1. A model of the Schumann- Runge continuum of O2;Allison;J. Geophys. Res.,1986
2. Polar twilight UV-visible radiation field, Perturbations due to multiple scattering, ozone depletion, stratospheric clouds, and surface albedo;Anderson;J. Geophys. Res.,1990
3. Synthetic dayglow spectra and the Rayleigh scattering background from the Far UV to the visible, Ultraviolet Technology II;Anderson,1988
4. Stratospheric determination of O2 cross-sections and photodissociation rate coefficients: 191–215nm;Anderson;J. Geophys. Res.,1986