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Benedikt Ehard, Peggy Achtert, Andreas Dörnbrack, Sonja Gisinger, Jörg Gumbel, Mikhail Khaplanov, Markus Rapp, and Johannes Wagner

wave field. Thus, it was possible to study the vertical propagation of gravity waves from the troposphere into the middle atmosphere, which is generally not possible with Rayleigh lidar observations alone. Furthermore, the Rayleigh lidar observations revealed a stratopause layer descending over several kilometers during both cases, indicating an interaction of the vertically propagating gravity waves with the stratopause. A more detailed analysis of the wave propagation and the interaction with the

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