Unlocking the Secrets of Jupiter and Saturn: How Polar Cyclones Expose Hidden Interiors

A groundbreaking study by planetary scientists at the Massachusetts Institute of Technology (MIT) reveals how the significant differences in polar vortex patterns between Jupiter and Saturn are influenced by the unique properties of their deep interiors. These findings offer valuable insights into the structure of these gas giants.

This composite image, captured by the JIRAM instrument aboard NASA’s Juno satellite, depicts a central low-pressure system at Jupiter’s north pole along with eight surrounding low-pressure systems. The colors in this image represent radiant heat, revealing temperature variations in their cloud layers. Image credit: NASA / JPL-Caltech / SwRI / ASI / INAF / JIRAM.

“Our study shows that the internal properties, including the softness of the vortex base, influence the fluid patterns observed at the surface,” explained Dr. Wang-Ying Kang from MIT.

The research was inspired by stunning images of Jupiter and Saturn obtained from NASA’s Juno and Cassini missions.

Since 2016, Juno has been orbiting Jupiter and revealing astonishing details about its north pole and intricate spiral formations.

The data suggest that each vortex on Jupiter is immense, measuring around 5,000 km (3,000 miles) in diameter.

Meanwhile, Cassini documented Saturn’s iconic polar vortex, which spans a singular hexagonal shape approximately 29,000 km (18,000 miles) wide, before its controlled descent into Saturn’s atmosphere in 2017.

“Despite their similarities in size and primary composition of hydrogen and helium, deciphering the differences in polar vortices between Jupiter and Saturn has been challenging,” noted MIT graduate student Jial Shi.

Researchers aimed to uncover the physical mechanisms behind the formation of either a single vortex or multiple vortices on these distant planets.

To achieve this, they employed a two-dimensional model of surface fluid dynamics.

While polar vortices are inherently three-dimensional, the fast rotation of Jupiter and Saturn leads to uniform motion along their rotational axes, allowing the team to effectively analyze vortex evolution in two dimensions.

“In rapidly rotating systems, fluid motion tends to be uniform along the axis,” Dr. Kang added. “This insight allowed us to convert a 3D challenge into a 2D problem, significantly speeding up simulations and reducing costs.”

With this in mind, researchers created a two-dimensional model of vortex behavior in gas giants, adapting equations that describe the evolution of swirling fluids over time.

“This equation is commonly used in various situations, including modeling cyclones on Earth,” Dr. Kang stated. “We tailored it for the polar regions of Jupiter and Saturn.”

Scientists applied the two-dimensional model to simulate fluid dynamics on gas giants in various scenarios, adjusting parameters such as planetary size, rotational speed, internal heating, and the characteristics of the fluid.

They introduced random “noise” to simulate initial chaotic fluid flow on the planets’ surfaces.

By analyzing how this fluid evolved over time across different scenarios, the researchers found that some conditions led to the formation of a single large polar vortex, akin to Saturn’s structure, while others resulted in multiple smaller vortices, similar to those on Jupiter.

Through careful examination of the parameters affecting each scenario, the study identified a unifying mechanism: the softness of the vortex base constrains the size that vortices can attain.

The softer and lighter the gas at the bottom of the vortex, the smaller the resulting vortex, enabling multiple smaller vortices to exist at Jupiter’s poles. Conversely, a denser and harder base permits the growth of sizable vortices, manifesting as a singular entity like Saturn.

If this mechanism holds for both gas giants, it could suggest that Jupiter has a softer internal composition, while Saturn may contain denser materials.

“The fluid patterns we observe on the surface of Jupiter and Saturn may provide insights into their interior compositions,” Shi remarked.

“This is crucial because Saturn’s interior likely harbors richer metals and more condensable materials, leading to stronger stratification than that found in Jupiter,” Shi added. “This will enhance our understanding of gas giant planets.”

The team’s findings will be published in the Proceedings of the National Academy of Sciences.

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Gial Sea & One In Can. 2026. Polar vortex dynamics of gas giant planets: Insights from 2D energy cascades. PNAS in press.

Source: www.sci.news

Researchers examine how tides impact the interiors of planets and moons

A team of scientists from the University of Arizona, Delft University of Technology, and the California Institute of Technology's Lunar and Planetary Institute has developed a new method to calculate how tides affect the interiors of the solar system's planets and moons. Importantly, they investigated the effects of internal tides on objects that do not have perfectly spherical internal structures.

Europa's surface stands out in this newly reprocessed color view. Image scale is 1.6 km per pixel. North of Europe is on the right. Image credit: NASA / JPL-Caltech / SETI Institute.

Celestial tides refer to the deformations that celestial bodies experience when they interact with other bodies due to gravity.

Consider how Jupiter's powerful gravity pulls on its icy moon Europa.

Because Europa's orbit is not circular, the overwhelming gravitational pressure on Jupiter's moons changes as it moves along Jupiter's orbit.

When Europa is closest to Jupiter, the planet's gravity is most felt.

The energy of this deformation heats Europa's interior, allowing an ocean of liquid water to exist beneath the moon's icy surface.

“The same is true for Saturn's moon Enceladus,” says Dr. Alexander Byrne, a researcher at the California Institute of Technology.

“Enceladus has an ice shell that is expected to have much more aspherical symmetry than Europa.”

The body tides experienced by celestial bodies influence how the world evolves over time and, in cases like Europa and Enceladus, its potential habitability for life as we know it. may give.

“The tidal response of spherically symmetric objects has the same wavelength as the tidal forces. Lateral inhomogeneities generate additional tidal responses with spectra that depend on the spatial pattern of such fluctuations.” the researchers said.

“For Mercury, the Moon, and Io, the amplitude of this signal is as much as 1-10% of the dominant tidal response to long-wavelength shear modulus fluctuations, which exceed about 10% of the mean shear modulus.”

“For Europa, Ganymede, and Enceladus, a shell thickness variation of 50% of the average shell thickness could result in an additional signal of about 1% and about 10% for Jupiter's moons and Enceladus, respectively.”

The authors also discussed how their results can help scientists interpret observations made by missions to a variety of different worlds, from Mercury to the moon to the outer planets of our solar system. .

“Future missions such as BepiColombo and JUICE have the potential to measure these signals,” they said.

“Lateral changes in viscosity affect the distribution of tidal heating.”

“This may promote the thermal evolution of tidal bodies and influence the distribution of active areas.”

of findings will appear in Planetary Science Journal.

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Mark Rovira-Navarro others. 2024. A spectral method for calculating the tides of laterally inhomogeneous objects. planet. Science. J 5, 129; doi: 10.3847/PSJ/ad381f

This article is a version of a press release provided by NASA.

Source: www.sci.news