Dancing dust devils on Mars trace raging winds

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Animation of a dust devil viewed from above on a gray surface with a few craters.
The High Resolution Stereo Camera (HRSC) on board ESA’s Mars Express tracked this dust devil across the Martian surface on November 20, 2018. Studying dust devils on Mars helps scientists trace the red planet’s raging winds. Image via ESA.
  • Combing through 20 years of images from ESA’s Mars Express and ExoMars Trace Gas Orbiter spacecraft, scientists have tracked 1,039 tornado-like whirlwinds to reveal how dust is lifted into the air and swept around Mars’ surface.
  • Their findings, including that the strongest winds on Mars blow much faster than we thought, give us a much clearer picture of the red planet’s weather and climate.
  • With these ‘dust devils’ collected into a single public catalog, this research is just the beginning. It will be useful for planning future missions.

ESA published this original article on October 8, 2025. Edits by EarthSky.

Dancing dust devils on Mars trace raging winds

For decades, we’ve seen dust devils from Mars rovers and orbiters. New research published on October 8, 2025, takes this a big step further. It’s the first study to track the motion of so many of these twisters to find out how exactly they travel across Mars’ surface.

Valentin Bickel from the University of Bern in Switzerland led the study. Their catalog is the first ever to include the speeds and directions of motions for dust devils all over Mars. Valentin explained:

Dust devils make the normally invisible wind visible. By measuring their speed and direction of travel we have started mapping the wind all over Mars’ surface. This was impossible before because we didn’t have enough data to make this kind of measurement on a global scale.

Mars is a dramatic planet, with vast volcanoes and cavernous craters. Why should we focus on something as seemingly dull as dust?

Dust can shield the sun to keep daytime temperatures cooler. And it acts like a blanket to keep nighttime temperatures warmer. Plus, particles of dust can act as the starting point for clouds to form, while dust storms can even force water vapor to escape into space.

Unlike on Earth, where it is washed out of the air by rain, dust can stay in Mars’ atmosphere for a long time, being blown all around the planet. So, for a better understanding of Mars’ climate, scientists are keen to understand when, where and how dust is lifted off the surface into the atmosphere.

Dust devils on Mars: Cratered surface near a canyon viewed from above with a dust devil.
The Colour and Stereo Surface Imaging System (CaSSIS) on board ESA’s ExoMars Trace Gas Orbiter (TGO) captured this dust devil tracking across the Martian surface on December 3, 2021. Image via ESA.

More data from dust devils on Mars

For this new study, researchers trained a neural network to recognize dust devils. Then they had it comb through images from Mars Express since 2004 and the ExoMars Trace Gas Orbiter (TGO) since 2016 to build up a catalog of 1,039 of them.

The map below shows the locations of all 1,039 dust devils, and the direction of motion for 373. It confirms that although dust devils are found all over Mars, even on its towering volcanoes, lots are swept up from certain source regions. For example, many were clustered in Amazonis Planitia (upper left of the map). This is a huge patch of Mars covered in a fine layer of dust and sand.

By tracking how fast the dust devils moved, the researchers found wind speeds of up to 44 meters a second, or 158 kilometers per hour (98 mph). This is faster than we’ve ever measured with rovers on the ground. It’s worth noting, though, that the Martian air is so thin that a human would barely even notice a wind of 100 kmh (62 mph) on Mars.

The researchers found that, in most cases, the dust devils were spinning across the landscape faster than our current Mars weather models predicted. In places where wind speeds are higher than expected, there may be more dust being lifted from the ground than we realized.

Like Earth, Mars has seasons. The catalog also highlights that dust devils are most common in the spring and summer of each hemisphere. They last a few minutes and typically happen during the daytime, peaking between about 11:00 and 14:00 local solar time.

This is very similar to what we see on Earth, where dust devils are most common in dry and dusty places in the late morning to early afternoon during the summer months.

Rolled-out map of Mars with very many tiny short lines in red, white, blue, and green pointing every which way.
View larger. | Map showing active dust devils during local spring and summer in Mars’ northern hemisphere (black and gray dots and arrows, respectively) and during spring and summer in the southern hemisphere (white and pink dots and arrows, respectively). Arrows show their direction of travel. Image via ESA.

