Why does Jupiter change its stripes? Scientists may finally have the answer

two infrared photos of jupiter showing the planet's cloud bands in shades of red and orange.
Two infrared images of Jupiter taken approximately 10 years apart by a ground-based telescope demonstrate the changes in the planet's bands over time. (Image credit: Arrate Antuñano/NASA/IRTF/NSFCam/SpeX)

When you picture Jupiter, you probably see a planet with orange and reddish bands and the famous Great Red Spot staring at you like a giant eye. 

But did you know those famous bands are ever-changing in size, color and location? Every four to five years, Jupiter changes its stripes, and ever since Galileo Galilei observed them in the 17th century, scientists have wondered why.

What we do know is that each band, consisting of clouds of ammonia and water in a hydrogen and helium atmosphere, corresponds to strong winds blowing east or west. Scientists have also linked the bands, which reach more than 1,000 miles (1,600 kilometers) deep into Jupiter's atmosphere, to changes in infrared variations within the planet. But a team of researchers has just discovered another important clue, and it all comes down to Jupiter's magnetic field.

Related: Jupiter, the solar system's largest planet (photos)

Using data from NASA's Jupiter-orbiting Juno spacecraft, the team correlated the variations in the gas giant's bands to changes in its magnetic field. 

"It is possible to get wavelike motions in a planetary magnetic field, which are called torsional oscillations. The exciting thing is that, when we calculated the periods of these torsional oscillations, they corresponded to the periods that you see in the infrared radiation on Jupiter," study co-author Chris Jones, a professor in the School of Maths at the University of Leeds in England, said in a statement.

As it goes in the science world, this discovery produces even more mysteries. 

"There remain uncertainties and questions, particularly how exactly the torsional oscillation produces the observed infrared variation, which likely reflects the complex dynamics and cloud/aerosol reactions. Those need more research," study lead author Kumiko Hori, formerly of the University of Leeds and currently of Kobe University in Japan, said in the same statement. 

"Nonetheless, I hope our paper could also open a window to probe the hidden deep interior of Jupiter, just like seismology does for the Earth and helioseismology does for the sun," Hori said.

The team's research was published on May 18 in the journal Nature Astronomy.

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Stefanie Waldek
Contributing writer

Space.com contributing writer Stefanie Waldek is a self-taught space nerd and aviation geek who is passionate about all things spaceflight and astronomy. With a background in travel and design journalism, as well as a Bachelor of Arts degree from New York University, she specializes in the budding space tourism industry and Earth-based astrotourism. In her free time, you can find her watching rocket launches or looking up at the stars, wondering what is out there. Learn more about her work at www.stefaniewaldek.com.

  • Classical Motion
    How much energy can the sun deposit on Jupiter? How much energy can the magnetic field induce at the poles with the solar charge wind? Heating the equator would coriolis the atmosphere like here. And spread heat and travel to the poles.

    But, if it were heated at the poles......we should get climate bands instead. The only coriolis is at the boundaries of temp or density bands. A banded atmosphere.
    Reply
  • billslugg
    Sun deposits 1366 watts/m^2 on Earth.
    It will vary by the inverse square of the distance from the Sun.
    Earth is at 1 AU, Jupiter at 5.2 AU.
    Jupiter insolation is thus: (1366 w/m^2 ) x (1/5.2)^2 = 50 watts per square meter but this strikes only on one side of Jupiter. Averaged over the entire surface area the insolation number must be multiplied by .2488. So Jupiter gets about 12 watts/m^2 from the Sun, of which half is reflected, meaning only 6.6 goes in. But 14 goes out. The remaining 7 is internal heat.

    Here is some data:
    Jupiter’s radiant energies and internal heat
    Parameter Power
    Reflected solar radiation 6.693 ± 0.160 W m−2
    Absorbed solar radiation 6.613 ± 0.160 W m−2
    Emitted thermal radiation 14.098 ± 0.031 W m−2
    Internal heat 7.485 ± 0.163 W m−2

    https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6137063/
    Reply