| ... | ... | @@ -172,8 +172,7 @@ Setup file has the same format, as the driver file. The list of parameters is gi |
|
|
|
| Keyword | Description and acceptable values set |
|
|
|
|
|:---------------|:-----------------------------------------------------------|
|
|
|
|
|*varalb* | Water albedo: 0 - constant, 1 - zenith-angle dependent |
|
|
|
|
|*PBLpar* | Surface fluxes scheme: -1 - sensible, latent heat and momentum fluxes are given as input for the model; 0 - the latent heat flux is set to zero, while sensible heat and momentum fluxes are constant in time, specified by *sensflux0* and *momflux0*; 1 - Businger-Dayer formulas (Monin-Obukhov theory) for exchange coefficients, the code from INM RAS climate model; 2 - formulation from NH3d (Louis, 1979); 3 - formulation from FLake;
|
|
|
|
4 - formulation implemented by D.Chechin |
|
|
|
|
|*PBLpar* | Surface fluxes scheme: -1 - sensible, latent heat and momentum fluxes are given as input for the model; 0 - the latent heat flux is set to zero, while sensible heat and momentum fluxes are constant in time, specified by *sensflux0* and *momflux0*; 1 - Businger-Dayer formulas (Monin-Obukhov theory) for exchange coefficients, the code from INM RAS climate model; 2 - formulation from NH3d (Louis, 1979); 3 - formulation from FLake; 4 - formulation implemented by D.Chechin |
|
|
|
|
|*waveenh* | The shallow water correction of surface fluxes (Panin et al., 1996) (0 - off, 1 - on) |
|
|
|
|
|*momflxpart* | Momentum flux treatment: 0 - all momentum flux from the atmosphere is consumed by currents acceleration; 2 - momentum flux from the atmosphere is partitioned between wave development (controlled by fetch) and currents acceleration (Stepanenko et al., 2014) |
|
|
|
|
|*c_d* | The momentum exchange coefficient, n/d; if -999, momentum flux is calculated by surface flux scheme |
|
| ... | ... | @@ -201,12 +200,10 @@ Setup file has the same format, as the driver file. The list of parameters is gi |
|
|
|
|*botfric* | The law for friction at the sloping bottom: 0 - no bottom friction, 1 - linear friction, 2 - quadratic friction |
|
|
|
|
|*horvisc* | Horizontal viscosity, m^2/s, used to damp the 1-st horizontal ve-
|
|
|
|
locity mode |
|
|
|
|
|*backdiff* | Switch for background diffusivity by Hondzo and Stefan (1993); 1
|
|
|
|
– off, 1 – on |
|
|
|
|
|*backdiff* | Switch for background diffusivity by Hondzo and Stefan (1993); 1 – off, 1 – on |
|
|
|
|
|*nManning* | Manning’s coefficient, relevant for dyn_pgrad =5 |
|
|
|
|
|*zero_model* | Switch for zero-dimensional model: 0 -off, 1 - on |
|
|
|
|
|
|
|
|
|
*thermokarst_meth_prod* | Switch for old organics methane production under thermokarst lakes: 1. - on, 0. - off |
|
|
|
|
|*thermokarst_meth_prod* | Switch for old organics methane production under thermokarst lakes: 1. - on, 0. - off |
|
|
|
|
|*soil_meth_prod* | Switch for new organics methane production under lakes: 1. - on, 0. - off |
|
|
|
|
|*outflpar* | The treatment of effluent temperature: 0 - value at the outflow = cross-section mean; 1 - the cross-section mean = 0.5*(inflow value + outflow value); 2 - variables at the outflow are calculated using Lagrangian approach |
|
|
|
|
|*sensflux0* | Sensible heat flux upwards, constant in time (relevant if PBLpar = 0), W/m^2 |
|
| ... | ... | |
