New URL for NEMO forge!   http://forge.nemo-ocean.eu

Since March 2022 along with NEMO 4.2 release, the code development moved to a self-hosted GitLab.
This present forge is now archived and remained online for history.
Changeset 8882 for branches/2017/dev_CNRS_2017/DOC/Namelists/namzdf_tke – NEMO

Ignore:
Timestamp:
2017-12-01T18:44:09+01:00 (6 years ago)
Author:
flavoni
Message:

dev_CNRS_2017 branch: merged dev_r7881_ENHANCE09_RK3 with trunk r8864

File:
1 edited

Legend:

Unmodified
Added
Removed
  • branches/2017/dev_CNRS_2017/DOC/Namelists/namzdf_tke

    r6997 r8882  
    11!----------------------------------------------------------------------- 
    2 &namzdf_tke    !   turbulent eddy kinetic dependent vertical diffusion  ("key_zdftke") 
     2&namzdf_tke    !   turbulent eddy kinetic dependent vertical diffusion  (ln_zdftke =T) 
    33!----------------------------------------------------------------------- 
    44   rn_ediff    =   0.1     !  coef. for vertical eddy coef. (avt=rn_ediff*mxl*sqrt(e) ) 
     
    88   rn_emin0    =   1.e-4   !  surface minimum value of tke [m2/s2] 
    99   rn_bshear   =   1.e-20  ! background shear (>0) currently a numerical threshold (do not change it) 
     10   nn_pdl      =   1       !  Prandtl number function of richarson number (=1, avt=pdl(Ri)*avm) or not (=0, avt=avm) 
    1011   nn_mxl      =   2       !  mixing length: = 0 bounded by the distance to surface and bottom 
    11                            !                 = 1 bounded by the local vertical scale factor 
    12                            !                 = 2 first vertical derivative of mixing length bounded by 1 
    13                            !                 = 3 as =2 with distinct disspipative an mixing length scale 
    14    nn_pdl      =   1       !  Prandtl number function of richarson number (=1, avt=pdl(Ri)*avm) or not (=0, avt=avm) 
     12   !                       !                 = 1 bounded by the local vertical scale factor 
     13   !                       !                 = 2 first vertical derivative of mixing length bounded by 1 
     14   !                       !                 = 3 as =2 with distinct disspipative an mixing length scale 
    1515   ln_mxl0     = .true.    !  surface mixing length scale = F(wind stress) (T) or not (F) 
    1616   rn_mxl0     =   0.04    !  surface  buoyancy lenght scale minimum value 
     17   ln_drg      = .false.   !  top/bottom friction added as boundary condition of TKE 
    1718   ln_lc       = .true.    !  Langmuir cell parameterisation (Axell 2002) 
    18    rn_lc       =   0.15    !  coef. associated to Langmuir cells 
    19    nn_etau     =   1       !  penetration of tke below the mixed layer (ML) due to near intertial waves 
    20                            !        = 0 no penetration 
    21                            !        = 1 add a tke source below the ML 
    22                            !        = 2 add a tke source just at the base of the ML 
    23                            !        = 3 as = 1 applied on HF part of the stress           (ln_cpl=T) 
    24    rn_efr      =   0.05    !  fraction of surface tke value which penetrates below the ML (nn_etau=1 or 2) 
    25    nn_htau     =   1       !  type of exponential decrease of tke penetration below the ML 
    26                            !        = 0  constant 10 m length scale 
    27                            !        = 1  0.5m at the equator to 30m poleward of 40 degrees 
     19      rn_lc       =   0.15    !  coef. associated to Langmuir cells 
     20   nn_etau     =   1       !  penetration of tke below the mixed layer (ML) due to NIWs 
     21                              !        = 0 none ; = 1 add a tke source below the ML 
     22                              !        = 2 add a tke source just at the base of the ML 
     23                              !        = 3 as = 1 applied on HF part of the stress           (ln_cpl=T) 
     24      rn_efr      =   0.05    !  fraction of surface tke value which penetrates below the ML (nn_etau=1 or 2) 
     25      nn_htau     =   1       !  type of exponential decrease of tke penetration below the ML 
     26                              !        = 0  constant 10 m length scale 
     27                              !        = 1  0.5m at the equator to 30m poleward of 40 degrees 
    2828/ 
Note: See TracChangeset for help on using the changeset viewer.