Martian mini-twisters: The atmospheric engines driving the Red Planet's weather

Martian Dust Devils | National Geographic · 3:45 · Video: National Geographic · Watch at the source

In short: Watch a larger Martian dust devil consume a smaller one in a rare atmospheric interaction. These convective vortices are more than just visual spectacles; they are critical drivers of the Martian dust cycle and climate.

Dust devils form when surface air is heated by the ground, causing it to rise rapidly through cooler air and begin to rotate. As this air rushes inward, it accelerates—much like a spinning ice skater pulling in their arms—and picks up surface dust. These vortices are key elements of the Planetary Boundary Layer, the lowest part of the atmosphere, where they mix heat, momentum, and chemical species.

Researchers use rovers like Perseverance to study these 'fiendish' phenomena because they are primary lifting mechanisms for Martian dust. Understanding these dynamics is essential for predicting dust storms and modeling the planet's climate. On January 25, 2025, Perseverance captured a larger dust devil, approximately 210 feet wide, consuming a smaller 16-foot-wide vortex near the rim of Jezero Crater.

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