Better picture, safer exploration

This kind of big-picture view requires a lot of data. And rovers and landers alone can’t capture it all. Until now, we’ve based our models of Mars’ climate on limited data from missions that don’t cover much of the planet’s surface.

Thanks to this study, we now have lots of new measurements from all over Mars. This helps to inform and refine the models. And it improves our understanding and predictions of wind patterns around the red planet. Valentin said:

Information on wind speeds and directions is also really important when planning the arrival of future landers and rovers at Mars. Our measurements could help scientists build up an understanding of wind conditions at a landing site before touchdown, which could help them estimate how much dust might settle on a rover’s solar panels, and therefore how often they should self-clean.

We’re already using dust information to plan our future missions. Our ExoMars Rosalind Franklin rover should touch down on Mars in 2030 to avoid landing during the planet’s global dust storm season.

Valentin emphasizes that:

… this catalog of dust devil tracks is already public and anybody can use it for their own research. More entries are being added over time. Mars Express and ExoMars TGO are collecting new images every day.

Now that we know where dust devils usually happen, we can direct more images to those exact places and times. We are also coordinating the missions to image the same dust devils at the same time, to be able to compare the movement measurements and validate the data.

View from above of 3 small vertical clouds on a cratered surface.
The Colour and Stereo Surface Imaging System (CaSSIS) on board ESA’s ExoMars Trace Gas Orbiter (TGO) captured these 3 dust devils tracking across the Martian surface on November 8, 2021. Image via ESA.

From noise to gold

Mars Express and ExoMars Trace Gas Orbiter (TGO) were never actually designed to measure wind speeds on Mars. Valentin’s team made use of a normally unwanted feature of the data to track the dust devils.

For both spacecraft, a single image is created by combining views from separate channels (each channel looks at Mars either in a specific color or from a specific direction, or both). By design, there is a small delay between the views. This delay causes no problems as long as the surface is static. However, it can cause slight color offsets in the final image whenever something is moving, such as clouds and dust devils. These offsets were exactly what the researchers were looking for. In Valentin’s words:

We turned image noise into valuable scientific measurements.

An imaging sequence from Mars Express combines up to nine image channels with a delay of about 7 to 19 seconds between each. During these delays, any dust devil passing below moves a short distance. And this allows the researchers to measure its speed. Because the study used five separate image channels, the team could even see how much the dust devil wobbled from left to right, as well as how its speed changed over time.

Images of dust devils on Mars

Images taken with ExoMars TGO’s CaSSIS combine two views taken either a second (for color images) or 46 seconds (for stereo images) apart. Though we can’t see any wobble or acceleration, the extra delay lets us see dust devils moving much farther between each image.

The first GIF below shows a dust devil photographed by ExoMars TGO with a one-second delay between views. The second GIF shows the same dust devil imaged with a 46-second delay.

Animation of a tornado-like dust devil moving near a large crater as viewed from above.
A 1-second delay: The CaSSIS instrument on board ESA’s ExoMars Trace Gas Orbiter captured this dust devil tracking across the Martian surface on February 28, 2019. Image via ESA.
Cratered surface from above, with 2 positions of a dust devil, animated.
A 46-second delay: The CaSSIS instrument, on board ESA’s ExoMars Trace Gas Orbiter, captured this dust devil tracking across the Martian surface on February 28, 2019. Image via ESA.

Colin Wilson, ESA project scientist for both missions, said:

It’s great to see researchers using Mars Express and ExoMars TGO for totally unexpected research. Dust affects everything on Mars, from local weather conditions to how well we can take images from orbit. It’s difficult to understate the importance of the dust cycle.

Bottom line: Using data from Mars missions, scientists have put together a catalog of dust devils on Mars that help track winds and troublesome dust.

Source: Dust devil migration patterns reveal strong near-surface winds across Mars

Via ESA

Read more: See one gigantic Mars dust devil eating another

The post Dancing dust devils on Mars trace raging winds first appeared on EarthSky.

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