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Winds at the Mars 2020 Landing Site. 2. Wind Variability and Turbulence.
D Viúdez-Moreiras1, M de la Torre2, J Gómez-Elvira3
1Centro de Astrobiología (CAB, CSIC-INTA) and National Institute for Aerospace Technology (INTA) Madrid Spain.
Mars 2020 Perseverance rover data reveal Jezero crater experiences calmer average winds but intense turbulence and wave activity. These transient high wind events, driven by vortices and convection, likely cause significant aeolian activity and instrument damage.
Area of Science:
- Planetary Science
- Atmospheric Science
- Mars Exploration
Background:
- Mars 2020 Perseverance rover collected wind data in Jezero crater.
- InSight lander data from Elysium Planitia provide comparative context.
- Jezero crater exhibits intense aeolian activity despite calmer average wind speeds.
Purpose of the Study:
- Characterize wind speed distributions and turbulence in Jezero crater.
- Investigate the drivers of aeolian activity on Mars.
- Understand the impact of wind dynamics on rover instrumentation.
Main Methods:
- Fitting wind speed data to a Weibull distribution.
- Analyzing power spectral density of wind speed fluctuations.
- Correlating wind variations with atmospheric phenomena like convection cells and dust storms.
Main Results:
- Jezero winds are calmer on average than at previous Mars landing sites.
- Turbulence and wave activity significantly influence wind speed variations and extreme wind events.
- Convective vortices and mechanical turbulence contribute to rapid wind fluctuations, peaking at 9.2 times background levels.
- A large dust cloud (0.75-1.5 km) was observed passing over the rover.
Conclusions:
- Transient high wind events, driven by vortex passages and turbulence, are key drivers of aeolian activity at Jezero.
- Observed aeolian activity has led to damage to the rover's wind sensor.
- Understanding Martian wind dynamics is crucial for future missions and instrument design.
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