The hydroxyl radical (OH) plays a fundamental role in the chemistry and dynamics of the middle and upper atmosphere. The measured OH rotational-vibrational line emissions are used to derive kinetic temperature and observe dynamical processes such as tides, planetary, and gravity waves (Grygalashvyly et al., 2014 and references therein). Moreover, as was recently shown by Sharma et al. (2015) and Kalogerakis et al. (2016), collisions between OH and O(3 P) provide a nighttime source of O(1 D). Therefore, detailed knowledge of [OH] and its variability is crucially important in understanding the formation of different types of airglow and infrared emissions (Kalogerakis, 2019; Panka et al., 2017) of the nighttime mesosphere. The emissions of nighttime mesospheric OH were measured by various instruments in a number of spectral ranges. Pickett et al. (2006) used the Microwave Limb Sounder instrument on the Aura satellite measurements of the thermal emission from 2.5 THz rotational lines to retrieve the altitude profile from 18-94 km of