Lurking just below the atmosphere of Venus is a wall of acid clouds that whip around the planet at speeds close to that of a commercial air jet on Earth.
The newly discovered atmospheric "feature" looms about 31 miles (50 kilometers) below the thick cloud tops of Venus and is extensive, sometimes stretching as far as 4,660 miles (7,500 km) across the equator and mid-latitudes of Venus. And it's been there for at least three decades.
It may seem odd that such a huge feature went undiscovered for so long, given that spacecraft have visited Venus sporadically since 1962, and high-resolution telescopes have been gazing at the planet for years before that. And the first hint that something strange was happening came from the Japanese Akatsuki spacecraft that has been orbiting Venus since 2015.
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It took a new survey of archival footage, however, to determine the cloud wall has been there since at least 1983. "We needed access to a large, growing and scattered collection of images of Venus gathered in recent decades with different telescopes," study co-author Pedro Machado, a researcher with Portugal's Institute of Astrophysics and Space Sciences, said in a statement.
The archival footage came from observatories including the Galileo National Telescope in the Canary Islands and the NASA Infrared Telescope Facility in Hawaii.
Enormous cloud patterns in the upper atmosphere are already well-known at Venus, including a bizarre "Y" shape that may arise from centrifugal forces, and a bow wave that could arise from air flow over static ground features like mountains. The newly discovered cloud wall, however, is at a lower altitude and in a region of Venus' atmosphere where the greenhouse effect is quite pronounced, keeping the surface at lead-melting temperatures of 870 degrees Fahrenheit (465 degrees Celsius).
Researchers suggest the cloud wall could be linked to the mysterious and long-observed fast rotation in Venus' upper atmosphere. The newly found feature could potentially dump enough momentum and energy to fuel the fast winds further up, lead author Javier Peralta, an astrophysicist at the Japanese Aerospace Exploration Agency (JAXA, which runs the Akatsuki mission), said in the same statement. That's because the cloud wall zooms above the surface at jet-like speeds of 203 miles (328 km) an hour.
What causes the cloud wall is still unknown and will require further research, the team said. However, the researchers added, the feature could be an atmospheric "Kelvin" wave, a class of atmospheric gravity waves that has already been observed at Venus. Gravity waves in a planet's atmosphere (not to be confused with gravitational waves) happen when winds move at high speed over static geological features like a crater wall or a mountain; the updraft rises and sinks in a layer of stable air just above the feature.
A study based on the research was published on May 27 in the journal Geophysical Research Letters.
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The greenhouse effect is the entrapment of insolation due to gases behaving like a greenhouse obviously, and the paper mention it as well as use a global circulation model that takes that into account when they reproduce the phenomena.
"The clouds of Venus are mostly composed of H2SO4‐H2O droplets and are stratified into three layers (Titov et al., 2018). In the upper clouds (56.5–70 km above the surface), absorbers of known and unknown composition are responsible for the dark markings observed in ultraviolet images and for most of the absorption of the solar energy not reflected by the clouds (Titov et al., 2018). The middle and lower clouds (hereafter, simply named deeper clouds ) are within 47.5–56.5 km and importantly contribute to the greenhouse effect and the radiative energy balance. "
Since the current man made global warming that we observe has been politicized in mainly US and so one can see partial or fully misunderstood physics being expressed, it is perhaps not superfluous to remark that these global circulation model are used to understand current Earth, Archean Earth with different atmosphere, and other planets with substantial atmosphere such as Venus.