Bob Yirka is a writer for Phys.org.

Dust devils and daytime upslope winds explain Mars’ constant haze
Stretched color version of a movie of a huge “gust lifting” event taken by the Navigation Camera (Navcam) on sol 117. Images are 14 seconds apart. Credit: NASA/Caltech-JPL/SSI

A large team of researchers affiliated with multiple institutions in the U.S., Spain, France and Finland have found that dust devils and daytime upslope winds are the reason for Mars's constant atmospheric haze. In their paper published in the journal Science Advances, the group describes their study of data from the first 216 sols of Perseverance rovers trek across the surface of parts of the red planet and what they learned from it.

Scientists have known for a long time that Mars looks red due to the amount of dust in the atmosphere. The factors that keep the dust aloft have remained a mystery. The study of dust storms on Mars has shown that they are not frequent enough to explain the persistence of dust in the atmosphere. The researchers studied the data from the Perseverance rover.

Perseverance has a panel of sensors known as the Mars Environment Dynamics Analyzer. Air pressure, temperature and wind speed are monitored. Dust dispersal through sunlight is analyzed by MEDA. The rover has a microphone that can be used to listen to the wind.

Dust devils are very common on Mars, at least on the part of the planet where Perseverance is traveling. There was at least one dust devil in the vicinity of the rover. They found that daytime upslope winds were common. The events were less common than the dust devils, but they pulled more dust from the surface into the atmosphere. The researchers suggest that the wind events provide a reasonable explanation for the persistence of dust in the atmosphere.

Credit: Claire Newman, Ricardo Hueso, Mark Lemmon, Tanguy Bertrand, the Mars 2020 Atmospheric Science Working Group, the Mars 2020 mission, and NASA/JPL-Caltech.
Movie showing the predicted near-surface horizontal wind speed (shaded contours) and velocity (arrows) over one complete Mars day (sol) for the Jezero crater region (topography shown as black contours), from a simulation of sol 117 (planetocentric solar longitude, Ls ~ 60°) of the Mars 2020 mission using the Mars Weather Research and Forecasting (MarsWRF) atmospheric model. The Perseverance rover’s landing site is marked by a red cross. Daytime winds are from the SE/ESE and are strongly controlled by regional upslope flows on the slopes of Isidis basin, whereas nighttime winds are from the NW and are more controlled by local topography and peak on the nearby slopes of Jezero crater. Credit: NASA/Aeolis Research
More information: Claire E. Newman et al, The dynamic atmospheric and aeolian environment of Jezero crater, Mars, Science Advances (2022). DOI: 10.1126/sciadv.abn3783 Journal information: Science Advances

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