Preprints
https://doi.org/10.5194/egusphere-2023-633
https://doi.org/10.5194/egusphere-2023-633
23 May 2023
 | 23 May 2023

High-altitude atmospheric turbulence and infrasound measurements using a balloon-launched small uncrewed aircraft system

Anisa N. Haghighi, Ryan D. Nolin, Gary D. Pundsack, Nick Craine, Aliaksei Stratislatau, and Sean C. C. Bailey

Abstract. This study investigates the use of a balloon-launched small Uncrewed Aircraft System (sUAS) for the measurement of turbulence in the troposphere and lower stratosphere. The sUAS was a glider which could conduct an automated descent following a designated flight trajectory and equipped with in-situ sensors for measuring thermodyanamic and kinematic atmospheric properties typically measured using balloon-borne instruments. The trajectory of the glider allowed for improved statistical convergence and higher spatial resolution of derived statistics measured by the in-situ sensors. In addition, this aircraft was equipped with an infrasonic microphone to assess its suitability for the remote detection of clear-air turbulence. The capabilities of the sUAS and sensing systems were tested using three flights conducted in 2021 in New Mexico. It was found that the profiles of temperature, humidity and horizontal winds measured during descent were consistent with those made by radiosonde. Importantly, analysis of the statistics produced along the flight trajectory allowed the identification of key turbulence quantities and features such as gravity waves, thermals and tropopause folding, which allowed the connection to be made between the locations of increased turbulence intensity and the source of its generation. In addition, the infrasonic microphone amplitude was found to be correlated with the measurements of turbulence intensity, indicating that the microphone was sensing turbulence. However, interpretation of the microphone signal was convoluted by the altitude dependence of the microphone response and the difficulty in discriminating individual sources from within the microphone signal.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this preprint. The responsibility to include appropriate place names lies with the authors.
Anisa N. Haghighi, Ryan D. Nolin, Gary D. Pundsack, Nick Craine, Aliaksei Stratislatau, and Sean C. C. Bailey

Status: final response (author comments only)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2023-633', Anonymous Referee #1, 25 Jun 2023
    • AC1: 'Reply on RC1', Sean Bailey, 06 Aug 2023
  • RC2: 'Comment on egusphere-2023-633', Anonymous Referee #2, 26 Jun 2023
    • AC2: 'Reply on RC2', Sean Bailey, 06 Aug 2023
  • RC3: 'Comment on egusphere-2023-633', Anonymous Referee #3, 26 Jun 2023
    • AC3: 'Reply on RC3', Sean Bailey, 06 Aug 2023
Anisa N. Haghighi, Ryan D. Nolin, Gary D. Pundsack, Nick Craine, Aliaksei Stratislatau, and Sean C. C. Bailey

Video abstract

Video summary of aircraft preparation and flight Nick Craine and Gary Pundsack https://vimeo.com/568101900

Anisa N. Haghighi, Ryan D. Nolin, Gary D. Pundsack, Nick Craine, Aliaksei Stratislatau, and Sean C. C. Bailey

Viewed

Total article views: 629 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
366 231 32 629 28 30
  • HTML: 366
  • PDF: 231
  • XML: 32
  • Total: 629
  • BibTeX: 28
  • EndNote: 30
Views and downloads (calculated since 23 May 2023)
Cumulative views and downloads (calculated since 23 May 2023)

Viewed (geographical distribution)

Total article views: 643 (including HTML, PDF, and XML) Thereof 643 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 26 May 2024
Download
Short summary
This work summarizes measurements conducted in June 2021 using a small, uncrewed, stratospheric glider which was launched from a weather balloon to altitudes up to 30 km above sea level. The aircraft conducted measurements of wind speed and direction, pressure, temperature and humidity during its descent, as well as infrasonic sound levels. These measurements were used to evaluate the atmospheric turbulence observed during the descent and relate it to the atmospheric dynamics producing it.