Wind and Turbulence Observations With the Mars Microphone on Perseverance

Author:

Stott Alexander E.1ORCID,Murdoch Naomi1ORCID,Gillier Martin1,Banfield Don2,Bertrand Tanguy3ORCID,Chide Baptiste4ORCID,De la Torre Juarez Manuel5ORCID,Hueso Ricardo6ORCID,Lorenz Ralph7ORCID,Martinez German89ORCID,Munguira Asier6ORCID,Mora Sotomayor Luis10ORCID,Navarro Sara10,Newman Claire11ORCID,Pilleri Paolo12ORCID,Pla‐Garcia Jorge10ORCID,Rodriguez‐Manfredi Jose Antonio10,Sanchez‐Lavega Agustin6ORCID,Smith Michael13ORCID,Viudez Moreiras Daniel10ORCID,Williams Nathan5ORCID,Maurice Sylvestre12,Wiens Roger C.14ORCID,Mimoun David1ORCID

Affiliation:

1. Institut Supérieur de l’Aéronautique et de l’Espace (ISAE‐SUPAERO) Université de Toulouse Toulouse France

2. NASA Ames Mountain View CA USA

3. Laboratoire d’Etudes Spatiales et d’Instrumentation en Astrophysique (LESIA) Observatoire de Paris‐PSL CNRS Sorbonne Université Université de Paris Cité Meudon France

4. Space and Planetary Exploration Team Los Alamos National Laboratory Los Alamos NM USA

5. Jet Propulsion Laboratory—California Institute of Technology Pasadena CA USA

6. Fisica Aplicada, Escuela de Ingeniería de Bilbao Universidad del País Vasco UPV/EHU Bilbao Spain

7. Johns Hopkins Applied Physics Lab Laurel MD USA

8. Lunar and Planetary Institute USRA Houston TX USA

9. University of Michigan Ann Arbor MI USA

10. Centro de Astrobiologia (CAB) CSIC‐INTA Madrid Spain

11. Aeolis Research Chandler AZ USA

12. CNRS CNES Institut de Recherche en Astrophysique et Planétologie (IRAP) Université de Toulouse 3 Paul Sabatier Toulouse France

13. Goddard Space Flight Center Greenbelt MD USA

14. Purdue University West Lafayette IN USA

Abstract

AbstractWe utilize SuperCam's Mars microphone to provide information on wind speed and turbulence at high frequencies on Mars. To do so, we first demonstrate the sensitivity of the microphone signal level to wind speed, yielding a power law dependence. We then show the relationship between the microphone signal level and pressure, air and ground temperatures. A calibration function is constructed using Gaussian process regression (a machine learning technique) taking the microphone signal and air temperature as inputs to produce an estimate of the wind speed. This provides a high rate wind speed estimate on Mars, with a sample every 0.01 s. As a result, we determine the fast fluctuations of the wind at Jezero crater which highlights the nature of wind gusts over the Martian day. To analyze the turbulent behavior of this wind speed estimate, we calculate its normalized standard deviation, known as gustiness. To characterize the behavior of this high frequency turbulent intensity at Jezero crater, correlations are shown between the evaluated gustiness statistic and pressure drop rates/sizes, temperature and energy fluxes. This has implications for future atmospheric models on Mars, taking into account turbulence at the finest scales.

Funder

Centre National d’Etudes Spatiales

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

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