“…Quantitative measurements of intensity have been made for individual rotational lines of the atmospheric oxygen b 1 + g (υ = 0,2) ← X 3 − g (υ = 0) or the A-and γ -bands by using different techniques such as: "White" multiple traversal absorption cells [38][39][40][47][48][49][50], intracavity laser-absorption spectroscopy (ICLAS) [37], and cavity ring down spectroscopy (CRDS) [18,51]. Previous measurements of the A-band absorption have been attempted to obtain experimental line parameters between 202 and 224 K. However, the temperatures had an uncertainty of 10 K, the actual spectra were not presented, and the temperature dependence of the pressure shift was not determined [50].…”