EGU21-14813
https://doi.org/10.5194/egusphere-egu21-14813
EGU General Assembly 2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Infrasound transmission in the "shadow zone" observed on balloons in the lower stratosphere

Johan Kero1, Daniel Bowman2, and Eli Bird3
Johan Kero et al.
  • 1Swedish Institute of Space Physics (IRF), Kiruna, Sweden (kero@irf.se)
  • 2Sandia National Laboratories, Albuquerque, New Mexico, USA (dbowma@sandia.gov)
  • 3Department of Geological Sciences, University of North Carolina at Chapel Hill, North Carolina, USA (elibird@live.unc.edu)

The temperature and wind structure of the lower atmosphere creates an "acoustic shadow", where acoustic propagation is not expected to occur from a ground based source. This region begins several tens of kilometers from the source and typically ends between one hundred and two hundred kilometers range in the downwind direction of the stratospheric jet. Ground microbarometers still occasionally record acoustic arrivals in this zone due to tropospheric waveguides and/or scattering off of stratospheric structure not accounted for in atmospheric models. However, the properties of these signals in the lower stratosphere (above the tropospheric duct) is unknown, because they have never been previously observed on sensors at these altitudes. Here we present a set of acoustic arrivals from ground explosions recorded on balloons in the lower stratosphere during the mini-BOOSTER campaign in Sweden. Although some of the balloons were in the shadow zone, they still recorded a variety of waveforms from each event. Dual payloads on tethers show that the acoustic waves came from below in these instances. We discuss the provenance of these signals and implications for acoustic transmission in regions where geometric ray theory predicts their absence.

How to cite: Kero, J., Bowman, D., and Bird, E.: Infrasound transmission in the "shadow zone" observed on balloons in the lower stratosphere, EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-14813, https://doi.org/10.5194/egusphere-egu21-14813, 2021.

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