Changes between Version 26 and Version 27 of ticket/1593_CNRS9_NOC3_LDF
- Timestamp:
- 2015-10-05T08:03:53+02:00 (9 years ago)
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ticket/1593_CNRS9_NOC3_LDF
v26 v27 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''' … … 61 61 ! ! Coefficients: 62 62 nn_aht_ijk_t = 21 ! space/time variation of eddy coef 63 ! ! =-20 (=-30) read in eddy_ induced_velocity_2D.nc (..._3D.nc) file63 ! ! =-20 (=-30) read in eddy_diffusivity_2D.nc (..._3D.nc) file 64 64 ! ! = 0 constant 65 65 ! ! = 10 F(k) =ldf_c1d … … 94 94 '''[[BR]]II.2 —''' '''Advective trends''' :TRA/traadv.... ===>>> OK see '''revision [https://forge.ipsl.jussieu.fr/nemo/log/branches/2015/dev_r5721_CNRS9_NOC3_LDF?rev=5737 5770] & [https://forge.ipsl.jussieu.fr/nemo/log/branches/2015/dev_r5721_CNRS9_NOC3_LDF?rev=5737 5771] ===>> SETTE OK with revision [https://forge.ipsl.jussieu.fr/nemo/log/branches/2015/dev_r5721_CNRS9_NOC3_LDF?rev=5737 5774] & [https://forge.ipsl.jussieu.fr/nemo/log/branches/2015/dev_r5721_CNRS9_NOC3_LDF?rev=5737 5775]''' 95 95 96 -traadv_muscl2.F90 removed[[BR]]- traadv_muscl.F90 renamed traadv_mus.F90[[BR]]- traadv_cen2.F90 replaced by traadv_cen which provides 2nd and 4th order centered scheme on both horizontal and vertical directions.[[BR]]- name TVD has been changed to the more commonly used FCT (Flux Correction Transport)[[BR]]- FCT offers now 2nd and 4th order centered scheme on both horizontal and vertical directions.[[BR]]- UBS offers now in option either a 2nd order FCT or a 4th order COMPACT scheme in the vertical direction[[BR]]- NB in case of 4th order in the vertical, CEN, UBS and FCT use a compact 4th order scheme[[BR]]- key_esopa removed from traadv.F9096 * traadv_muscl2.F90 removed[[BR]]- traadv_muscl.F90 renamed traadv_mus.F90[[BR]]- traadv_cen2.F90 replaced by traadv_cen which provides 2nd and 4th order centered scheme on both horizontal and vertical directions.[[BR]]- name TVD has been changed to the more commonly used FCT (Flux Correction Transport)[[BR]]- FCT offers now 2nd and 4th order centered scheme on both horizontal and vertical directions.[[BR]]- UBS offers now in option either a 2nd order FCT or a 4th order COMPACT scheme in the vertical direction[[BR]]- NB in case of 4th order in the vertical, CEN, UBS and FCT use a compact 4th order scheme[[BR]]- key_esopa removed from traadv.F90 97 97 98 98 [[BR]]- Surface boundary condition in ISF case has been added in all cases (except 4th order COMPACT scheme which currently don't work with ISF) … … 123 123 * Atmospheric pressure forcing: change to a systematic call of sbc_apr in step.F90 (with or without BDY) and remove its call from sbcmod[[BR]]- remove key_ldftra_smag and associated module (ldftra_smag.F90)[[BR]]- remove key_vectopt_loop from all the code except in domzgr_substitute.h90 (it is an obsolescent feature only adapted to vector computers)[[BR]]- remove all "!CDIR " lines = NEC vector compiler instructions 124 124 125 ''' [[BR]] [[BR]]III. Phasing of viscous trends'''125 ''' [[BR]] [[BR]] III. Phasing of viscous trends''' 126 126 127 127 '''III.1 —''' '''LDF on dynamics''' - viscous trends : ===>>> OK see '''revision .... and ..... with SETTE OK''' 128 128 129 ''operator'': [[BR]]- laplacian operator: re-entrant laplacian for iso-level operators ( dynldf_lap);[[BR]]- bilaplacian operator: dynldf_blp.F90 module: use of the re-entrant iso-level laplacian [[BR]]- suppression of .... ;[[BR]]- rotb and rotn arrays suppressed (even from the restart file) NB: the viscous operator now uses the full before velocity field (i.e. including the asselin filter)[[BR]]- hdivn and hdivb removed from restart too[[BR]]- divcur.F90 becomes divhor.F90 and only computes the horizontal divergence129 ''operator'': [[BR]]- laplacian operator: re-entrant laplacian for iso-level operators (routine dyn_ldf_lap found in dynldf_lap_blp);[[BR]]- bilaplacian operator: dynldf_blp.F90 module: use of the re-entrant iso-level laplacian (routine dyn_ldf_blp found in dynldf_lap_blp.F90)[[BR]]- suppression of dynnept.F90 to finalize the suppression of Neptune effect param. ;[[BR]]- suppression of dynldf_lap.F90 and dynldf_bilap.F90 replaced by dynldf_lap_blp.F90 (which contains dyn_ldf_lap & dyn_ldf_blp routines) ; dynldf_bilapg.F90 (remove old and approximative rotated bi-laplacian on momentum)[[BR]]- rotb and rotn arrays suppressed (even from the restart file) NB: the viscous operator now uses the full before velocity field (i.e. including the asselin filter)[[BR]]- hdivb array is suppressed. hdivn and hdivb are removed from restart[[BR]]- associate with rotn and rotb suppression comes the suppression of no-slip accurate option (key_noslip_accurate is removed)[[BR]]- divcur.F90 becomes divhor.F90 and only computes the horizontal divergence 130 130 131 131 [[BR]]''lateral mixing coefficient'':[[BR]]- new user interface (namelist) : … … 159 159 / 160 160 }}} 161 [[BR]]- default value of the namelist: ''no operator chosen'': ln_dynldf_lap=dyndf_blp=0 No lateral diffusion applied on momentum '''===>>> check THAT'''[[BR]]- create the 2D and 3D ahtu and ahtv file for ORCA_R2 '''===>>> TO BE DONE for ORCA_R1''' . nn_ahm_ijk_t must be set to -20 or -30 for ORCA2 and ORCA1 (read in a file) [[BR]]- both laplacian and bi-laplacian coef. are always 3D arrays defined at T- and F- points. Bi-laplacian eddy coefficient defined as SQRT(bhm) [[BR]]''' ====>>> TO BE DONE: explore the possibility of u- and v-points'''[[BR]]- redesign of space variation of the eddy viscosity: suppression of: ldfdyn_substitute.h90 ; ldfdyn_c1d.h90 , ldfdyn_c2d.h90 and ldfdyn_c3d.h90 (replaced by ldfc1d_c2d.F90, a module share with ldftra.F90) ; ldfdyn_oce.F90 (now included in ldfdyn.F90)[[BR]]- remove ldfdyn_smag.F90 (suppression of smagorinsky option) '''==>>> TO BE re-add in the new framework by someone...'''[[BR]]- suppression of key_esopa in traldf.F90[[BR]]- change in all standard namelist_cfg and 1_namelist_cfg''' ===>>> TO BE DONE'''161 [[BR]]- default value of the namelist: ''no operator chosen'': ln_dynldf_lap=dyndf_blp=0 No lateral diffusion applied on momentum '''===>>> check THAT'''[[BR]]- create the 2D and 3D ahtu and ahtv file for ORCA_R2 '''===>>> TO BE DONE for ORCA_R1''' . nn_ahm_ijk_t must be set to -20 or -30 for ORCA2 and ORCA1 (read in a file) [[BR]]- both laplacian and bi-laplacian coef. are always 3D arrays defined at T- and F- points. Bi-laplacian eddy coefficient defined as SQRT(bhm) [[BR]]''' ====>>> TO BE DONE: explore the possibility of u- and v-points'''[[BR]]- redesign of space variation of the eddy viscosity: suppression of: ldfdyn_substitute.h90 ; ldfdyn_c1d.h90 , ldfdyn_c2d.h90 and ldfdyn_c3d.h90 (replaced by ldfc1d_c2d.F90, a module share with ldftra.F90) ; ldfdyn_oce.F90 (now included in ldfdyn.F90)[[BR]]- remove ldfdyn_smag.F90 (suppression of smagorinsky option) '''==>>> TO BE re-add in the new framework by someone...'''[[BR]]- suppression of key_esopa in dynldf.F90[[BR]]- suppression of key_dynldf_c1d, key_dynldf_c2d, key_dynldf_c3d[[BR]]- change in all standard namelist_cfg and 1_namelist_cfg ''' ===>>> TO BE DONE''' 162 162 163 163 [[BR]]'''IV. Solve the pending issues''' 164 164 165 ''' (IV.1) ''' specification of eddy viscosity/diffusivity coefficients in case of grid-size dependency.[[BR]] Issue: define the grid-size dependency in such a way that does not require the Equator being inside the domain.[[BR]] Solution: 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[[BR]] and use this scalar to compute the grid-size dependency of the coefficients. [[BR]] ''' (IV.2) ''' 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: 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[[BR]] and use this scalar to compute the grid-size dependency of the coefficients. [[BR]] ''' (IV.3)'''Add a proper coding of Smagorinsky eddy viscosity and diffusivity165 ''' (IV.1) ''' specification of eddy viscosity/diffusivity coefficients in case of grid-size dependency.[[BR]] Issue: define the grid-size dependency in such a way that does not require the Equator being inside the domain.[[BR]] Solution: 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[[BR]] and use this scalar to compute the grid-size dependency of the coefficients. [[BR]] ''' (IV.2) ''' 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: 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[[BR]] and use this scalar to compute the grid-size dependency of the coefficients. [[BR]] ''' (IV.3)''' Add a proper coding of Smagorinsky eddy viscosity and diffusivity 166 166 167 167 ... … … 175 175 * test with SETTE (especially restartability and reproducibility ) 176 176 177 [[BR]] '''V. Finalize the simplification'''178 179 ''' (V.1) add''' in NEMOGCM/TOOLS directory a program that read a coordinates.nc file apply a reduction of scale factors in some straits, and create the associated extended coordinates file (coordinates_e1e2u_v.nc).[[BR]] ''' (V.2) create''' the extended coordinates files form ORCA 2°, 1°, and 0.5°. ===>>> Done for ORCA 2° and 1°, ''' 1/2° and 1/4° missing''' ...[[BR]] ''' (V.3) create''' in NEMOGCM/TOOLS directory a program that create the ORCA2 and ORCA1 eddy viscosity'''????'''177 [[BR]] ''' V. Finalize the simplification''' 178 179 ''' (V.1) add''' in NEMOGCM/TOOLS directory a program that read a coordinates.nc file apply a reduction of scale factors in some straits, and create the associated extended coordinates file (coordinates_e1e2u_v.nc).[[BR]] ''' (V.2) create''' the extended coordinates files form ORCA 2°, 1°, and 0.5°. ===>>> Done for ORCA 2° and 1°, ''' 1/2° and 1/4° missing''' ...[[BR]] ''' (V.3) create''' in NEMOGCM/TOOLS directory a program that create the ORCA2 and ORCA1 eddy viscosity''' ????''' 180 180 181 181 ...
