


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Timestamp:
2010-07-09T14:55:36+02:00 (10 years ago)
Author:
mlelod
Comment:

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  • ticket/0663_MLF

    v24 v25  
    229229• the modifications in trasbc will interfere with the new runoff scheme (see 2009WP/2009Stream3#Substream3.2:fromNEMOteamshort-term) 
    230230 
    231 • Add 'real 3D' treatment of fse3(t/u/v)_b: 
    232    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. 
    233    fse3(u/v)_b are deduced from fse3t_b by a surface averaging (as ssh(u/v) from ssh) 
    234  
    235    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. 
    236    NO!!! It doesn't work. The whole 3D fse3t_b field has to be in the restart file. 
    237  
    238 • Computation of ub and vb 
    239    Devide the filtered transport by the correct scale factor (the fture fse3(u/v)b) in dynnxt 
    240  
    241231• 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. 
    242232