EGU26-8082, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-8082
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
PICO | Friday, 08 May, 11:03–11:05 (CEST)
 
PICO spot 5, PICO5.6
The impact of gravity wave parameterizations on the upper atmosphere ICON model and infrasound propagation.
Samuel Kristoffersen1, Constantino Listowski1, Ulrich Achatz2, Georg-Sebastian Völker3, Robin Wing4, Sergey Khaykin5, Gerd Baumgarten4, Alain Hauchecorne5, Alexis Le Pichon1, and Julien Vergoz1
Samuel Kristoffersen et al.
  • 1French Atomic and Alternative Energy Commission, France (samuel.kristoffersen@unb.ca)
  • 2Goethe University Frankfurt
  • 3Leibniz Institute for Baltic Sea Research Warnemünde
  • 4Leibniz Institute of Atmospheric Physics
  • 5LATMOS – Laboratoire Atmosphère Observations Spatiales, UVSQ, CNRS, Sorbonne University

Infrasound signals are generated by various anthropogenic and natural sources, and are one of the technologies used in monitoring compliance with the Comprehensive Nuclear-Test Ban Treaty (CTBT). It is, therefore, of interest to study and better understand the impacts of atmospheric parameters, notably gravity waves (GW), on infrasound propagation. Middle-atmosphere dynamics, up to the lower thermosphere, must be simulated to account for the different acoustic waveguides that allow the long-range propagation and infrasound detections by the CTBT’s International Monitoring System.

 

Since infrasound propagates up to the lower thermosphere, an upper atmospheric model like the upper-atmosphere extension of the ICON model (UA-ICON) is necessary to properly understand and predict infrasound propagation. Toward this goal, we will present studies of UA-ICON using two different GW parameterizations: the operational one also used for the operational ICON forecasts issued by DWD, and a 3D gravity wave parameterization scheme (MS-GWaM) that includes improved GW propagation. We also propose a method to derive stochastic predictions of realistic GW perturbation profiles using MS-GWaM. These results are compared to lidar observations, showing the importance of correctly tuned GW parameterizations on temperature profiles, from tropical to high latitudes. In addition, we will present case studies of infrasound propagation to highlight the importance of mesospheric wind and temperature, as well as GWs, on infrasound propagation and source localization. Notably, infrasound allows us to investigate equatorial latitudes where lidar measurements are missing.

How to cite: Kristoffersen, S., Listowski, C., Achatz, U., Völker, G.-S., Wing, R., Khaykin, S., Baumgarten, G., Hauchecorne, A., Le Pichon, A., and Vergoz, J.: The impact of gravity wave parameterizations on the upper atmosphere ICON model and infrasound propagation., EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-8082, https://doi.org/10.5194/egusphere-egu26-8082, 2026.