“…Atmospheric parameters such as the temperature, pressure, humidity, and possibly the CO 2 content are measured to calculate the refractive index using the Edlén equation 6 , 7 , However, it is difficult to get an accurate distribution of these parameters along the optical path, especially at long distances and with a moving stage 8 . Nevertheless, the influence of the turbulence of the atmosphere can be corrected using the two-color method proposed by Bender and Owens 9 , 10 , which is widely used in optical frequency combs 11 – 14 and laser interferometers 15 – 18 . This method measures a geometric distance, L , with both wavelength λ 1 and λ 2 , to obtain two optical distances, L λ 1 and L λ 2 , and gives the geometric distance L = L λ 1 − A ( L λ 2 − L λ 1 ), where A is the so-called A-coefficient in two-color method that represents the dispersion relation for air refractive indices at two wavelengths.The conventional two-color method eliminated the influence of the atmosphere, yet simultaneously enlarged the uncertainties in measured optical distances, Δ L λ 1 and Δ L λ 2 , because of the stability of the laser wavelength, thermal expansion and the optical thermal drift 19 .…”