NASA’s Webb Exposes Complex Atmosphere of Starless Super-Jupiter

NASA’s Webb Exposes Complex Atmosphere of Starless Super-Jupiter

6 Min Read

NASA’s Webb Exposes Complex Atmosphere of Starless Super-Jupiter

Illustration of a large spherical object that looks like a gas giant planet or a brown dwarf. The object appears to be glowing, with wavy, horizontal bands of yellow, orange, and red forming patterns similar to those in the atmosphere of Jupiter. In the mid-latitudes of the northern hemisphere, just to the right of center, is a large, elliptical, dark red feature similar to Jupiter’s Great Red Spot. Hints of a blue-green auroral glow emanate from the south pole. Larger blue-green auroral arcs descend from the north pole down toward the middle northern latitudes. The background is filled with with thousands of distant stars that form a Milky Way-like band running from left to light. The object is isolated, with no host star nearby. The words “Artist’s Concept” are in the lower left corner of the illustration.
This artist’s concept shows what the isolated planetary-mass object SIMP 0136 could look like based on recent observations from NASA’s James Webb Space Telescope and previous observations from Hubble, Spitzer, and numerous ground-based telescopes.
Credits:
NASA, ESA, CSA, and Joseph Olmsted (STScI)

An international team of researchers has discovered that previously observed variations in brightness of a free-floating planetary-mass object known as SIMP 0136 must be the result of a complex combination of atmospheric factors, and cannot be explained by clouds alone.

Using NASA’s James Webb Space Telescope to monitor a broad spectrum of infrared light emitted over two full rotation periods by SIMP 0136, the team was able to detect variations in cloud layers, temperature, and carbon chemistry that were previously hidden from view.

The results provide crucial insight into the three-dimensional complexity of gas giant atmospheres within and beyond our solar system. Detailed characterization of objects like these is essential preparation for direct imaging of exoplanets, planets outside our solar system, with NASA’s Nancy Grace Roman Space Telescope, which is scheduled to begin operations in 2027.

Rapidly Rotating, Free-Floating

SIMP 0136 is a rapidly rotating, free-floating object roughly 13 times the mass of Jupiter, located in the Milky Way just 20 light-years from Earth. Although it is not classified as a gas giant exoplanet — it doesn’t orbit a star and may instead be a brown dwarf — SIMP 0136 is an ideal target for exo-meteorology: It is the brightest object of its kind in the northern sky. Because it is isolated, it can be observed with no fear of light contamination or variability caused by a host star. And its short rotation period of just 2.4 hours makes it possible to survey very efficiently.

Prior to the Webb observations, SIMP 0136 had been studied extensively using ground-based observatories and NASA’s Hubble and Spitzer space telescopes.

“We already knew that it varies in brightness, and we were confident that there are patchy cloud layers that rotate in and out of view and evolve over time,” explained Allison McCarthy, doctoral student at Boston University and lead author on a study published today in The Astrophysical Journal Letters. “We also thought there could be temperature variations, chemical reactions, and possibly some effects of auroral activity affecting the brightness, but we weren’t sure.”

To figure it out, the team needed Webb’s ability to measure very precise changes in brightness over a broad range of wavelengths.

Graphic A: Isolated Planetary-Mass Object SIMP 0136 (Artist’s Concept)

Illustration of a large spherical object that looks like a gas giant planet or a brown dwarf. The object appears to be glowing, with wavy, horizontal bands of yellow, orange, and red forming patterns similar to those in the atmosphere of Jupiter. In the mid-latitudes of the northern hemisphere, just to the right of center, is a large, elliptical, dark red feature similar to Jupiter’s Great Red Spot. Hints of a blue-green auroral glow emanate from the south pole. Larger blue-green auroral arcs descend from the north pole down toward the middle northern latitudes. The background is filled with with thousands of distant stars that form a Milky Way-like band running from left to light. The object is isolated, with no host star nearby. The words “Artist’s Concept” are in the lower left corner of the illustration.
This artist’s concept shows what the isolated planetary-mass object SIMP 0136 could look like based on recent observations from NASA’s James Webb Space Telescope and previous observations from Hubble, Spitzer, and numerous ground-based telescopes. Researchers used Webb’s NIRSpec (Near-Infrared Spectrograph) and MIRI (Mid-Infrared Instrument) to measure subtle changes in the brightness of infrared light as the object completed two 2.4-hour rotations. By analyzing the change in brightness of different wavelengths over time, they were able to detect variability in cloud cover at different depths, temperature variations in the upper atmosphere, and changes in carbon chemistry as different sides of the object rotated in and out of view. This illustration is based on Webb’s spectroscopic observations. Webb has not captured a direct image of the object.
NASA, ESA, CSA, and Joseph Olmsted (STScI)

