\emph{massflux}& The massflux parameterization of convection (Siebesma et al., 2007): 0 - off, 1 - on. \\
\hline
\emph{ifrad}& Radiation fluxes at the water surface: 0 - set to zero; 1 - full treatment \\
\emph{ifrad}& Radiation fluxes at the water surface: 0 - set to zero; 1 - full treatment of surface radiation budget \\
\hline
\emph{ifbubble}& Switch for the bubble model: 0 - off (bubbles do not change with depth); 1 - on \\
\hline
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@@ -379,9 +379,9 @@ give significant speedup \\
\emph{horvisc}& Horizontal viscosity, m$^2$/s, used to damp the 1-st horizontal velocity mode \\
\hline
\hline
\emph{backdiff}& Switch for background diffusivity by Hondzo and Stefan (1993); 1 -- off, 1 -- on \\
\emph{backdiff}& Switch for background diffusivity: 0 -- off, 1 -- background diffusivity by Hondzo and Stefan (1993); 2 -- background diffusivity from KPP model, based in Ri number, 3 -- constant background diffusivity\\
\hline
\emph{backdiff0}& A multiplier in background diffusivity expression by Hondzo and Stefan (1993), relevant if \emph{backdiff}=1; if \emph{backdiff0}$<$0., then a reference value from original paper is used \\
\emph{backdiff0}& A reference value in background diffusivity, m$^2$/s, expression by Hondzo and Stefan (1993) or KPP model, or a value of constant background diffusivity, relevant if \emph{backdiff}>0; if \emph{backdiff0}$<$0., then the reference values are used \\
\hline
\emph{nManning}& Manning's coefficient, relevant for \emph{dyn\_pgrad}=5 \\
