Tables of integrated absorption coefficients were evaluated for high-temperature air by summation of the contributions from discrete and continuous transitions. The tables were computed for dry air in the temperature range from 1,000 deg K to 12,000 deg K, at equal energy increments of 0.25 ev (2,016.5 cm. to the -1 power), in the wavelength range from 1,167 A to 19,837 A, and for density ratios relative to sea level at each order of magnitude from 10 to .000001.