Sampled opacities of a silicate atmosphere. Shown for a typical Bulk Silicate Earth melt composition with a surface temperature of ~2700 K and atmospheric pressure of 10⁻⁴ bar. The individual species indicate contributed absorption to the total opacity, with the minimum cutoff threshold of 5%. The upper panel shows temperature-specific absorption contribution relative to the maximum opacity for all wavelengths, with a minimum threshold of 10⁻¹⁰. The curve is fitted to indicate the maximum, wavelength-specific opacity for all temperatures. Note that the labelled temperatures are atmospheric, which represent the temperature of the melt.