- Timestamp:
- 2017-12-06T18:17:10+01:00 (7 years ago)
- File:
-
- 1 edited
Legend:
- Unmodified
- Added
- Removed
-
branches/2017/dev_CNRS_2017/NEMOGCM/CONFIG/SHARED/namelist_ref
r8881 r8930 875 875 ln_zdftke = .false. ! Turbulent Kinetic Energy closure (T => fill namzdf_tke) 876 876 ln_zdfgls = .false. ! Generic Length Scale closure (T => fill namzdf_gls) 877 ln_zdfosm = .false. ! OSMOSIS BL closure (T => fill namzdf_osm) 877 878 ! 878 879 ! ! convection … … 957 958 nn_stab_func = 2 ! stability function (0=Galp, 1= KC94, 2=CanutoA, 3=CanutoB) 958 959 nn_clos = 1 ! predefined closure type (0=MY82, 1=k-eps, 2=k-w, 3=Gen) 960 / 961 !----------------------------------------------------------------------- 962 &namzdf_osm ! OSM vertical diffusion (ln_zdfosm =T) 963 !----------------------------------------------------------------------- 964 ln_use_osm_la = .false. ! Use namelist rn_osm_la 965 rn_osm_la = 0.3 ! Turbulent Langmuir number 966 rn_osm_dstokes = 5. ! Depth scale of Stokes drift (m) 967 nn_ave = 0 ! choice of horizontal averaging on avt, avmu, avmv 968 ln_dia_osm = .true. ! output OSMOSIS-OBL variables 969 rn_osm_hbl0 = 10. ! initial hbl value 970 ln_kpprimix = .true. ! Use KPP-style Ri# mixing below BL 971 rn_riinfty = 0.7 ! Highest local Ri_g permitting shear instability 972 rn_difri = 0.005 ! max Ri# diffusivity at Ri_g = 0 (m^2/s) 973 ln_convmix = .true. ! Use convective instability mixing below BL 974 rn_difconv = 1. ! diffusivity when unstable below BL (m2/s) 975 nn_osm_wave = 0 ! Method used to calculate Stokes drift 976 ! = 2: Use ECMWF wave fields 977 ! = 1: Pierson Moskowitz wave spectrum 978 ! = 0: Constant La# = 0.3 959 979 / 960 980 !-----------------------------------------------------------------------
Note: See TracChangeset
for help on using the changeset viewer.