\begin{table}%t5
\caption{\label{5:table:out}Outflow properties of the red and blue outflow lobe.}
\par
%\centerline
{\small
\par
\begin{tabular}{l r c c c c c c}
\hline \hline
\multicolumn{8}{c}{Outflow properties} \\ \hline
& $V_{\rm{max}}$$^a$ & $R$ &$M$$^b$$^{,c}$ & $t_{\rm{d}}$$^a$$^{,d}$ & $\dot{M}$$^a$$^{,e}$ & $F_{\rm CO}$$^b$$^{,f}$ & $L_{\rm{kin}}$$^{b,g}$  \\ % 
 & (km s$^{-1}$) & (AU)& ($M_\odot$) & (yr) & ($M_\odot$  &($M_\odot$ yr$^{-1}$ & ($L_\odot$)  \\ % 
             &     &           &     &      &  yr$^{-1}$)& km s$^{-1}$) & \\
             \hline 
 \multicolumn{8}{c}{Red Lobe} \\ 
 %\hline
CO 2--1 & 14.2 &  5e4      & 0.8/2.9$^h$     &  2.6e4   & 9.1e-5  & 9.8e-4  & 1.2e-2 \\
CO 3--2 & 14.0 & $>$2.5e4  & 0.68    &$>$1.3e4  & 4.2e-5  & 4.5e-4  & 5.4e-3\\
CO 4--3$^i$ & 11.0 & --     & $>$0.18 & --         & --    & -- & --\\
CO 6--5 & 10.5 &  $>$2.5e4 & 0.48    & 2.2e4   & 1.8e-5 & 1.1e-4  & 8.0e-4 \\
CO 7--6 & 12.1 & 2.0e4     & 0.4     & 1.4e4   & 2.2e-5 & 1.7e-4  & 1.6e-3\\ 
\hline
\multicolumn{8}{c}{Blue Lobe} \\ 
%\hline
CO 2--1 & 0.5 & 1.2e4  & 0.24& 1.2e4  &  1.6e-5  & 9.3e-5  & 6.0e-4 \\
CO 3--2 & 0.3 & 1.6e4  & 0.24& 1.5e4  &  1.3e-5  & 7.6e-5  & 5.0e-4\\
CO 4--3 & 1.7 & 1.1e4  & 0.19& 1.5e4  &  1.1e-5  & 4.5e-5  & 2.2e-4\\
CO 6--5 & 0.5 & 1.1e4  & 7e-3& 1.1e4  &  5.4e-7  & 3.0e-6  & 2.0e-5\\
CO 7--6 & 1.1 & 1.0e4  & 1e-2& 1.2e4  &  8.6e-7  & 4.3e-6  & 2.4e-5\\ \hline
\end{tabular}}
\par
\medskip
$^a$ Actual LSR velocities; note that the quiescent gas is at $V_{\rm LSR}=5.3$~km~s$^{-1}$. $\delta V_{\max}$ = abs($V_{\max}- V_{\rm{LSR}}$). Velocities are not corrected for inclination.  \\
$^b$ Corrected for inclination using the average correction factors of
\citet{Cabrit90}.\\ 
$^c$ Constant temperature of 100~K assumed for red outflow and 70~K for blue outflow.\\
$^d$ Dynamical time scale: $t_{\rm{d}}=R/\delta V_{\max}$.\\ 
$^e$ Mass outflow rate: $\dot{M}=M/t_{\rm d}$, not corrected for swept-up gas.\\ 
$^f$ Outflow force: $F_{\rm CO}=MV_{\max}^2/R$.\\ 
$^g$ Kinetic luminosity: $L_{\rm{kin}}=0.5M(\delta V_{\rm{max}})^3/R$.\\ 
$^h$ 0.8~$M_\odot$ is derived for a temperature of 50~K. 2.9~$M_\odot$ is derived for a temperature of 100~K.\\
$^i$ Outflow extends to far larger scales than map scale.
\end{table}