FORMATION CHARACTERISTICS OF SPORADIC NA LAYERS OBSERVED SIMULTANEOUSLY BY LIDAR AND AIRGLOW INSTRUMENTS DURING ALOHA-90

Sporadic Na (Na(s)) layers were observed by the airborne lidar during ALOHA-90 on the 22, 25 and 27 March flight missions. Perturbations in the O2 and OH nighttime airglow emission intensities and temperatures were also observed by instruments on the aircraft and at Haleakala Crater (20.8-degrees-N, 156.2-degrees-W) during these events. The most striking correlation between the airglow and lidar measurements occurred during the northbound flight leg of the 25 March mission. When the Na(s) layer formed at 90.7 km, while the Electra aircraft was between 750 and 500 km south of Haleakala, the O2 temperatures near 95 km above the Electra and Haleakala increased by approximately 45 K. The data for this night suggest a connection between Na(s) and a large-scale wave, and suggest that the wave is tidal in nature. The data also suggest that some Na(s) layers can form very quickly over large geographic areas. Fast chemical processes are required to generate the large amounts of atomic Na involved in some of these events.