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%                    L O S _ L T R . T E X 
%                    doc: Tue Feb 29 17:54:55 2000
%                    dlm: Wed Dec  6 13:50:59 2000
%                    (c) 2000 A.M. Thurnherr
%                    uE-Info: 113 0 NIL 0 0 72 2 2 4 ofnI
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\section*{Greek Symbols}

\begin{flushleft}
\begin{tabular}{lll}
Symbol 	& Units & Meaning \\ \hline
$\alpha$		& \pdegC{}	& thermal expansion coefficient (general) \\
$\alpha_0$		& \pdegC{}	& thermal expansion coefficient (linear equation of state) \\
$\beta$			& \ppsu{}	& haline contraction coefficient (general) \\
$\beta_0$		& \ppsu{}	& haline contraction coefficient (linear equation of state) \\
$\gamma$		&			& rift-valley topographic slope\prs{gamma} \\
$\epsilon$		& \mmpss{}	& error variance of along-mean flow\prs{epsilon} \\
$\theta$		& \degC{}	& potential temperature \\
$\overline{\Delta\theta}$	& \degC{}	& mean potential temperature deficit\prs{mdt} \\
$\theta_2$		& \degC{}	& potential temperature referenced to \dbar{2000} \\
$\Delta\theta_e$ & \degC{}	& equilibrium-plume temperature anomaly\prs{De} \\
$\De{\theta}$	& \degC{}	& mean equilibrium-plume temperature anomaly (c.f.\ $\Delta_\rho T$)\prs{Debar} \\
$\Di{\theta}$	& \degC{}	& mean hydrothermal source temperature anomaly\prs{Dibar} \\
$\theta_z$		& \degCpm{}	& vertical potential temperature gradient \\
\dsym{Bgamma}{\kappa} &		& model parameter for outflow across multiple sills\prs{Bgamma} \\
$\Lambda$		&			& bulk-plume entrainment coefficient\prs{Lambda} \\
$\lambda$ 		& \m{} 		& horizontal wave length \\
$\mu$			&			& mean \\
\end{tabular}

\begin{tabular}{lll}
Symbol 	& Units & Meaning \\ \hline
$\rho$			& \kgpmmm{}	& density \\
$\rho_0$		& \kgpmmm{}	& reference density \\
$\rho_b$		& \kgpmmm{}	& density of background water column\prs{rho_b} \\
$\rho_i$		& \kgpmmm{}	& asymptotic hydrothermal source-fluid density\prs{rho_i} \\
$\rho_k$		& \kgpmmm{}	& individual density measurement\prs{rho_k} \\
$\sigma$  		&			& standard deviation \\
\SigmaTwo 		& \kgpmmm{} & potential density referenced to \dbar{2000} \\
\SigmaTheta 	& \kgpmmm{} & potential density referenced to the surface \\
$\sigma_l$		& \mps{}	& standard deviation of along-mean flow\prs{sigmal} \\
$\sigma_x$		& \mps{}	& standard deviation of cross-mean flow\prs{sigmax} \\
\dsym{Btau}{\tau}& \d{} 	& analytic model solution time scale\prs{Btau} \\
$\tau_l$  		& \d{}		& integral time scale of along-mean flow\prs{taul} \\
$\chi^2$		&			& chi-squared merit function\prs{chisq} \\
$\omega$  		& \ps{}		& frequency \\
\end{tabular}
\end{flushleft}

\section*{Latin Symbols}

\begin{flushleft}
\begin{tabular}{lll}
Symbol 	& Units & Meaning \\
\hline%----------------------------------------------------------------------
$A$				& \degC{}	& regression coefficient of bilinear method\prs{bilin_A} \\
\dsym{BAisopycnal}{A_\rho} & \mm{} & area of isopycnal surface\prs{BAisopycnal} \\
$B$				& \degCmmmpkg{} & regression coefficient of bilinear method\prs{bilin_B} \\
$B_i$			& \mmmmpsss{}	& hydrothermal source buoyancy flux\prs{B_i} \\
$C$				& \degCpV{} & regression coefficient of bilinear method\prs{bilin_C} \\
$C_d$			& 			& drag coefficient\prs{Cd} \\
$C_r$			&			& rotary coefficient\prs{Cr} \\
$c_p$			& \JpkgpK{}	& specific heat \\
\dsym{Bd}{d}	& \m{}		& depth of model basin\prs{Bd} \\
$E$				& 			& cross-valley section\prs{E} \\
$f$				& \ps{}		& Coriolis parameter (\ps*{8.6}{-5} at \degN{36}) \\
\end{tabular}

