“…With this technique, effective pathlengths of tens to hundreds of kilometers through the sample can be achieved, overcoming many of the sensitivity limitations noted above. By careful control of the ICLAS generation time t g 1 and data acquisition procedure (12), it is possible to carry out quantitative lineshape measurements, as has been demonstrated for water vapor (14,15), methane (16), and the (vЈ ϭ 2) 4 (vЉ ϭ 0) band of the O 2 b 4 X transition (␥ band) (17,18).…”