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Changeset 15009 – NEMO

Changeset 15009


Ignore:
Timestamp:
2021-06-17T13:06:44+02:00 (3 years ago)
Author:
amoulin
Message:

typo errors in the MANUAL updates for wave-current interaction -ticket #2613

Location:
NEMO/branches/2021/dev_r14886_VLD-03_Aimie_Moulin_Wave_Coupling_TestCase/doc
Files:
2 edited

Legend:

Unmodified
Added
Removed
  • NEMO/branches/2021/dev_r14886_VLD-03_Aimie_Moulin_Wave_Coupling_TestCase/doc/latex/NEMO/subfiles/chap_SBC.tex

    r14968 r15009  
    15731573Ocean waves represent the interface between the ocean and the atmosphere, so \NEMO\ is extended to incorporate 
    15741574physical processes related to ocean surface waves, namely the surface stress modified by growth and 
    1575 dissipation of the oceanic wave field, the Stokes-Coriolis force, the vortex-force, the Bernoulli head J term and the Stokes drift impact on mass and tracer advection; moreover the neutral surface drag coefficient or the Charnock parameter from a wave model can be used to evaluate the wind stress. NEMO has also been extended to take into account the impact of surface waves on the vertical mixing, via the parameterization of the Langmuir turbulence, the modification of the surface boundary conditions for the Turbulent Kinetic Energy closure scheme, and the inclusion the Stokes drift contribution to the shear production term in different turbulent closure schemes (RIC, TKE, GLS).\\ 
     1575dissipation of the oceanic wave field, the Stokes-Coriolis force, the vortex-force, the Bernoulli head $J$ term and the Stokes drift impact on mass and tracer advection; moreover the neutral surface drag coefficient or the Charnock parameter from a wave model can be used to evaluate the wind stress. NEMO has also been extended to take into account the impact of surface waves on the vertical mixing, via the parameterization of the Langmuir turbulence, the modification of the surface boundary conditions for the Turbulent Kinetic Energy closure scheme, and the inclusion of the Stokes drift contribution to the shear production term in different turbulent closure schemes (RIC, TKE, GLS).\\ 
    15761576 
    15771577Physical processes related to ocean surface waves can be accounted by setting the logical variable 
     
    16441644 
    16451645\begin{description} 
    1646 \item [By default (\forcode{ln_breivikFV_2016=.true.})]:\\  
     1646\item [By default (\forcode{ln_breivikFV_2016=.false.})]:\\  
    16471647An exponential integral profile parameterization proposed by \citet{breivik.janssen.ea_JPO14} is used: 
    16481648 
  • NEMO/branches/2021/dev_r14886_VLD-03_Aimie_Moulin_Wave_Coupling_TestCase/doc/namelists/namsbc_cpl

    r14968 r15009  
    4848   sn_rcv_isf    =   'none'                 ,    'no'    ,     ''      ,         ''           ,   '' 
    4949   sn_rcv_icb    =   'none'                 ,    'no'    ,     ''      ,         ''           ,   '' 
    50    sn_rcv_wdrag  =   'none'                 ,    'no'    ,     ''      ,         ''           ,   '' 
    5150   sn_rcv_charn  =   'none'                 ,    'no'    ,     ''      ,         ''           ,   '' 
    5251   sn_rcv_taw    =   'none'                 ,    'no'    ,     ''      ,         ''           ,   'U,V' 
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