NASA’s Webb Observes Exoplanet Whose Composition Defies Explanation

NASA’s Webb Observes Exoplanet Whose Composition Defies Explanation

6 min read

NASA’s Webb Observes Exoplanet Whose Composition Defies Explanation

6 Min Read

NASA’s Webb Observes Exoplanet Whose Composition Defies Explanation

llustration labeled “artist’s concept” at right bottom corner. At left bottom corner, a partially illuminated, lemon-shaped exoplanet appears against a black background. This planet is most brightly illuminated at its elongated tip on its right side. On the left side, which is wider, the planet trails off into the darkness of the background. The planet is colored in varying, mottled shades of red, light pink, and fuchsia. Most of the pink occurs closest to the tip, while most of the fuchsia is at the top and bottom edges. At right top corner, a white beam emanates diagonally, oriented from 10 o’clock to 4 o’clock, from either side of a small, glowing, white star.
This artist’s concept shows what the exoplanet called PSR J2322-2650b (left) may look like as it orbits a rapidly spinning neutron star called a pulsar (right).
Credits:
Illustration: NASA, ESA, CSA, Ralf Crawford (STScI)

Scientists using NASA’s James Webb Space Telescope have observed a rare type of exoplanet, or planet outside our solar system, whose atmospheric composition challenges our understanding of how it formed. 

Officially named PSR J2322-2650b, this Jupiter-mass object appears to have an exotic helium-and-carbon-dominated atmosphere unlike any ever seen before. Soot clouds likely float through the air, and deep within the planet, these carbon clouds can condense and form diamonds. How the planet came to be is a mystery. The paper appears Tuesday in The Astrophysical Journal Letters. 

“This was an absolute surprise,” said study co-author Peter Gao of the Carnegie Earth and Planets Laboratory in Washington. “I remember after we got the data down, our collective reaction was ‘What the heck is this?’ It’s extremely different from what we expected.”

Image A: Exoplanet PSR J2322-2650b and Pulsar (Artist’s Concept)

llustration labeled u201cartistu2019s conceptu201d at right bottom corner. At left bottom corner, a partially illuminated, lemon-shaped exoplanet appears against a black background. This planet is most brightly illuminated at its elongated tip on its right side. On the left side, which is wider, the planet trails off into the darkness of the background. The planet is colored in varying, mottled shades of red, light pink, and fuchsia. Most of the pink occurs closest to the tip, while most of the fuchsia is at the top and bottom edges. At right top corner, a white beam emanates diagonally, oriented from 10 ou2019clock to 4 ou2019clock, from either side of a small, glowing, white star.
This artist’s concept shows what the exoplanet called PSR J2322-2650b (left) may look like as it orbits a rapidly spinning neutron star called a pulsar (right). Gravitational forces from the much heavier pulsar are pulling the Jupiter-mass world into a bizarre lemon shape.
Illustration: NASA, ESA, CSA, Ralf Crawford (STScI)

This planet-mass object was known to orbit a pulsar, a rapidly spinning neutron star. A pulsar emits beams of electromagnetic radiation at regular intervals typically ranging from milliseconds to seconds. These pulsing beams can only be seen when they are pointing directly toward Earth, much like beams from a lighthouse.  

This millisecond pulsar is expected to be emitting mostly gamma rays and other high energy particles, which are invisible to Webb’s infrared vision. Without a bright star in the way, scientists can study the planet in intricate detail across its whole orbit. 

“This system is unique because we are able to view the planet illuminated by its host star, but not see the host star at all,” said Maya Beleznay, a third-year PhD candidate at Stanford University in California who worked on modeling the shape of the planet and the geometry of its orbit. “So we get a really pristine spectrum. And we can study this system in more detail than normal exoplanets.” 

“The planet orbits a star that’s completely bizarre — the mass of the Sun, but the size of a city,” said the University of Chicago’s Michael Zhang, the principal investigator on this study. “This is a new type of planet atmosphere that nobody has ever seen before. Instead of finding the normal molecules we expect to see on an exoplanet — like water, methane, and carbon dioxide — we saw molecular carbon, specifically C3 and C2.”

Molecular carbon is very unusual because at these temperatures, if there are any other types of atoms in the atmosphere, carbon will bind to them. (Temperatures on the planet range from 1,200 degrees Fahrenheit at the coldest points of the night side to 3,700 degrees Fahrenheit at the hottest points of the day side.) Molecular carbon is only dominant if there’s almost no oxygen or nitrogen. Out of the approximately 150 planets that astronomers have studied inside and outside the solar system, no others have any detectable molecular carbon.

PSR J2322-2650b is extraordinarily close to its star, just 1 million miles away. In contrast, Earth’s distance from the Sun is about 100 million miles. Because of its extremely tight orbit, the exoplanet’s entire year — the time it takes to go around its star — is just 7.8 hours. Gravitational forces from the much heavier pulsar are pulling the Jupiter-mass planet into a bizarre lemon shape.

