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

. 2006 ), radars (e.g., Stober et al. 2013 ), airglow imagers (e.g., Suzuki et al. 2010 ), noctilucent cloud images (e.g., Pautet et al. 2011 ), satellite measurements (e.g., Alexander et al. 2008 ), radiosonde soundings (e.g., Dörnbrack et al. 1999 ; Zhang and Yi 2005 ), and rocket soundings (e.g., Rapp et al. 2004 ). However, these instruments are limited to particular altitude ranges and are only sensitive to a distinct part of the gravity wave spectrum ( Gardner and Taylor 1998 ; Preusse

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