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Mars's Oddest Cloud Just Got Odder

Mars's Oddest Cloud Just Got Odder

Author: Roggie D/Wednesday, November 11, 2026/Categories: Astronomy, Atmospheric Phenomena

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Image: the Arsia Mons Elongated Cloud, imaged by Mars Express. Credit: ESA/DLR/FU Berlin/J. Cowart (share-alike).

CASE FILE No. 002 · RRH-CF-002
SOLVED

The cloud is real and well measured. A 2026 meteorological model only grows an AMEC-like plume when homogeneous ice nucleation is included. That strongly suggests the mechanism. It does not prove it.

Every southern spring and summer morning on Mars, a white water-ice cloud grows downwind of Arsia Mons, a volcano about 20 kilometers (12 miles) high. It stretches for up to roughly 1,800 kilometers (about 1,100 miles), then evaporates before most afternoon orbiters ever see it. It does this day after day for months.

ESA's Mars Express has been watching that show for years. On October 7, 2026, ESA and a Nature Geoscience team said the physics behind it may be stranger than the postcard.

What happened

The feature has a name that sounds like a catalog number and behaves like a recurring character: the Arsia Mons Elongated Cloud, or AMEC. Mars Express made it famous in 2018. A 2021 observational study mapped its life cycle across instruments from ESA, NASA, Viking-era archives, and India's Mars Orbiter Mission. That study also found that NASA's Viking 2 had already partially imaged the same kind of veil in the 1970s.

Fact: It is an orographic water-ice cloud, meaning wind is forced up and over topography, cooling as it rises, the same family of cloud you get on Earth when moist air climbs a mountain.

Fact: At its largest it has been measured about 1,800 km long and about 150 km across, forming near about 45 km altitude, expanding westward for roughly two and a half hours at over 600 kilometers per hour, then detaching and fading by late morning.

Fact: It prefers southern spring and summer (solar longitude roughly 220 to 320 degrees), a dusty season when low-latitude clouds are otherwise scarce. Arsia Mons is the odd volcano out for hosting this veil then.

The trouble was not that nobody could see it. The trouble was that standard Mars weather models refused to grow a cloud that looked like the one in the pictures.

Why it matters

Clouds on Earth and Mars usually form the polite way: heterogeneous nucleation. Water vapor needs something to cling to (dust, salt, soot, pollen). On Mars, dust is the usual suspect.

The new work, led by Jorge Hernández-Bernal (LMD/CNRS/Sorbonne Université), says that to make an AMEC-like cloud in their meteorological model they had to switch on homogeneous ice nucleation: vapor freezing into ice particles with no solid seed. ESA quotes the lead author calling that textbook theory that is "usually thought not to happen in nature," and "wholly unexpected" in a planetary atmosphere.

The published Nature Geoscience paper is careful. Its title says the process is "suggested" by the elongated clouds, and the abstract says the result "strongly suggests" that homogeneous ice nucleation from water vapor occurs on Mars. An earlier open preprint used stronger language ("demonstrates," "first evidence"). This file follows the published wording.

Fact (mechanism proposed): Winds past Arsia Mons drive a powerful wave that lofts moist air several kilometers in minutes. Temperatures can drop by about 30°C (54°F) in roughly ten minutes. Relative humidity spikes to extremes far beyond everyday Earth experience. Vapor then freezes spontaneously into cloud ice. ESA's release popularizes those humidity extremes as more than 100,000 times everyday Earth levels. That figure is ESA's wording, not a lab measurement from inside the cloud.

Claim / interpretation, label this clearly: That homogeneous nucleation is occurring on Mars is a strong scientific inference from model-observation agreement, not a lab measurement taken inside the cloud. ESA's own release notes that some aspects of the modeled cloud still do not exactly match the images.

Why should you care if you don't live on a Tharsis volcano? Because cloud rules that we treat as universal get stress-tested on other worlds. If Mars can hit the weird corner of the phase diagram, exoplanet atmospheres might too. Exotic physics is not a plot twist reserved for fiction. Sometimes it is what the data demand.

What's still uncertain

Homogeneous nucleation has been suggested for parts of Earth's and Venus's upper atmospheres, but it has not been clearly spotted there. Extreme supersaturation is rare for a reason.

We still do not have an in-situ, particle-by-particle autopsy of AMEC ice. The model wins by reproducing morphology and timing that heterogeneous-only runs missed, which is powerful, and still one step removed from catching vapor mid-freeze. Remaining mismatches between model and image are an open invitation for the next orbit of Mars Express cameras (VMC, HRSC, OMEGA) and for rival models to try to break the result.

So the case file stamp is SOLVED for what the cloud is: a real, recurring, orographic water-ice plume, measured at up to about 1,100 miles. The homogeneous-nucleation story is the leading formation explanation, because the simulations do not grow this cloud without it. The stamp is not "every ice crystal on Mars is now explained," and it is not a closed physics textbook. Stay curious about the mismatches. That is where the next paper lives.

What's your bet: rare Mars physics that Earth just never hosts at this scale, or a process we will eventually catch closer to home once we look harder?

Stay curious. Question everything. See where the rabbit hole leads.

GO DEEPER
  1. VT J1906+0849 · RRH-CF-001. Another rules-don't-fit sky object: a Galactic radio transient that switched on, faded, and came back.
  2. Earth orographic clouds vs AMEC · Same mountain-wave family, very different length and morning-only drama. Future RRH short; no live article yet.
  3. Homogeneous vs heterogeneous nucleation · Classroom physics that just got a planetary field test. Future short; no live article yet.
  4. The Flannan Isles Keepers · Existing RRH Case File No. 003. Different domain, same habit: keep the claim no stronger than the record.
CASE REOPENED when new evidence lands, this file gets an update stamp.

Sources

  1. ESA Mars Express, "Mars's oddest cloud may be even odder than we thought," Oct. 7, 2026. https://www.esa.int/articles/about-us/directorates/science/mars-express/mars-s-oddest-cloud-may-be-even-odder-than-we-thought
  2. Hernández-Bernal et al., "Homogeneous ice nucleation from water vapour suggested by elongated clouds on Mars," Nature Geoscience, Oct. 7, 2026. https://doi.org/10.1038/s41561-026-02089-9 · https://www.nature.com/articles/s41561-026-02089-9
  3. Open preprint of the same study, arXiv:2609.37259. https://arxiv.org/abs/2609.37259
  4. Hernández-Bernal et al., "An Extremely Elongated Cloud over Arsia Mons Volcano on Mars: I. Life Cycle," JGR Planets, 2021. https://arxiv.org/abs/2103.03919 (Wiley DOI: https://doi.org/10.1029/2020JE006517)
  5. ESA Mars Express, "Mars Express unlocks the secrets of curious cloud," March 9, 2021. https://www.esa.int/articles/about-us/directorates/science/mars-express/mars-express-unlocks-the-secrets-of-curious-cloud
  6. ESA image page, "Mars Express views the most striking cloud on Mars." https://www.esa.int/media/the-arsia-mons-elongated-cloud-as-seen-by-mars-express

Fact note: The published Nature Geoscience paper says the result strongly suggests homogeneous nucleation. An earlier preprint used stronger language. This article follows the published wording: a lead, not a verdict.

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