Charting Thousands of Infrared Rainbows

Using NIRSpec (Near-Infrared Spectrograph), Webb captured thousands of individual 0.6- to 5.3-micron spectra — one every 1.8 seconds over more than three hours as the object completed one full rotation. This was immediately followed by an observation with MIRI (Mid-Infrared Instrument), which collected hundreds of spectroscopic measurements of 5- to 14-micron light — one every 19.2 seconds, over another rotation.

The result was hundreds of detailed light curves, each showing the change in brightness of a very precise wavelength (color) as different sides of the object rotated into view.

“To see the full spectrum of this object change over the course of minutes was incredible,” said principal investigator Johanna Vos, from Trinity College Dublin. “Until now, we only had a little slice of the near-infrared spectrum from Hubble, and a few brightness measurements from Spitzer.”

The team noticed almost immediately that there were several distinct light-curve shapes. At any given time, some wavelengths were growing brighter, while others were becoming dimmer or not changing much at all. A number of different factors must be affecting the brightness variations.

“Imagine watching Earth from far away. If you were to look at each color separately, you would see different patterns that tell you something about its surface and atmosphere, even if you couldn’t make out the individual features,” explained co-author Philip Muirhead, also from Boston University. “Blue would increase as oceans rotate into view. Changes in brown and green would tell you something about soil and vegetation.”

Graphic B: Isolated Planetary-Mass Object SIMP 0136 (NIRSpec Light Curves)

Infographic titled “Isolated Planetary-Mass Object SIMP 0136, Change in Brightness as Object Rotates, NIRSpec Time-Series Spectroscopy” with graph of Relative Brightness near-infrared emitted light on y-axis (brighter toward top) versus Time on July 23, 2023, Coordinated Universal Time (UTC) on x-axis (ranging from 7 to 10:15 PM). Three curves plotted. Red: Light from deep iron cloud layer. Yellow: Light from high silicate cloud layer. Blue: Light related to temperature high above the clouds. Curves overlap; each has different shape, with peaks and valleys of different size occurring at different times. Below curves are illustrations showing visible face of rotating object at beginning, middle, and end of 2.4-hour rotation period. To right of graph is atmosphere diagram showing red arrows coming up from deep iron cloud layer at 10 bars, yellow arrows coming from high silicate cloud layer at 1 bar, and blue arrows at top of atmosphere.
These light curves show the change in brightness of three different sets of wavelengths (colors) of near-infrared light coming from the isolated planetary-mass object SIMP 0136 as it rotated. The light was captured by Webb’s NIRSpec (Near-Infrared Spectrograph), which collected a total of 5,726 spectra — one every 1.8 seconds — over the course of about 3 hours on July 23, 2023. The variations in brightness are thought to be related to different atmospheric features — deep clouds composed of iron particles, higher clouds made of tiny grains of silicate minerals, and high-altitude hot and cold spots — rotating in and out of view. The diagram at the right illustrates the possible structure of SIMP 0136’s atmosphere, with the colored arrows representing the same wavelengths of light shown in the light curves. Thick arrows represent more (brighter) light; thin arrows represent less (dimmer) light.
NASA, ESA, CSA, and Joseph Olmsted (STScI)

Patchy Clouds, Hot Spots, and Carbon Chemistry

To figure out what could be causing the variability on SIMP 0136, the team used atmospheric models to show where in the atmosphere each wavelength of light was originating.

“Different wavelengths provide information about different depths in the atmosphere,” explained McCarthy. “We started to realize that the wavelengths that had the most similar light-curve shapes also probed the same depths, which reinforced this idea that they must be caused by the same mechanism.”

