Changeset 14062 for NEMO/branches/2020/dev_r13333_KERNEL-08_techene_gm_HPG_SPG/cfgs/SHARED/namelist_ref
- Timestamp:
- 2020-12-03T17:39:30+01:00 (3 years ago)
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- 1 edited
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NEMO/branches/2020/dev_r13333_KERNEL-08_techene_gm_HPG_SPG/cfgs/SHARED/namelist_ref
r14044 r14062 998 998 ln_dynvor_eeT = .false. ! energy conserving scheme (een using e3t) 999 999 ln_dynvor_een = .false. ! energy & enstrophy scheme 1000 nn_een_e3f = 0 ! =0 e3f = mi(mj(e3t))/4 1001 ! ! =1 e3f = mi(mj(e3t))/mi(mj( tmask)) 1000 ! 1002 1001 ln_dynvor_msk = .false. ! vorticity multiplied by fmask (=T) ==>>> PLEASE DO NOT ACTIVATE 1003 ! ! (f-point vorticity schemes only) 1002 ! ! (f-point vorticity schemes only) 1003 ! 1004 nn_e3f_typ = 0 ! type of e3f (EEN, ENE, ENS, MIX only) =0 e3f = mi(mj(e3t))/4 1005 ! ! =1 e3f = mi(mj(e3t))/mi(mj( tmask)) 1004 1006 / 1005 1007 !----------------------------------------------------------------------- … … 1011 1013 ln_hpg_isf = .false. ! s-coordinate (sco ) adapted to isf 1012 1014 ln_hpg_djc = .false. ! s-coordinate (Density Jacobian with Cubic polynomial) 1015 ln_hpg_djc_vnh = .true. ! hor. bc type for djc scheme (T=von Neumann, F=linear extrapolation) 1016 ln_hpg_djc_vnv = .true. ! vert. bc type for djc scheme (T=von Neumann, F=linear extrapolation) 1013 1017 ln_hpg_prj = .false. ! s-coordinate (Pressure Jacobian scheme) 1014 1018 / … … 1033 1037 ! ! Type of the operator : 1034 1038 ln_dynldf_OFF = .false. ! No operator (i.e. no explicit diffusion) 1039 nn_dynldf_typ = 0 ! =0 div-rot (default) ; =1 symmetric 1035 1040 ln_dynldf_lap = .false. ! laplacian operator 1036 1041 ln_dynldf_blp = .false. ! bilaplacian operator … … 1163 1168 ln_mxl0 = .true. ! surface mixing length scale = F(wind stress) (T) or not (F) 1164 1169 nn_mxlice = 2 ! type of scaling under sea-ice 1165 1166 1167 1168 1170 ! ! = 0 no scaling under sea-ice 1171 ! ! = 1 scaling with constant sea-ice thickness 1172 ! ! = 2 scaling with mean sea-ice thickness ( only with SI3 sea-ice model ) 1173 ! ! = 3 scaling with maximum sea-ice thickness 1169 1174 rn_mxlice = 10. ! max constant ice thickness value when scaling under sea-ice ( nn_mxlice=1) 1170 1175 rn_mxl0 = 0.04 ! surface buoyancy lenght scale minimum value … … 1173 1178 rn_lc = 0.15 ! coef. associated to Langmuir cells 1174 1179 nn_etau = 1 ! penetration of tke below the mixed layer (ML) due to NIWs 1175 1176 1177 1180 ! ! = 0 none ; = 1 add a tke source below the ML 1181 ! ! = 2 add a tke source just at the base of the ML 1182 ! ! = 3 as = 1 applied on HF part of the stress (ln_cpl=T) 1178 1183 rn_efr = 0.05 ! fraction of surface tke value which penetrates below the ML (nn_etau=1 or 2) 1179 1184 nn_htau = 1 ! type of exponential decrease of tke penetration below the ML 1180 1181 1185 ! ! = 0 constant 10 m length scale 1186 ! ! = 1 0.5m at the equator to 30m poleward of 40 degrees 1182 1187 nn_eice = 1 ! attenutaion of langmuir & surface wave breaking under ice 1183 1188 ! ! = 0 no impact of ice cover on langmuir & surface wave breaking … … 1216 1221 &namzdf_osm ! OSM vertical diffusion (ln_zdfosm =T) 1217 1222 !