Topographically Scattered Infrasound Waves Observed on Microbarometer Arrays in the Lower Stratosphere

When an acoustic wave strikes a topographic feature, some of its energy is scattered. Sensors on the ground cannot capture these scattered signals when they propagate at high angles. We report observations of upwardly-scattered acoustic waves prior to refraction back to the ground, intercepting them...

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Published in:Earth and Space Science
Main Authors: Bird, Elijah J., Lees, J. M., Kero, J., Bowman, D. C.
Language:unknown
Published: 2023
Subjects:
Online Access:http://www.osti.gov/servlets/purl/1870466
https://www.osti.gov/biblio/1870466
https://doi.org/10.1029/2022ea002226
id ftosti:oai:osti.gov:1870466
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spelling ftosti:oai:osti.gov:1870466 2023-07-30T04:05:52+02:00 Topographically Scattered Infrasound Waves Observed on Microbarometer Arrays in the Lower Stratosphere Bird, Elijah J. Lees, J. M. Kero, J. Bowman, D. C. 2023-02-23 application/pdf http://www.osti.gov/servlets/purl/1870466 https://www.osti.gov/biblio/1870466 https://doi.org/10.1029/2022ea002226 unknown http://www.osti.gov/servlets/purl/1870466 https://www.osti.gov/biblio/1870466 https://doi.org/10.1029/2022ea002226 doi:10.1029/2022ea002226 58 GEOSCIENCES 2023 ftosti https://doi.org/10.1029/2022ea002226 2023-07-11T10:12:43Z When an acoustic wave strikes a topographic feature, some of its energy is scattered. Sensors on the ground cannot capture these scattered signals when they propagate at high angles. We report observations of upwardly-scattered acoustic waves prior to refraction back to the ground, intercepting them with a set of balloon-borne infrasound microbarometers in the lower stratosphere over northern Sweden. We show that these scattered waves generate a coda whose presence can be related to topography beneath balloons and low-altitude acoustic ducts. The inclination of the coda signals changes systematically with time, as expected from waves arriving from scatterers successively closer to receivers. The codas are present when a temperature inversion channels infrasound from a set of ground chemical explosions along the ground, but are absent following the inversion's dissipation. Since scattering partitions energy away from the main arrival, these observations imply a mechanism of amplitude loss that had previously been inaccessible to measurement. As such, these data and results allow for a better comprehension of interactions between atmospheric infrasound propagation and the solid earth Other/Unknown Material Northern Sweden SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) Earth and Space Science 9 4
institution Open Polar
collection SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy)
op_collection_id ftosti
language unknown
topic 58 GEOSCIENCES
spellingShingle 58 GEOSCIENCES
Bird, Elijah J.
Lees, J. M.
Kero, J.
Bowman, D. C.
Topographically Scattered Infrasound Waves Observed on Microbarometer Arrays in the Lower Stratosphere
topic_facet 58 GEOSCIENCES
description When an acoustic wave strikes a topographic feature, some of its energy is scattered. Sensors on the ground cannot capture these scattered signals when they propagate at high angles. We report observations of upwardly-scattered acoustic waves prior to refraction back to the ground, intercepting them with a set of balloon-borne infrasound microbarometers in the lower stratosphere over northern Sweden. We show that these scattered waves generate a coda whose presence can be related to topography beneath balloons and low-altitude acoustic ducts. The inclination of the coda signals changes systematically with time, as expected from waves arriving from scatterers successively closer to receivers. The codas are present when a temperature inversion channels infrasound from a set of ground chemical explosions along the ground, but are absent following the inversion's dissipation. Since scattering partitions energy away from the main arrival, these observations imply a mechanism of amplitude loss that had previously been inaccessible to measurement. As such, these data and results allow for a better comprehension of interactions between atmospheric infrasound propagation and the solid earth
author Bird, Elijah J.
Lees, J. M.
Kero, J.
Bowman, D. C.
author_facet Bird, Elijah J.
Lees, J. M.
Kero, J.
Bowman, D. C.
author_sort Bird, Elijah J.
title Topographically Scattered Infrasound Waves Observed on Microbarometer Arrays in the Lower Stratosphere
title_short Topographically Scattered Infrasound Waves Observed on Microbarometer Arrays in the Lower Stratosphere
title_full Topographically Scattered Infrasound Waves Observed on Microbarometer Arrays in the Lower Stratosphere
title_fullStr Topographically Scattered Infrasound Waves Observed on Microbarometer Arrays in the Lower Stratosphere
title_full_unstemmed Topographically Scattered Infrasound Waves Observed on Microbarometer Arrays in the Lower Stratosphere
title_sort topographically scattered infrasound waves observed on microbarometer arrays in the lower stratosphere
publishDate 2023
url http://www.osti.gov/servlets/purl/1870466
https://www.osti.gov/biblio/1870466
https://doi.org/10.1029/2022ea002226
genre Northern Sweden
genre_facet Northern Sweden
op_relation http://www.osti.gov/servlets/purl/1870466
https://www.osti.gov/biblio/1870466
https://doi.org/10.1029/2022ea002226
doi:10.1029/2022ea002226
op_doi https://doi.org/10.1029/2022ea002226
container_title Earth and Space Science
container_volume 9
container_issue 4
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