“…The extreme temperature and pressure regime in the deep atmosphere of Venus, however, makes high demands on new theoretical and methodical work including hot gaseous absorption bands, far spectral line wings and pressure‐induced absorption. Much effort has been devoted to explaining the effects of spectral line shape under high temperature and pressure conditions [e.g., Burch et al , 1969; Tonkov et al , 1996; Filippov and Tonkov , 1998; Ma et al , 1999; Tvorogov and Rodimova , 1995; Afanasenko and Rodin , 2005], but up to now, the related works do not offer a self‐sufficient model that is suitable for practical calculations over the full spectral range that is of interest for surface and deep atmosphere studies. This is the reason why currently most simulation algorithms make use of empirically determined continuum opacities to fit the observations.…”