----------------------------------------------------------------------- 1218 ln_use_osm_la = .false. ! Use namelistrn_osm_la1223 ln_use_osm_la = .false. ! Use rn_osm_la 1219 1224 rn_osm_la = 0.3 ! Turbulent Langmuir number 1220 rn_osm_dstokes = 5. ! Depth scale of Stokes drift (m) 1225 rn_zdfosm_adjust_sd = 1.0 ! Stokes drift reduction factor 1226 rn_osm_hblfrac = 0.1 ! specify top part of hbl for nn_osm_wave = 3 or 4 1227 rn_osm_bl_thresh = 5.e-5 !Threshold buoyancy for deepening of OSBL base 1221 1228 nn_ave = 0 ! choice of horizontal averaging on avt, avmu, avmv 1222 1229 ln_dia_osm = .true. ! output OSMOSIS-OBL variables … … 1226 1233 rn_difri = 0.005 ! max Ri# diffusivity at Ri_g = 0 (m^2/s) 1227 1234 ln_convmix = .true. ! Use convective instability mixing below BL 1228 rn_difconv = 1. ! diffusivity when unstable below BL (m2/s) 1235 rn_difconv = 1. !0.01 !1. ! diffusivity when unstable below BL (m2/s) 1236 rn_osm_dstokes = 5. ! Depth scale of Stokes drift (m) 1229 1237 nn_osm_wave = 0 ! Method used to calculate Stokes drift 1230 1238 ! ! = 2: Use ECMWF wave fields 1231 1239 ! ! = 1: Pierson Moskowitz wave spectrum 1232 1240 ! ! = 0: Constant La# = 0.3 1233 / 1241 nn_osm_SD_reduce = 0 ! Method used to get active Stokes drift from surface value 1242 ! ! = 0: No reduction 1243 ! = 1: use SD avged over top 10% hbl 1244 ! = 2:use surface value of SD fit to slope at rn_osm_hblfrac*hbl below surface 1245 ln_zdfosm_ice_shelter = .true. ! reduce surface SD and depth scale under ice 1246 ln_osm_mle = .false. ! Use integrated FK-OSM model 1247 / 1248 !----------------------------------------------------------------------- 1249 &namosm_mle ! mixed layer eddy parametrisation (Fox-Kemper) (default: OFF) 1250 !----------------------------------------------------------------------- 1251 rn_osm_mle_ce = 0.06 ! magnitude of the MLE (typical value: 0.06 to 0.08) 1252 nn_osm_mle = 0 ! MLE type: =0 standard Fox-Kemper ; =1 new formulation 1253 rn_osm_mle_lf = 5.e+3 ! typical scale of mixed layer front (meters) (case rn_osm_mle=0) 1254 rn_osm_mle_time = 172800. ! time scale for mixing momentum across the mixed layer (seconds) (case rn_osm_mle=0) 1255 rn_osm_mle_lat = 20. ! reference latitude (degrees) of MLE coef. (case rn_mle=1) 1256 rn_osm_mle_rho_c = 0.01 ! delta rho criterion used to calculate MLD for FK 1257 rn_osm_mle_thresh = 0.0005 ! delta b criterion used for FK MLE criterion 1258 rn_osm_mle_tau = 172800. ! time scale for FK-OSM (seconds) (case rn_osm_mle=0) 1259 ln_osm_hmle_limit = .false. ! limit hmle to rn_osm_hmle_limit*hbl 1260 rn_osm_hmle_limit = 1.2 1261 / 1234 1262 !----------------------------------------------------------------------- 1235 1263 &namzdf_mfc ! Mass Flux Convection … … 1374 1402 ln_sstnight = .false. ! Logical switch for calculating night-time average for SST obs 1375 1403 ln_bound_reject = .false. ! Logical to remove obs near boundaries in LAMs. 1404 ln_default_fp_indegs = .true. ! Logical: T=> averaging footprint is in degrees, F=> in metres 1376 1405 ln_sla_fp_indegs = .true. ! Logical for SLA: T=> averaging footprint is in degrees, F=> in metres 1377 1406 ln_sst_fp_indegs = .true. ! Logical for SST: T=> averaging footprint is in degrees, F=> in metres … … 1389 1418 cn_gridsearchfile ='gridsearch.nc' ! Grid search file name 1390 1419 rn_gridsearchres = 0.5 ! Grid search resolution 1420 rn_default_avglamscl = 0. ! Default E/W diameter of observation footprint (metres/degrees) 1421 rn_default_avgphiscl = 0. ! Default N/S diameter of observation footprint (metres/degrees) 1391 1422 rn_mdtcorr = 1.61 ! MDT correction 1392 1423 rn_mdtcutoff = 65.0 ! MDT cutoff for computed correction … … 1402 1433 rn_sic_avgphiscl = 0. ! N/S diameter of SIC observation footprint (metres/degrees) 1403 1434 nn_1dint = 0 ! Type of vertical interpolation method 1404 nn_2dint = 0! Default horizontal interpolation method1435 nn_2dint_default = 0 ! Default horizontal interpolation method 1405 1436 nn_2dint_sla = 0 ! Horizontal interpolation method for SLA 1406 1437 nn_2dint_sst = 0 ! Horizontal interpolation method for SST
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