Newer
Older
!-----------------------------------------------------------------------
&namzdf_gls ! GLS vertical diffusion (ln_zdfgls =T)
!-----------------------------------------------------------------------
rn_emin = 1.e-7 ! minimum value of e [m2/s2]
rn_epsmin = 1.e-12 ! minimum value of eps [m2/s3]
ln_length_lim = .true. ! limit on the dissipation rate under stable stratification (Galperin et al., 1988)
rn_clim_galp = 0.267 ! galperin limit
ln_sigpsi = .true. ! Activate or not Burchard 2001 mods on psi schmidt number in the wb case
rn_crban = 100. ! Craig and Banner 1994 constant for wb tke flux
rn_charn = 70000. ! Charnock constant for wb induced roughness length
rn_hsro = 0.02 ! Minimum surface roughness
rn_hsri = 0.03 ! Ice-ocean roughness
rn_frac_hs = 1.3 ! Fraction of wave height as roughness (if nn_z0_met>1)
nn_z0_met = 2 ! Method for surface roughness computation (0/1/2/3)
! ! = 3 requires ln_wave=T
nn_z0_ice = 1 ! attenutaion of surface wave breaking under ice
! ! = 0 no impact of ice cover
! ! = 1 roughness uses rn_hsri and is weigthed by 1-TANH(10*fr_i)
! ! = 2 roughness uses rn_hsri and is weighted by 1-fr_i
! ! = 3 roughness uses rn_hsri and is weighted by 1-MIN(1,4*fr_i)
nn_mxlice = 1 ! mixing under sea ice
! = 0 No scaling under sea-ice
! = 1 scaling with constant Ice-ocean roughness (rn_hsri)
! = 2 scaling with mean sea-ice thickness
! = 3 scaling with max sea-ice thickness
nn_bc_surf = 1 ! surface condition (0/1=Dir/Neum)
nn_bc_bot = 1 ! bottom condition (0/1=Dir/Neum)
nn_stab_func = 2 ! stability function (0=Galp, 1= KC94, 2=CanutoA, 3=CanutoB)
nn_clos = 1 ! predefined closure type (0=MY82, 1=k-eps, 2=k-w, 3=Gen)
/