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ticket/1593_CNRS9_NOC3_LDF (diff) – NEMO

Changes between Version 33 and Version 34 of ticket/1593_CNRS9_NOC3_LDF


Ignore:
Timestamp:
2015-10-24T10:29:57+02:00 (8 years ago)
Author:
gm
Comment:

--

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  • ticket/1593_CNRS9_NOC3_LDF

    v33 v34  
    2323Three steps: [[BR]] 
    2424 
    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)''' 
    2626 
    2727'''   (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 
     
    2929'''   (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]''' 
    3030 
    31   '''            [[BR]]            [[BR]]            II. Phasing of the advective/diffusive trends on tracers''' 
     31  '''             [[BR]]             [[BR]]             II. Phasing of the advective/diffusive trends on tracers''' 
    3232 
    3333'''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''' 
     
    123123 * 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_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 
    124124 
    125   '''             [[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=5737 5777]     & [https://forge.ipsl.jussieu.fr/nemo/log/branches/2015/dev_r5721_CNRS9_NOC3_LDF?rev=5737 5778]     and   [https://forge.ipsl.jussieu.fr/nemo/log/branches/2015/dev_r5721_CNRS9_NOC3_LDF?rev=5737 5782]     with SETTE OK''' 
     125  '''              [[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=5737 5777]      & [https://forge.ipsl.jussieu.fr/nemo/log/branches/2015/dev_r5721_CNRS9_NOC3_LDF?rev=5737 5778]      and   [https://forge.ipsl.jussieu.fr/nemo/log/branches/2015/dev_r5721_CNRS9_NOC3_LDF?rev=5737 5782]      with SETTE OK''' 
    126126 
    127127'''III.1 —''' '''LDF on dynamics'''  - viscous trends 
     
    191191[[BR]]'''         IV. Pending issues : need to be solved before v3.7 release''' 
    192192 
    193 '''(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: [[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. [[BR]]In addition:[[BR]]- '''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]]- '''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]]'''- '''explore''' the possibility of defining ahm coef. at u- and v-points.  This will improve the velocity dependent case. 
    194  
    195 '''(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: [[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. 
    196  
    197   '''   V. Pending issues : to be solved in 2016 ?''' 
     193'''•''' remove key_noslip_accurate from dom_oce.F90 and domsk.F90. 
     194 
     195'''•''' Update the documentation. 
     196 
     197'''•''' ensure the restartability & reproducibility for triad operator. 
     198 
     199'''• '''                                           specification of eddy viscosity/diffusivity coefficients in case of grid-size dependency. 
     200 
     201Issue:  define the grid-size dependency in such a way that does not require the Equator being inside the domain.[[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. [[BR]]In addition:[[BR]]- '''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]]- '''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]]'''- '''explore''' the possibility of defining ahm coef. at u- and v-points.  This will improve the velocity dependent case. 
     202 
     203'''• '''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. 
     204 
     205  '''[[BR]]    [[BR]]V. Pending issues : to be solved in 2016 ?''' 
    198206 
    199207'''(V.1)''' Add a proper coding of Smagorinsky eddy viscosity and diffusivity... 
     
    201209'''(V.2)''' It should be possible to remove hdivn ... think about that 
    202210 
    203   [[BR]]     '''   Next Step :''' 
     211  [[BR]]      '''    Next Step :''' 
    204212 
    205213Starting from this branch, another branch is created ('''given the name here''') which will contain the following item (random order):