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Ever-Changing Venus Superstorm Sparks Interest

Infrared Radiation from Storm Circling Venus South Pole
Infrared radiation from the cyclonelike storm circling the south pole of Venus. White regions show cooler, high-altitude clouds. (Image credit: ESA/VIRTIS-VenusX/INAF-IASF/LESIA-Obs. de Paris (G. Piccioni, INAF-IASF))

Elements of a giant cyclone circling above the south pole of Venus constantly break apart and re-form, according to new research. Scientists studying observations of the planet taken over the last six years have concluded that the long-lived storm is constantly evolving, raising even more questions about the unusual weather formation.

A storm on the move

When the European Space Agency's Venus Express satellite arrived at the hot planet in April 2006, it observed a cyclonelike structure above Venus' south pole, four times as large as similar storms on Earth. Over the past six years, the spacecraft has collected daily observations about the storm, which resembles one spotted over Venus' north pole by NASA's Pioneer Venus spacecraft in 1979.

"Both vortices are probably permanent features in the atmosphere of Venus," planetary scientist Itziar Garate-Lopez, of the University of the Basque Country in Spain, told by email.

The South Polar Vortex of Venus changes its shape day-to-day. The upper panels of the figure show the upper clouds at 63km above the surface and the lower panels present the vortex as observed in the lower clouds at 42km altitude level. (Image credit: ESA/VIRTIS/INAF-IASF/Obs. de Paris-LESIA/Universidad del País Vasco (I. Garate-Lopez))

Using the observations taken by Venus Express, Garate-Lopez and her team concluded that the giant storm is in constant flux. Elements of the vortex are constantly breaking apart and reforming as it circles every 2.2 days. [Amazing Venus Photos by ESA's Venus Express]


The cause for the constant evolution remains a puzzle that the team still hopes to solve.

Using the spacecraft's Visible and Infrared Thermal Imaging Spectrometer (VIRTIS), the scientists probed the upper and lower layers of the planet's atmosphere. They concluded that the two centers of rotation of the 12-mile-high (20 kilometers) storm, which exist at different altitudes, rarely line up, a surprising find.

"Even if the small-scale structures are different at both altitude levels, the overall morphology of the vortex is conserved, so we thought that the vortex should move as one large-scale feature in the same way in both vertical layers," Garate-Lopez said. "However, this is not the case."

The constantly shifting centers create what Garate-Lopez calls a "twisted tube" in the vortex.

Although VIRTIS can observe the upper and lower layers of the atmosphere, the middle section remains hidden, keeping the team from more fully understanding the off-kilter movement.

The results were published online today (Mar 24) in the journal Nature Geoscience.

A close-up view of the powerful double-eyed storm over the south pole of Venus. (Image credit: ESA/VIRTIS/INAF-IASF/Obs. de Paris-LESIA)

A bizarre atmosphere

Venus spins slowly on its axis, taking 243 Earth-days for the sun to rise and set once. But Venus' atmosphere moves significantly faster, circling the planet once every four Earth days.

"The main unsolved question about the atmosphere of Venus is precisely the reason why it super-rotates much faster than the solid planet," Garate-Lopez said.

The relationship between the oddly moving atmosphere and the vortices also remains a mystery.

The cyclone sits 26 miles (42 km) above the surface of the planet. No rain falls from the towering storm, because the planet's atmosphere evaporates all particles within 22 miles (35 km) of the ground. Winds are also inconsequential far beneath the storm.

"If we were at Venus' south pole, we may observe a permanent whirl of clouds high above our heads, with no consequences at the surface," Garate-Lopez said.

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Nola Taylor Redd