One group of wavelengths, for example, originates deep in the atmosphere where there could be patchy clouds made of iron particles. A second group comes from higher clouds thought to be made of tiny grains of silicate minerals. The variations in both of these light curves are related to patchiness of the cloud layers.

A third group of wavelengths originates at very high altitude, far above the clouds, and seems to track temperature. Bright “hot spots” could be related to auroras that were previously detected at radio wavelengths, or to upwelling of hot gas from deeper in the atmosphere.

Some of the light curves cannot be explained by either clouds or temperature, but instead show variations related to atmospheric carbon chemistry. There could be pockets of carbon monoxide and carbon dioxide rotating in and out of view, or chemical reactions causing the atmosphere to change over time.

“We haven’t really figured out the chemistry part of the puzzle yet,” said Vos. “But these results are really exciting because they are showing us that the abundances of molecules like methane and carbon dioxide could change from place to place and over time. If we are looking at an exoplanet and can get only one measurement, we need to consider that it might not be representative of the entire planet.”

This research was conducted as part of Webb’s General Observer Program 3548.

The James Webb Space Telescope is the world’s premier space science observatory. Webb is solving mysteries in our solar system, looking beyond to distant worlds around other stars, and probing the mysterious structures and origins of our universe and our place in it. Webb is an international program led by NASA with its partners, ESA (European Space Agency) and CSA (Canadian Space Agency).

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View/Download the research results from The Astrophysical Journal Letters.

Media Contacts

Laura Betz – laura.e.betz@nasa.gov
NASA’s Goddard Space Flight Center, Greenbelt, Md.

Margaret W. Carruthersmcarruthers@stsci.edu
Space Telescope Science Institute, Baltimore, Md.

Hannah Braunhbraun@stsci.edu
Space Telescope Science Institute, Baltimore, Md.

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NASA Marks 110 Years Since Founding of Predecessor Organization

NASA Marks 110 Years Since Founding of Predecessor Organization

2 min read

Preparations for Next Moonwalk Simulations Underway (and Underwater)

To celebrate the 110th anniversary of the organization that ultimately became NASA, the agency released a new collection of videos to highlight the history of the National Advisory Committee for Aeronautics (NACA) and the ways it transformed flight over four decades.

A new video collection highlights the history and significance of NASA’s predecessor organization.

Not long after the beginning of World War I, the United States Congress, concerned that America was lagging behind other countries, created a new committee to advance the nation’s flight technology development. On March 3, 1915, the NACA was founded “to supervise and direct the scientific study of the problems of flight, with a view to their practical solution.”

While the NACA began as a committee of only 12 leaders representing government, military, and industry, it rapidly expanded through World War II to develop America’s flight capabilities for defense and commercial uses. The organization became home to some of the nation’s best and brightest aeronautical engineers and world-class facilities, transforming into NASA at the dawn of the Space Age in 1958.

The new video collection highlights some of NACA’s striking historic photography and celebrates this pioneering organization with a brief history of its formation, expansion, and groundbreaking aeronautics research at four centers across the United States — the current homes of NASA’s Langley Research Center in Hampton Virginia, Ames Research Center in California’s Silicon Valley, Glenn Research Center in Cleveland, and Armstrong Flight Research Center in Edwards, California.

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Michele Ostovar

Touchdown! Carrying NASA Science, Firefly’s Blue Ghost Lands on Moon

Touchdown! Carrying NASA Science, Firefly’s Blue Ghost Lands on Moon

First image captured by Firefly's Blue Ghost lunar lander, taken shortly after confirmation of a successful landing at Mare Crisium on the Moon's near side. This is the second lunar delivery of NASA science and tech instruments as part of the agency's Commercial Lunar Payload Services initiative.
First image captured by Firefly’s Blue Ghost lunar lander, taken shortly after confirmation of a successful landing at Mare Crisium on the Moon’s near side. This is the second lunar delivery of NASA science and tech instruments as part of the agency’s Commercial Lunar Payload Services initiative.
Credit: Firefly Aerospace

Carrying a suite of NASA science and technology, Firefly Aerospace’s Blue Ghost Mission 1 successfully landed at 3:34 a.m. EST on Sunday near a volcanic feature called Mons Latreille within Mare Crisium, a more than 300-mile-wide basin located in the northeast quadrant of the Moon’s near side.