\begin{tabular}{lll}
Symbol 	& Units & Meaning \\ \hline
$\NhU$ 			& 			& topographic blocking parameter\prs{NhU} \\
\dsym{gp}{g'}	& \mpss{} 	& reduced gravity \\
\dsym{BHc}{H_c} & \W{} 		& conductive geothermal heat flux\prs{BHc} \\
\dsym{BHp}{H_p} & \W{} 		& convective geothermal heat flux\prs{BHp} \\
\dsym{Bh}{h}	&	\m{}	& vertical length scale \\
				&	\m{}	& in \rchapNP{BOF}: model interface height above outflow sill\prs{Bh} \\
\dsym{Bhzero}{h_0} & \m{}	& model interface height initial condition\prs{Bhzero} \\
$h_b$			&	\m{}	& obstacle height\prs{hb} \\
\dsym{Bheq}{h_\mathit{eq}}& \m{} & model-interface equilibrium height\prs{Bheq} \\
\dsym{hu}{h_u}	&	\m{}	& upstream interface height of hydraulic calculation\prs{hu} \\
\dsym{Kv}{K_v}	  & \mmps{} & diapycnal diffusivity \\
$k_l$	 		&	\Pm{}	& along-slope wave number\prs{kl} \\
$k_x$	 		&	\Pm{}	& cross-slope wave number\prs{kx} \\
\dsym{Bl}{l}	& 	\m{} 	& horizontal length scale \\
				& 	\m{}	& in \rchapNP{BOF}: length of model basin\prs{Bl} \\
$N$				&	\ps{}	& buoyancy frequency \\
$N_i$			&	\ps{}	& buoyancy frequency upstream of obstacle\prs{Ni} \\
$\Delta n$		& \V{}		& nephelometry anomaly \\
$\Delta_r n$	& \V{}		& residual nephelometry anomaly\prs{Drn} \\
$\Delta n^*$	& \V{}		& peak value of Gaussian nephelometry plume\prs{Delta_n_star} \\
$P$				&			& sill friction parameter\prs{P} \\
$Q$				& \mmmps{}	& volume flux \\
$Q_e$			& \mmmps{}	& equilibrium-plume volume flux\prs{Q_e} \\
\dsym{BQi}{Q_i}	& \mmmps{}	& hydrothermal source volume flux\prs{Q_i} \\
				& \mmps{} 	& in \rchapNP{BOF}: model inflow (forcing term)\prs{BQi} \\
\dsym{Qi}{Q^*_i}& \mmmps{} 	& observed inflow into segment\prs{Qi} \\
\dsym{BQo}{Q_o}	& \mmps{} 	& model outflow\prs{BQo} \\
\dsym{Qo}{Q^*_o}& \mmmps{} 	& observed outflow from segment\prs{Qo} \\
\dsym{BQu}{Q_u}	& \mmps{} 	& volume flux across model interface\prs{BQu} \\
\end{tabular}

%\newpage\vspace*{-\baselineskip}
\begin{tabular}{lll}
Symbol 	& Units & Meaning \\
\hline%----------------------------------------------------------------------
\Rr				&			& water-column stability ratio\prs{Rr} \\
\Ri				& 			& hydrothermal source density-anomaly ratio\prs{Ri} \\
$\Ro$			&			& Rossby number\prs{Ro} \\
$r$				& 			& correlation coefficient of linear regression \\
$r_{BC}$		& 			& cross-correlation coefficient of bilinear method\prs{r_BC} \\
$S$				& \psu{}   	& salinity \\
$\Di{S}$ 		& \psu{}	& mean hydrothermal source salinity anomaly\prs{Sibar} \\
$\Delta_\rho S$	& \psu{}	& isopycnal salinity anomaly\prs{DrhoS} \\
$S_+$			& \mmpss{} & anticlockwise-polarized flow spectral energy\prs{Sp} \\
$S_-$			& \mmpss{} & clockwise-polarized flow spectral energy\prs{Sm} \\
$S_0$			& \psu{}   & reference salinity \\
$S_b$			& \psu{}   & salinity of background water column \\
$S_z$			& \psupm{} & vertical salinity gradient \\
\dsym{Bs}{s}	& 			& analytic model solution\prs{Bs} \\
\dsym{Bsp}{s'}	& 			& analytic model solution\prs{Bsp} \\
$T$				& \degC{}	& temperature \\
$\Delta_\rho T$	& \degC{}	& isopycnal temperature anomaly (c.f.\ $\De{\theta}$)\prs{DrhoT} \\
$\Delta_S T$		& \degC{}	& isohaline temperature anomaly\prs{DST} \\
$T_0$			& \degC{}	& reference temperature \\
$T_r$			& \d{}		& current-meter record length\prs{Tr} \\
$U$				& \mps{} 	& horizontal velocity \\
$\overline{U}$	& \mps{} 	& mean horizontal velocity \\
$U_0$			& \mps{}	& reference velocity \\
$U_i$			& \mps{} 	& velocity upstream of obstacle\prs{Ui} \\
$U_n$			& \mps{}	& equilibrium-plume advection velocity\prs{U_n} \\
$W$				& \mps{}	& vertical velocity \\
\dsym{Bw}{w}	& \m{}		& width of hydraulic overflow current\prs{w} \\
				& \m{}		& in \rchapNP{BOF}: model-basin width\prs{Bw} \\
$X$				& \mm{}		& cross-sectional area of time-averaged buoyant plume\prs{X} \\
$z^*$			& \m{}		& maximum plume rise height\prs{zstar} \\
$z_0$			& \m{}		& reference depth \\
\end{tabular}

\end{flushleft}
