Changes between Version 10 and Version 11 of ticket/1593_CNRS9_NOC3_LDF
- Timestamp:
- 2015-09-16T12:26:24+02:00 (9 years ago)
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ticket/1593_CNRS9_NOC3_LDF
v10 v11 23 23 Three steps: 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] ''')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] ''' ) 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. 30 30 31 ''' II. Phasing of the advective/diffusive trends on tracers'''31 ''' II. Phasing of the advective/diffusive trends on tracers''' 32 32 33 ''' (II.1)''' ... 33 ''' (II.1)''' ...Diffusive trends : [[BR]]- 34 34 35 ''' III. Phasing of viscous trends''' 35 '''(II.1)''' ...Diffusive trends : 36 37 '''(II.X)''' ..Miscellaneous : [[BR]]- 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) 38 39 : 40 41 ''' III. Phasing of viscous trends''' 36 42 37 43 ''' (III.1)''' … … 39 45 ... 40 46 41 ''' IV. Solve the pending issues'''47 ''' IV. Solve the pending issues''' 42 48 43 ''' (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. 44 '''(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. 49 ''' (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. ''' (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. 45 50 46 51 ... 47 52 48 ''' V. Finalize the simplification'''53 ''' V. Finalize the simplification''' 49 54 50 ''' (V.1) '''suppression of hard coded reduction of scale factor in some straits for some given ORCA configuration.[[BR]]'''add''' in NEMOGCM/TOOLS a 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°.55 ''' (V.1) ''' suppression of hard coded reduction of scale factor in some straits for some given ORCA configuration.[[BR]] ''' add''' in NEMOGCM/TOOLS a 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°. 51 56 52 57 ... 53 58 54 59 ---- 55 [[BR]]56 60 ---- 57 61 '''To be CHECKED''' (not necessary associated with this branch
