Articles | Volume 26, issue 11
https://doi.org/10.5194/acp-26-8145-2026
https://doi.org/10.5194/acp-26-8145-2026
Research article
 | 
11 Jun 2026
Research article |  | 11 Jun 2026

Identifying orographic gravity waves in 3D observations via backward ray tracing

Sebastian Rhode, Peter Preusse, and Jörn Ungermann

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Latest update: 11 Jun 2026
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Short summary
Mountain waves are excited when wind flows over elevated terrain. These waves travel through the atmosphere and alter the winds locally when they break, thereby impacting global-scale dynamic phenomena. Understanding mountain waves and their interactions, they need to be identified in measurement data or model simulations. This study provides a method for disentangling the mountain waves from atmospheric fluctuations of other origin in three-dimensional temperature data.
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