The Blue Ghost lander is in an upright and stable configuration, and the successful Moon delivery is part of NASA’s CLPS (Commercial Lunar Payload Services) initiative and Artemis campaign. This is the first CLPS delivery for Firefly, and their first Moon landing.  

The 10 NASA science and technology instruments aboard the lander will operate on the lunar surface for approximately one lunar day, or about 14 Earth days.

“This incredible achievement demonstrates how NASA and American companies are leading the way in space exploration for the benefit of all,” said NASA acting Administrator Janet Petro. “We have already learned many lessons – and the technological and science demonstrations onboard Firefly’s Blue Ghost Mission 1 will improve our ability to not only discover more science, but to ensure the safety of our spacecraft instruments for future human exploration – both in the short term and long term.”

Since launching from NASA’s Kennedy Space Center in Florida on Jan. 15, Blue Ghost traveled more than 2.8 million miles, downlinked more than 27 GB of data, and supported several science operations. This included signal tracking from the Global Navigation Satellite System (GNSS) at a record-breaking distance of 246,000 miles with the Lunar GNSS Receiver Experiment payload – showing NASA can use the same positioning systems on Earth when at the Moon. Science conducted during the journey also included radiation tolerant computing through the Van Allen Belts with the Radiation-Tolerant Computer System payload and measurements of magnetic field changes in space with the Lunar Magnetotelluric Sounder payload.

“The science and technology we send to the Moon now helps prepare the way for future NASA exploration and long-term human presence to inspire the world for generations to come,” said Nicky Fox, associate administrator for science at NASA Headquarters in Washington. “We’re sending these payloads by working with American companies – which supports a growing lunar economy.”

During surface operations, the NASA instruments will test and demonstrate lunar subsurface drilling technology, regolith sample collection capabilities, global navigation satellite system abilities, radiation tolerant computing, and lunar dust mitigation methods. The data captured will benefit humanity by providing insights into how space weather and other cosmic forces impact Earth.  

Before payload operations conclude, teams will aim to capture imagery of the lunar sunset and how lunar dust reacts to solar influences during lunar dusk conditions, a phenomenon first documented by former NASA astronaut Eugene Cernan on Apollo 17. Following the lunar sunset, the lander will operate for several hours into the lunar night.

“On behalf of our entire team, I want to thank NASA for entrusting Firefly as their lunar delivery provider,” said Jason Kim, CEO of Firefly Aerospace. “Blue Ghost’s successful Moon landing has laid the groundwork for the future of commercial exploration across cislunar space. We’re now looking forward to more than 14 days of surface operations to unlock even more science data that will have a substantial impact on future missions to the Moon and Mars.”

To date, five vendors have been awarded 11 lunar deliveries under CLPS and are sending more than 50 instruments to various locations on the Moon, including the lunar South Pole. Existing CLPS contracts are indefinite-delivery, indefinite-quantity contracts with a cumulative maximum contract value of $2.6 billion through 2028. 

Learn more about NASA’s CLPS initiative at:

https://www.nasa.gov/clps

-end-

Amber Jacobson / Karen Fox 
Headquarters, Washington
202-358-1600
amber.c.jacobson@nasa.gov / karen.c.fox@nasa.gov 

Natalia Riusech / Nilufar Ramji
Johnson Space Center, Houston
281-483-5111
nataila.s.riusech@nasa.gov / nilufar.ramji@nasa.gov

Antonia Jaramillo
Kennedy Space Center, Florida
321-501-8425
antonia.jaramillobotero@nasa.gov

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Tiernan P. Doyle

Progress Cargo Craft Docks to Station Resupplying Crew

Progress Cargo Craft Docks to Station Resupplying Crew

March 1, 2025: International Space Station Configuration. Five spaceships are parked at the space station including the SpaceX Dragon crew spacecraft, the Northrop Grumman Cygnus resupply ship, the Soyuz MS-26 crew ship, and the Progress 90 and 91 resupply ships.
March 1, 2025: International Space Station Configuration. Five spaceships are parked at the space station including the SpaceX Dragon crew spacecraft, the Northrop Grumman Cygnus resupply ship, the Soyuz MS-26 crew ship, and the Progress 90 and 91 resupply ships.
NASA

