Rosseland & Planck gaseous mean opacities

Such calculations are used in modeling the atmospheres, interiors, formation, and evolution of these objects. Our calculations are an expansion of those presented in Freedman (2008ApJS..174..504F) to include lower pressures, finer temperature resolution, and also the higher metallicities most relevant for giant planet atmospheres.

Calculations span 1{mu}bar to 300bar, and 75-4000K, in a nearly square grid. Opacities at metallicities from solar to 50 times solar abundances are calculated. We also provide an analytic fit to the Rosseland mean opacities over the grid in pressure, temperature, and metallicity.