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Mozhgan Amiramjadi, Ali R. Mohebalhojeh, Mohammad Mirzaei, Christoph Zülicke, and Riwal Plougonven

noted that the apparent source around 4°S and between 150° and 140°W due to jet, where | v ′| exceeds the threshold of 1.3 m s −1 is discarded by the Froude number filter described above. c. Source distributions Both of the calculated energies have been taken care of by quality controls. As discussed in section 2 , the Froude number is taken into account to deal with the horizontal propagation of gravity waves in the troposphere. Figure 8 shows how applying the criterion of Fr ≥ 0.3 can

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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

approximately 9 and 97 km (261–0.001 hPa) with a vertical resolution of about 4 km in the stratosphere and about 14 km near the mesopause. The temporal resolution is 1 day at each location and data are available from August 2004 ( Livesey et al. 2017 ). Note that version 4 MLS data are used and that the most recent recommended quality screening procedures of Livesey et al. (2017) have been applied. The two-dimensional least squares method used by Wu et al. (1995) is applied to the global datasets of ERA

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Christoph Zülicke, Erich Becker, Vivien Matthias, Dieter H. W. Peters, Hauke Schmidt, Han-Li Liu, Laura de la Torre Ramos, and Daniel M. Mitchell

: Dynamical coupling of the stratosphere and mesosphere in the 2002 Southern Hemisphere major stratospheric sudden warming . Geophys. Res. Lett. , 32 , L13804 , https://doi.org/10.1029/2005GL022939 . 10.1029/2005GL022939 Livesey , N. J. , and Coauthors , 2015 : Earth Observing System (EOS) Aura Microwave Limb Sounder (MLS) Version 4.2x Level 2 data quality and description document. Tech. Rep. JPL D-33509 Rev. B, Jet Propulsion Laboratory, California Institute of Technology, 169 pp., https://mls.jpl.nasa.gov/data

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Martina Bramberger, Andreas Dörnbrack, Henrike Wilms, Steffen Gemsa, Kevin Raynor, and Robert Sharman

resolutions of less than 10 km. Thus, high-resolution global data are a valuable source for detecting and predicting mountain waves. Dörnbrack et al. (2017) showed that the recent increase of horizontal resolution of the Integrated Forecast System (IFS) of the European Centre for Medium-Range Weather Forecasts (ECMWF) led to a realistic simulation of wave-induced mesoscale temperature anomalies. Moreover, they concluded that the remarkable agreement of the simulated wave structure in the IFS short

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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

the EOL/Research Aviation Facility (RAF) Aeros and catalog maps tools for displaying real-time aircraft position, flight-level data displays, satellite and model data overlays, dropsonde launches and plots, and lidar and AMTM data sharing. A unique aspect of DEEPWAVE was the ability to make real-time dropsonde deployment decisions at specific points over New Zealand and widely over the Southern Ocean. These data were relayed via satellite to the ground for quality control and processing by EOL

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