“…The altitude of the OH* layer has frequently been measured using rocket-borne photometers, satellite-borne instruments and lidar remote sensing (through calculating equivalent OH*-temperatures from lidar temperature profiles) and was always found to peak at that altitude region with some minor variability (e.g. von Savigny et al, 2004;Shepherd et al, 2004;Iwagami et al, 2002;Melo et al, 2000;She and Lowe, 1998;Takahashi et al, 1996;Mende et al, 1993;Takano et al, 1990;Baker and Stair, 1988;von Zahn et al, 1987;Lopez-Moreno et al, 1987;Watanabe et al, 1981;Witt et al, 1979;Good, 1976). We therefore assume that these values apply also to our measurements.…”