% Appendix: List of symbols \chapter{List of symbols} \section*{Greek Symbols} \begin{flushleft} \begin{tabular}{lll} Symbol & Units & Meaning \\ \hline $\alpha$ & & thermal expansion coefficient \\ $\beta$ & & haline contraction coefficient \\ $\theta$ & & potential temperature \\ $\theta_2$ & & potential temperature referenced to 2000\,dbar \\ $\overline{\Delta\theta}$&& mean potential temperature deficit \\ $\theta_z$ & & vertical potential temperature gradient \\ $\rho$ & & density \\ $\rho_0$ & & reference density \\ $\rho_b$ & & density of background water column \\ $\rho_i$ & & asymptotic hydrothermal source-fluid density \\ $\rho_k$ & & individual density measurement\\ $\sigma$ & & standard deviation \\ $\sigma_2$ & & potential density referenced to 2000\,dbar \\ $\sigma_\theta$ & & potential density referenced to the surface \\ $\sigma$ & & standard deviation of along-mean flow \\ $\omega$ & & frequency \\ \end{tabular} \end{flushleft} \section*{Latin Symbols} \begin{flushleft} \begin{tabular}{lll} Symbol & Units & Meaning \\ \hline%---------------------------------------------------------------------- $A$ & & regression coefficient of bilinear method \\ $B$ & & regression coefficient of bilinear method \\ $B_i$ & & hydrothermal source buoyancy flux \\ $C$ & & regression coefficient of bilinear method \\ $c_p$ & & specific heat \\ $f$ & & Coriolis parameter ( at 48$^\circ$N) \\ %$\NhU$ & & topographic blocking parameter \\ $k_v$ & & diapycnal diffusivity \\ $N$ && buoyancy frequency \\ $Q$ && volume flux \\ $Q_e$ & & equilibrium-plume volume flux \\ $Q_i$ & & hydrothermal source volume flux \\ $R_r$ && water-column stability ratio \\ $R_i$ && hydrothermal source density-anomaly ratio \\ $Ro$ && Rossby number \\ $S$ & psu & salinity \\ $\Delta_\rho S$ & psu & isopycnal salinity anomaly \\ $\Delta_z S$ & psu & level salinity anomaly \\ $S_z$ & psu/m & vertical salinity gradient \\ $T$ & $^\circ$C & temperature \\ $\Delta_\rho\theta$ & $^\circ$C & isopycnal potential temperature anomaly \\ $\Delta_S\theta$ & $^\circ$C & isohaline potential temperature anomaly \\ $\Delta_z\theta$ & $^\circ$C & level potential temperature anomaly \\ $U$ & m/s & horizontal velocity \\ $\overline{U}$ & m/s & mean horizontal velocity \\ $W$ & m/s & vertical velocity \\ $X$ & m & $x$ coordinate or lateral distance \\ $z^*$ & m & maximum plume rise height \\ $z_0$ & m & reference depth \\ \end{tabular} \end{flushleft