The optical constants of substances composing atmospheric aerosols are required to evaluate properly the effects of aerosols on the earth's radiation balance. We briefly review techniques for determining optical constants and also discuss pitfalls in using measured optical constants to simulate the optical constants of the real particles found in the atmosphere. We then compile the optical constants of (NH4hSO4, Al:Os, and NaCI. The optical constants of Al:Os and NaCI are derived from values quoted in the literature. The optical constants of (NH4):SO• are derived partly from values quoted in the literature and partly from our own measurements. Spitzer, W. G., and D. A. Kleinman, Infrared lattice bands of quartz, Phys. Rev., 121, 1324, 1961•." Strukov, Bi A., The temperature dependence of birefringence in crystals of ammonium sulfate and ammonium fluoroberYllate, Sot). Phys. Crystallogr., 6, 511, 1961. Toon, O. B., and J. B. Pollack, A global average model of atmospheric aerosols for radiative transfer calculations, J. Appl. Meteorol., 15, 225, 1976. Toon, O. B., J. B. Pollack, and C. Sagan, Properties of suspended aerosols from their infrared spectra: Application to Martian dust storms of 1971, Icarus, in press, 1976. Verleur, H. W., Determination of optical constants from reflectance or transmittance measurements on bulk crystals or thin films, d. Opt. Soc. Amer., 58, 1356, 1968. Volz, F. E., Infrared refractive index of atmospheric aerosol substances, Appl. Opt., 11, 755, 1972. Volz, F. E., Infrared optical constants of ammonium sulfate, Sahara dust, volcanic pumice, and flyash, Appl. Opt., 12, 564, 1973.