Changes between Version 39 and Version 40 of doc/app/parlist


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Timestamp:
Sep 13, 2010 2:21:36 PM (15 years ago)
Author:
herbort
Comment:

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  • doc/app/parlist

    v39 v40  
    1919|| [../parpar#bc_par_ns bc_par_ns] || P || bc || C*15 || 'cyclic' || Lateral boundary condition (y-direction) for particle transport. ||
    2020|| [../parpar#bc_par_t bc_par_t] || P || bc || C*15 || 'absorb' || Top boundary condition for particle transport. ||
    21 || [../inipar#bc_pt_b] || I || bc || C*20 || '' ||  ||
     21|| [../inipar#bc_pt_b bc_pt_b] || I || bc || C*20 || 'dirichlet' || Bottom boundary condition of the potential temperature. ||
     22|| [../inipar#bc_pt_t bc_pt_t] || I || bc || C*20 || 'initial_gradient' || Top boundary condition of the potential temperature. ||
     23|| [../inipar#bc_q_b bc_q_b] || I || bc || C*20 || 'dirichlet' || Bottom boundary condition of the specific humidity / total water content.  ||
     24|| [../inipar#bc_q_t bc_q_t] || I || bc || C*20 || 'neumann' || Top boundary condition of the specific humidity / total water content. ||
     25|| [../inipar#bc_s_b bc_s_b] || I || bc || C*20 || 'dirichlet' || Bottom boundary condition of the scalar concentration.  ||
     26|| [../inipar#bc_s_t bc_st] || I || bc || C*20 || 'neumann' || Top boundary condition of the scalar concentration.  ||
     27|| [../inipar#bc_sa_t bc_sa_t] || I || bc || C*20 || 'neumann' || Top boundary condition of the salinity.  ||
     28|| [../inipar#bc_uv_t bc_uv_t] || I || bc || C*20 || 'dirichlet' || Bottom boundary condition of the horizontal wind components u and v. ||
    2229|| [../inipar#] ||  ||  ||  ||  ||  ||
    2330|| [../inipar#] ||  ||  ||  ||  ||  ||
    2431|| [../inipar#] ||  ||  ||  ||  ||  ||
    2532|| [../inipar#] ||  ||  ||  ||  ||  ||
     33