A huge wave has been spotted in the upper atmosphere of Venus, baffling scientists because it’s staying so still above the planet’s surface. Usually clouds in that region move at about 100 meters (328 feet) per second, whereas this cloud is stationary compared to the planet’s rotation.
New work suggests that the wave was created in the lower atmosphere when it flowed over a mountain, which would be similar to a phenomenon on Earth called a “gravity wave.” The feature, related to atmospheric flow over mountains, has nothing to do with the similarly named “gravitational wave,” which refers to space-time ripples in the early universe.
The new findings came from observations by Japan’s Akatsuki spacecraft, which has orbited Venus since 2015. The work was detailed yesterday (Jan. 16) in the journal Nature Geoscience, and it was led by Makoto Taguchi at Rikkyo University in Tokyo.
The standstill region is about 10,000 kilometers (6,213 miles) in diameter and hovers over mountains on the planet’s surface, shaped like a bow and very bright, the study’s authors said. The strange feature was observed by the Japanese Aerospace Exploration Agency’s Akatsuki spacecraft, which entered Venus’ orbit in late 2015.
Venus has been known for its weird cloud formations for more than 50 years. For example, a large Y-shaped feature was first observed in ultraviolet light; the Mariner 10 spacecraft in 1973 discovered that this feature was also moving independently of clouds in the same region. In 2015, scientists hypothesized it may be created by centrifugal forces, which draw things on a rotating body away from its rotating center, much like a centrifuge.
The European Space Agency also investigated the role of mountains in disturbing Venus’ atmosphere in 2016. Based on observations from the now-finished Venus Express mission, scientists found that air filled with water vapor rises up from the lower atmosphere as it moves over the planet’s mountains and creates gravity waves.
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