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The sound of a Martian dust devil.
Murdoch, N; Stott, A E; Gillier, M; Hueso, R; Lemmon, M; Martinez, G; Apéstigue, V; Toledo, D; Lorenz, R D; Chide, B; Munguira, A; Sánchez-Lavega, A; Vicente-Retortillo, A; Newman, C E; Maurice, S; de la Torre Juárez, M; Bertrand, T; Banfield, D; Navarro, S; Marin, M; Torres, J; Gomez-Elvira, J; Jacob, X; Cadu, A; Sournac, A; Rodriguez-Manfredi, J A; Wiens, R C; Mimoun, D.
Affiliation
  • Murdoch N; Institut Supérieur de l'Aéronautique et de l'Espace (ISAE-SUPAERO), Université de Toulouse, Toulouse, France. naomi.murdoch@isae-supaero.fr.
  • Stott AE; Institut Supérieur de l'Aéronautique et de l'Espace (ISAE-SUPAERO), Université de Toulouse, Toulouse, France.
  • Gillier M; Institut Supérieur de l'Aéronautique et de l'Espace (ISAE-SUPAERO), Université de Toulouse, Toulouse, France.
  • Hueso R; Física Aplicada, Escuela de Ingeniería de Bilbao, Universidad del País Vasco (UPV/EHU), Bilbao, Spain.
  • Lemmon M; Space Science Institute, Boulder, CO, 80301, USA.
  • Martinez G; Lunar and Planetary Institute, Universities Space Research Association, Houston, TX, USA.
  • Apéstigue V; Department of Climate and Space Sciences and Engineering, University of Michigan, Ann Arbor, MI, USA.
  • Toledo D; Instituto Nacional de Técnica Aeroespacial, Madrid, Spain.
  • Lorenz RD; Instituto Nacional de Técnica Aeroespacial, Madrid, Spain.
  • Chide B; Space Exploration Sector, Johns Hopkins Applied Physics Laboratory, Laurel, MD, USA.
  • Munguira A; Space and Planetary Exploration Team, Los Alamos National Laboratory, Los Alamos, NM, USA.
  • Sánchez-Lavega A; Física Aplicada, Escuela de Ingeniería de Bilbao, Universidad del País Vasco (UPV/EHU), Bilbao, Spain.
  • Vicente-Retortillo A; Física Aplicada, Escuela de Ingeniería de Bilbao, Universidad del País Vasco (UPV/EHU), Bilbao, Spain.
  • Newman CE; Centro de Astrobiología (INTA-CSIC), Madrid, Spain.
  • Maurice S; Aeolis Research, Chandler, AZ, USA.
  • de la Torre Juárez M; Institut de Recherche en Astrophysique et Planétologie, Université de Toulouse 3 Paul Sabatier, CNRS, CNES, Toulouse, France.
  • Bertrand T; Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA.
  • Banfield D; Laboratoire d'Etudes Spatiales et d'Instrumentation en Astrophysique (LESIA), Observatoire de Paris, Université PSL, CNRS, Sorbonne Université, Univ. Paris Diderot, Sorbonne Paris Cité, 5 place Jules Janssen, 92195, Meudon, France.
  • Navarro S; Cornell University, Ithaca, NY, USA.
  • Marin M; NASA AMES Research Center, Moffett Field, CA, USA.
  • Torres J; Centro de Astrobiología (INTA-CSIC), Madrid, Spain.
  • Gomez-Elvira J; Centro de Astrobiología (INTA-CSIC), Madrid, Spain.
  • Jacob X; Centro de Astrobiología (INTA-CSIC), Madrid, Spain.
  • Cadu A; Instituto Nacional de Técnica Aeroespacial, Madrid, Spain.
  • Sournac A; Institut de Mécanique des Fluides, Université de Toulouse III Paul Sabatier, INP, CNRS, Toulouse, France.
  • Rodriguez-Manfredi JA; Institut Supérieur de l'Aéronautique et de l'Espace (ISAE-SUPAERO), Université de Toulouse, Toulouse, France.
  • Wiens RC; Institut Supérieur de l'Aéronautique et de l'Espace (ISAE-SUPAERO), Université de Toulouse, Toulouse, France.
  • Mimoun D; Centro de Astrobiología (INTA-CSIC), Madrid, Spain.
Nat Commun ; 13(1): 7505, 2022 12 13.
Article in En | MEDLINE | ID: mdl-36513637
ABSTRACT
Dust devils (convective vortices loaded with dust) are common at the surface of Mars, particularly at Jezero crater, the landing site of the Perseverance rover. They are indicators of atmospheric turbulence and are an important lifting mechanism for the Martian dust cycle. Improving our understanding of dust lifting and atmospheric transport is key for accurate simulation of the dust cycle and for the prediction of dust storms, in addition to being important for future space exploration as grain impacts are implicated in the degradation of hardware on the surface of Mars. Here we describe the sound of a Martian dust devil as recorded by the SuperCam instrument on the Perseverance rover. The dust devil encounter was also simultaneously imaged by the Perseverance rover's Navigation Camera and observed by several sensors in the Mars Environmental Dynamics Analyzer instrument. Combining these unique multi-sensorial data with modelling, we show that the dust devil was around 25 m large, at least 118 m tall, and passed directly over the rover travelling at approximately 5 m s-1. Acoustic signals of grain impacts recorded during the vortex encounter provide quantitative information about the number density of particles in the vortex. The sound of a Martian dust devil was inaccessible until SuperCam microphone recordings. This chance dust devil encounter demonstrates the potential of acoustic data for resolving the rapid wind structure of the Martian atmosphere and for directly quantifying wind-blown grain fluxes on Mars.
Subject(s)

Full text: 1 Collection: 01-internacional Database: MEDLINE Main subject: Mars / Extraterrestrial Environment Type of study: Prognostic_studies Language: En Journal: Nat Commun Journal subject: BIOLOGIA / CIENCIA Year: 2022 Document type: Article Affiliation country: Francia

Full text: 1 Collection: 01-internacional Database: MEDLINE Main subject: Mars / Extraterrestrial Environment Type of study: Prognostic_studies Language: En Journal: Nat Commun Journal subject: BIOLOGIA / CIENCIA Year: 2022 Document type: Article Affiliation country: Francia
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