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David C. Fritts, Ronald B. Smith, Michael J. Taylor, James D. Doyle, Stephen D. Eckermann, Andreas Dörnbrack, Markus Rapp, Bifford P. Williams, P.-Dominique Pautet, Katrina Bossert, Neal R. Criddle, Carolyn A. Reynolds, P. Alex Reinecke, Michael Uddstrom, Michael J. Revell, Richard Turner, Bernd Kaifler, Johannes S. Wagner, Tyler Mixa, Christopher G. Kruse, Alison D. Nugent, Campbell D. Watson, Sonja Gisinger, Steven M. Smith, Ruth S. Lieberman, Brian Laughman, James J. Moore, William O. Brown, Julie A. Haggerty, Alison Rockwell, Gregory J. Stossmeister, Steven F. Williams, Gonzalo Hernandez, Damian J. Murphy, Andrew R. Klekociuk, Iain M. Reid, and Jun Ma

(GV) provided in situ, dropsonde, and microwave temperature profiler (MTP) measurements extending from Earth’s surface to ∼20 km throughout the core field program (see Table 2 ). The GV also carried three new instruments designed specifically to address DEEPWAVE science goals: 1) a Rayleigh lidar measuring densities and temperatures from ∼20 to 60 km, 2) a sodium resonance lidar measuring sodium densities and temperatures from ∼75 to 100 km, and 3) an advanced mesosphere temperature mapper (AMTM

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Sonja Gisinger, Andreas Dörnbrack, Vivien Matthias, James D. Doyle, Stephen D. Eckermann, Benedikt Ehard, Lars Hoffmann, Bernd Kaifler, Christopher G. Kruse, and Markus Rapp

analyzes the atmospheric conditions from the troposphere up to the mesosphere during austral winter 2014. We emphasize key circulation features during the DEEPWAVE campaign period and relate them to the climatological mean conditions. The different meteorological conditions are related to observed wave events [intensive observing periods (IOPs) with airborne observations and periods with only ground-based (GB) measurements as listed in Tables 4 and 5 in Fritts et al. (2016) ]. Section 2 provides

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