\\ Species Tag:        &   48005 & Name:&  O3-v2         
\\ Version:            &       4 & &(010) or $\nu_2$ state
\\ Date:       &  Nov. 2005     & &
\\ Contributor:&  B. J. Drouin  & &
\\             &  H. M. Pickett & &
\\ Lines Listed:       &    4911 & Q(300.0)=&     3553.040
\\ Freq. (GHz) $<$     &    5945 & 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$^{-1}$) $>$&   700.9 & Q(9.375)=&       19.037
\\ $\mu_a$ = &                   & A=& 108137.91
\\ $\mu_b$ = &  0.5261           & B=& 13311.44
\\ $\mu_c$ = &                   & C=& 11765.03
\headend

The ozone spectrum was fitted using the microwave, millimeter, far-infrared,
and infrared transitions given in H. M. Pickett {\it et al.}, 1988, J. Mol.~Spect.~
{\bf 128}, 151. The dipole moment is
from K. M. Mack and J. S. Muenter, (1977)
J.\ Chem.\ Phys.\ {\bf 66}, 15.  Line strengths were calculated using
Herman Wallis parameters fitted to match intensities from 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 function includes all vibrational states.