\\ Species Tag:        &   49001 & Name:&  O3-sym-O-17    
\\ Version:            &       2 & & Ozone,
\\ Date:       &  Mar. 1995      & & symmetric $^{17}$O isotope
\\ Contributor:&  E. A. Cohen    & & 
\\             &                 & & 
\\ Lines Listed:       &   26092 & Q(300.0)=&    20803.525 
\\ Freq. (GHz) $<$     &    4603 & Q(225.0)=&    13507.522 
\\ Max. J:             &      76 & Q(150.0)=&     7352.785 
\\ LOGSTR0=            &    -8.5 & Q(75.00)=&     2605.615 
\\ LOGSTR1=            &    -8.0 & Q(37.50)=&      928.081 
\\ Isotope Corr.:      &  -3.432 & Q(18.75)=&      334.464 
\\ Egy. (cm$^{-1}$) $>$&     0.0 & Q(9.375)=&      123.884 
\\ $\mu_a$ = &                   & A=& 102351.
\\ $\mu_b$ = & 0.5337            & B=&  13350.8
\\ $\mu_c$ = &                   & C=&  11781.7
\headend 

	The spectra are from E. A. Cohen, K. W. Hillig II, and H. M. Pickett,
1995, J. Mol.\ Struct.\ {\bf 352/353,} 273. The calculation fixes centrifugal
distortion constants beyond the sextic terms to those of the parent species
with the exception of the coefficients of $P_a^{2n}$ which are assumed to
be proportional to $A^n$.  The dipole moment was assumed to be the same as for
the parent species, however centrifugal corrections have not been applied. 
Where several experimental lines have the same frequency,
the uncertainties refer to the center of a blended feature, not to the
individual components.