ESA Captured Image of Elongated Martian Cloud
The European Space Agency imaged a vast water ice cloud stretching from Mars' Arsia Mons volcano on June 24, 2024.
Updated on Oct. 8, 2026 in Space

On June 24, 2024, the European Space Agency's Mars Express probe captured an image of the Arsia Mons Elongated Cloud. This water ice formation stretches up to 1,800 km downwind of the 20-km-tall volcano.
Why it matters
Researchers are studying the cloud to understand exotic physical processes like homogeneous nucleation that drive its daily growth and decay cycles on Mars.
The cloud forms downwind of the 20-km-tall Arsia Mons volcano through homogeneous nucleation, a process where water vapor turns directly into ice particles. This daily cycle occurs repeatedly over a region covering 780,000 square km.
The players
European Space Agency
This intergovernmental organization is responsible for space exploration and the operation of the Mars Express mission.
Mars Express
This is a long-standing space exploration mission that has been orbiting Mars to study its surface and atmosphere.
The details
The cloud appears, grows, and fades on a daily basis throughout the morning hours. Scientific analysis suggests that the height of the Arsia Mons volcano is instrumental in forcing the water vapor to nucleate into these massive, elongated structures.
Timeline
The Mars Express High Resolution Stereo Camera captured the cloud image on 24 June 2024.
The Big Picture
This observation follows a long-standing pattern of data collection set by the Mars Express mission's atmospheric monitoring program. By documenting these daily cycles, scientists refine planetary climate models that bridge the gap between Earth-based physics and Martian atmospheric behavior.
Understanding the unique nucleation processes that create these massive clouds provides researchers with critical data for future high-altitude weather modeling. This knowledge helps refine how scientists interpret complex atmospheric phenomena on other planets compared to Earth.
The takeaway
The recurring Arsia Mons cloud serves as a testament to the complex, daily weather cycles occurring on our neighbor planet. This discovery emphasizes that Martian weather is highly dynamic, driven by specific geological features that dictate atmospheric conditions.
Further reading
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