\\ Species Tag:        &   48004 & Name:&  O3            
\\ Version:            &       3 & &Ozone,
\\ Date:       &  May 1990       & &ground vibrational 
\\ Contributor:&  H. M. Pickett & &state
\\             &                 & &
\\ Lines Listed:       &    7089 & Q(300.0)=&     3553.040
\\ Freq. (GHz) $<$     &    8908 & Q(225.0)=&     2230.489
\\ Max. J:             &      80 & Q(150.0)=&     1198.671
\\ LOGSTR0=            &    -9.8 & Q(75.00)=&      423.448
\\ LOGSTR1=            &   -10.0 & Q(37.50)=&      150.038
\\ Isotope Corr.:      &     0.0 & Q(18.75)=&       53.297
\\ Egy. (cm$^{-1}$) $>$&     0.0 & Q(9.375)=&       19.037
\\ $\mu_a$ = &                   & A=&106536.24
\\ $\mu_b$ = &    0.5324         & B=&13349.26
\\ $\mu_c$ = &                   & C=&11834.36
\headend

The ozone spectrum was fitted using the microwave, millimeter, far-infrared,
and infrared transitions given in H. M. Pickett {\it et al.}, 1985, J. Mol.\ 
Spect.\ {\bf 110}, 186, and H. M. Pickett {\it et al.}, 1988, J. Mol.\ 
Spect.\ {\bf 128}, 151. The dipole moment is from M. Lichtenstein {\it et al.},
1971, J. Mol.\ Spect.\ {\bf 40}, 10.  Line strengths were calculated using 
a model Hamiltonian in which the ground state and the three fundamentals 
were coupled with theoretical matrix elements, and infrared transition 
dipoles were allowed to mix with the permanent dipole.
This treatment gives the correct perturbation of the rotational intensities 
due to centrifugal distortion.  The partition includes contributions from 
all vibrational states.