The unpiloted Progress 91 spacecraft arrived at the aft port of the orbiting laboratory’s Zvezda Service module at 6:02 p.m. EST, March 1. The spacecraft launched at 4:24 p.m. EST (2:24 a.m. Baikonur time) Feb. 27, on a Soyuz rocket from the Baikonur Cosmodrome in Kazakhstan. 

The Roscosmos spacecraft is delivering about three tons of food, fuel, and supplies for the Expedition 72 crew aboard the International Space Station and will remain docked for approximately six months before departing for a re-entry into Earth’s atmosphere to dispose of trash loaded by the crew. 

.Learn more about station activities by following the space station blog, @space_station and @ISS_Research on X, as well as the ISS Facebook and ISS Instagram accounts.

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Mark A. Garcia

Smooshing for Science: A Flat-Out Success

Smooshing for Science: A Flat-Out Success

2 min read

Smooshing for Science: A Flat-Out Success

A color photograph from the Martian surface shows a close-up, overhead view of flat, cracked terrain colored pale orange-tan. At the center of the image a circular hole has been dug into the ground, shadowed and dark, and it’s surrounded by mounded grainy soil, colored a very light golden tan, that appears to have been dug out of the hole.
NASA’s Mars Perseverance rover acquired this image using its SHERLOC WATSON camera, located on the turret at the end of the rover’s robotic arm. The view is looking down at a flattened pile of tailings created by the coring of science target “Green Gardens,” so named because it contains serpentine, a mineral often green in color. The rover’s SHERLOC instrument (Scanning Habitable Environments with Raman & Luminescence for Organics & Chemicals) uses cameras, spectrometers, and a laser to search for organics and minerals that have been altered by watery environments and may be signs of past microbial life; in addition to its black-and-white context camera, SHERLOC is assisted by WATSON (Wide Angle Topographic Sensor for Operations and eNgineering), a color camera for taking close-up images of rock grains and surface textures. Perseverance acquired this image on Feb. 20, 2025 — sol 1424, or Martian day 1,424 of the Mars 2020 mission — at the local mean solar time of 13:11:41. This photo was selected by public vote and featured as “Image of the Week” for Week 210 (Feb. 16-22, 2025) of the Perseverance rover mission on Mars.
NASA/JPL-Caltech

Written by Henry Manelski, Ph.D. student at Purdue University

The Perseverance team is always looking for creative ways to use the tools we have on Mars to maximize the science we do. On the arm of the rover sits the SHERLOC instrument, which specializes in detecting organic compounds and is crucial in our search for signs of past microbial life. But finding these organics isn’t easy. The uppermost surface of most rocks Perseverance finds on Mars have been exposed to ultraviolet rays from the sun and the long-term oxidative potential of the atmosphere, both of which have the potential to break down organic compounds. For this reason, obtaining SHERLOC measurements from a “fresh” rock face is ideal. Last week the rover cored a serpentine-rich rock aptly named “Green Gardens,” resulting in a fresh pile of drill tailings. To get this material ready for the SHERLOC instrument, which requires a smooth area to obtain a measurement, the science team did something for the first time on Mars: We smooshed it!

Using the contact sensor of our sampling system, designed to indicate when our drill is touching a rock as it prepares to take a core, Perseverance pressed down into the tailings pile, compacting it into a flat, stable patch for SHERLOC to investigate. This unorthodox approach worked perfectly! The resulting SHERLOC spectral scan of these fresh tailings — which include serpentine, a mineral of key astrobiological interest — was a success. These flattened drill tailings are a great example of how a bit of out-of-the-box (or out-of-this-world!) thinking helps us maximize science on Mars. With this success behind us, the rover is rolling west toward the heart of “Witch Hazel Hill,” where more ancient rocks — and who knows what surprises — await!

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Last Updated
Feb 28, 2025

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