Changes between Version 41 and Version 42 of ticket/1593_CNRS9_NOC3_LDF
- Timestamp:
- 2015-10-25T12:23:23+01:00 (8 years ago)
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ticket/1593_CNRS9_NOC3_LDF
v41 v42 23 23 Three steps: [[BR]] 24 24 25 ''' I. Phasing of horizontal scale factors ''' ===>>> OK see ''' revision [https://forge.ipsl.jussieu.fr/nemo/log/branches/2015/dev_r5721_CNRS9_NOC3_LDF?rev=5737 5737] ''' + minor correction''' revision [https://forge.ipsl.jussieu.fr/nemo/log/branches/2015/dev_r5721_CNRS9_NOC3_LDF?rev=5737 5737](SETTE OK)'''25 ''' I. Phasing of horizontal scale factors ''' ===>>> OK see ''' revision [https://forge.ipsl.jussieu.fr/nemo/log/branches/2015/dev_r5721_CNRS9_NOC3_LDF?rev=5737 5737] ''' + minor correction''' revision [https://forge.ipsl.jussieu.fr/nemo/log/branches/2015/dev_r5721_CNRS9_NOC3_LDF?rev=5737 5737] (SETTE OK)''' 26 26 27 27 ''' (I.1)''' standardisation of the name of quantities derived from horizontal scale factors (many modules of NEMO)[[BR]]The chosen names of quantities derived from horizontal scale factors are:[[BR]]- inverse of scale factors : r1_e1t, r1_e2t, r1_e1u, r1_e2u, r1_e1v, r1_e2v, r1_e1f, r1_e2f ;[[BR]]- surfaces and their inverse: e1e2t, e1e2u , e1e2v, e1e2f and, r1_e1e2t , r1_e1e2u , r1_e1e2v, r1_e1e2f ;[[BR]]- ratio (used in traldf...) : e2_e1u , e1_e2v(I.1) generalize of the use of surface scale factors ;[[BR]]These quantities are defined in memory in dom_oce.F90, and set to their proper value in domhgr.F90 … … 29 29 ''' (I.2)''' add a optional read of surface scale factors at velocity points in coordinate file (domhgr.F90)[[BR]] The input coordinate file have to include e1e2u and e1e2v in case of reduction of the scale factors in some straits.[[BR]] When e1u or e2v are reduced in some straits, the surface at u- and v-points remains unchanged.[[BR]] This allows to suppress the dom_vvl_orca_fix routine from dlmvvl.F90 module.[[BR]]''Note that this change modifies the model results'', as it contains a better handling of reduced strait width (i.e. reduced surface between 2 adjacent U or V points, but unchanged U and V points volume).[[BR]] The implementation performed here is a first step to the full simplification of domhgr.F90. We kept here the hard coded reduction of scale factor in some straits for some given ORCA configuration. [[BR]] A last step (see IV) will be to suppress the hard coded reduction of some scale factor as it will be always given in the coordinates.nc file together with the e1e2u & e1e2v surfaces. ===>>> OK see '''revision [https://forge.ipsl.jussieu.fr/nemo/log/branches/2015/dev_r5721_CNRS9_NOC3_LDF?rev=5737 5755]''' 30 30 31 ''' [[BR]] [[BR]]II. Phasing of the advective/diffusive trends on tracers'''31 ''' [[BR]] [[BR]] II. Phasing of the advective/diffusive trends on tracers''' 32 32 33 33 '''II.1 —''' '''LDF on tracers''' (both TRA & TRC) - Diffusive trends : ''' '''===>>> OK see '''revision [https://forge.ipsl.jussieu.fr/nemo/log/branches/2015/dev_r5721_CNRS9_NOC3_LDF?rev=5737 5758] & [https://forge.ipsl.jussieu.fr/nemo/log/branches/2015/dev_r5721_CNRS9_NOC3_LDF?rev=5737 5759] and [https://forge.ipsl.jussieu.fr/nemo/log/branches/2015/dev_r5721_CNRS9_NOC3_LDF?rev=5737 5760] with SETTE OK''' … … 125 125 * remove all "!CDIR " lines = NEC vector compiler instructions 126 126 127 ''' [[BR]] [[BR]] III. Phasing of momentum trends ''' ===>>> OK see ''' revision [https://forge.ipsl.jussieu.fr/nemo/log/branches/2015/dev_r5721_CNRS9_NOC3_LDF?rev=5777 5777] & [https://forge.ipsl.jussieu.fr/nemo/log/branches/2015/dev_r5721_CNRS9_NOC3_LDF?rev=5778 5778] and [https://forge.ipsl.jussieu.fr/nemo/log/branches/2015/dev_r5721_CNRS9_NOC3_LDF?rev=5782 5782]with SETTE OK'''127 ''' [[BR]] [[BR]] III. Phasing of momentum trends ''' ===>>> OK see ''' revision [https://forge.ipsl.jussieu.fr/nemo/log/branches/2015/dev_r5721_CNRS9_NOC3_LDF?rev=5777 5777] & [https://forge.ipsl.jussieu.fr/nemo/log/branches/2015/dev_r5721_CNRS9_NOC3_LDF?rev=5778 5778] and [https://forge.ipsl.jussieu.fr/nemo/log/branches/2015/dev_r5721_CNRS9_NOC3_LDF?rev=5782 5782] with SETTE OK''' 128 128 129 129 '''III.1 —''' '''LDF on dynamics''' - viscous trends … … 206 206 '''• '''specification of lateral friction at the coast.[[BR]]Issue: the different values of fmask at the coast have been removed so that this lateral boundary condition doesn't affect the advective term (''' double check that''' !). fmask is still used for laplacian and bilaplacian viscosities. Nevertheless, the magnitude of lateral friction depends on the magnitude of ahm (bhm, reap.). It seems better to define this magnitude [[BR]]Solution: [[BR]]- '''add''' a scalar in the coordinate file which is equal to the grid-size at the equator even if Equator is not in the domain and use this scalar to compute the grid-size dependency of the coefficients. 207 207 208 ''' [[BR]] [[BR]]V. Pending issues : to be solved in 2016 ?'''208 ''' [[BR]] [[BR]] V. Pending issues : to be solved in 2016 ?''' 209 209 210 210 '''(V.1)''' Add a proper coding of Smagorinsky eddy viscosity and diffusivity... … … 212 212 '''(V.2)''' It should be possible to remove hdivn ... think about that 213 213 214 [[BR]] '''Next Step :'''214 [[BR]] ''' Next Step :''' 215 215 216 216 Starting from this branch, another branch is created ('''given the name here''') which will contain the following item (random order): … … 231 231 '''To be CHECKED''' (not necessary associated with this branch) 232 232 233 * find ''!!gm'' everywhere in the fortran code, and try to solve the issues raised ! 233 234 * check that task_i use ssmask, i.e. that it takes into account the under ice shelf seas. 234 235 235 * CRS : the new arrays derived from horizontal scale factors MUST be added in CRS. 236 237 236 * Bug in diawri.F90 when NOT using key_iomput (OK ==>> see ticket #1596) 238 237