Image B: Exoplanet PSR J2322-2650b (Artist’s Concept)

Partially illuminated, lemon-shaped planet appears against a black background. The planet is most brightly illuminated at its elongated tip on its right side. On the left side, which is wider, the planet trails off into the darkness of the background. The planet is colored in varying, mottled shades of red, light pink, and fuchsia. Most of the pink occurs closest to the tip, while most of the fuchsia is at the top and bottom edges.
This artist’s concept shows what the exoplanet PSR J2322-2650b may look like. Gravitational forces from the much heavier pulsar it orbits are pulling the Jupiter-mass world into this bizarre lemon shape.
Illustration: NASA, ESA, CSA, Ralf Crawford (STScI)

Together, the star and exoplanet may be considered a “black widow” system, though not a typical example. Black widow systems are a rare type of double system where a rapidly spinning pulsar is paired with a small, low-mass stellar companion. In the past, material from the companion streamed onto the pulsar, causing the pulsar to spin faster over time, which powers a strong wind. That wind and radiation then bombard and evaporate the smaller and less massive companion. Like the spider for which it is named, the pulsar slowly consumes its unfortunate partner.

But in this case, the companion is officially considered an exoplanet, not a star. The International Astronomical Union defines an exoplanet as a celestial body below 13 Jupiter masses that orbits a star, brown dwarf, or stellar remnant, such as a pulsar.

Of the 6,000 known exoplanets, this is the only one reminiscent of a gas giant (with mass, radius, and temperature similar to a hot Jupiter) orbiting a pulsar. Only a handful of pulsars are known to have planets.

“Did this thing form like a normal planet? No, because the composition is entirely different,” said Zhang. “Did it form by stripping the outside of a star, like ‘normal’ black widow systems are formed? Probably not, because nuclear physics does not make pure carbon. It’s very hard to imagine how you get this extremely carbon-enriched composition. It seems to rule out every known formation mechanism.”

Study co-author Roger Romani, of Stanford University and the Kavli Institute for Particle Astrophysics and Cosmology Institute, proposes one evocative phenomenon that could occur in the unique atmosphere. “As the companion cools down, the mixture of carbon and oxygen in the interior starts to crystallize,” said Romani. “Pure carbon crystals float to the top and get mixed into the helium, and that’s what we see. But then something has to happen to keep the oxygen and nitrogen away. And that’s where the mystery come in.

“But it’s nice to not know everything,” said Romani. “I’m looking forward to learning more about the weirdness of this atmosphere. It’s great to have a puzzle to go after.”

Video A: Exoplanet PSR J2322-2650b and Pulsar (Artist’s Concept)

This animation shows an exotic exoplanet orbiting a distant pulsar, or rapidly rotating neutron star with radio pulses. The planet, which orbits about 1 million miles away from the pulsar, is stretched into a lemon shape by the pulsar’s strong gravitational tides. NASA&rsqu…

Animation: NASA, ESA, CSA, Ralf Crawford (STScI)

With its infrared vision and exquisite sensitivity, this is a discovery only the Webb telescope could make. Its perch a million miles from Earth and its huge sunshield keep the instruments very cold, which is necessary for these observations. It is not possible to conduct this study from the ground.

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).

To learn more about Webb, visit:

https://science.nasa.gov/webb

  

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Last Updated
Dec 15, 2025
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Laura Betz
NASA’s Goddard Space Flight Center
Greenbelt, Maryland
laura.e.betz@nasa.gov

Ann Jenkins
Space Telescope Science Institute
Baltimore, Maryland

Christine Pulliam
Space Telescope Science Institute
Baltimore, Maryland

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NASA ORBIT Challenge 2026

NASA ORBIT Challenge 2026

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The NASA ORBIT (Opportunities in Research, Business, Innovation, and Technology for the Workforce) Challenge is a multi-phase, student-focused challenge designed to inspire and empower the next generation of innovators, engineers, entrepreneurs, and researchers.

Compete for cash prizes, receive mentorship from NASA experts, and present your work at an in-person showcase. Finalists gain access to an exclusive accelerator program designed to launch careers in STEM and entrepreneurship.

Award: $380,000 in total prizes

Registration Open Date: December 15, 2025

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NASA’s Carruthers Geocorona Observatory Reveals ‘First Light’ Images

NASA’s Carruthers Geocorona Observatory Reveals ‘First Light’ Images

3 min read

NASA’s Carruthers Geocorona Observatory Reveals ‘First Light’ Images

NASA’s Carruthers Geocorona Observatory has captured its first images from space, revealing rare views of Earth and the Moon in ultraviolet light. Taken on Nov. 17 — still months before the mission’s science phase begins — these “first light” images confirm the spacecraft is healthy while hinting at the incredible views to come.

The initial images consist of two from Carruthers’ Wide Field Imager and two from its Narrow Field Imager. Each imager captured two different views: one showing a broad spectrum of far ultraviolet light, and one revealing light from Earth’s geocorona.

Comparison of wide field and narrow field images from NASA's Carruthers Geocorona Observatory: Each column shows far ultraviolet and Lyman-alpha views of Earth, with brightness color scales, using wide and narrow field imagers.
These four images constitute the “first light” for the Carruthers Geocorona Observatory mission. The images were taken on Nov. 17, 2025, from a location near the Sun-Earth Lagrange point 1 by the spacecraft’s Wide Field Imager (left column) and Narrow Field Imager (right column) in far ultraviolet light (top row) and the specific wavelength of light emitted by atomic hydrogen known as Lyman-alpha (bottom row). Earth is the larger, bright circle near the middle of each image; the Moon is the smaller circle below and to the left of it. The fuzzy “halo” around Earth in the images in the bottom row is the geocorona: the ultraviolet light emitted by Earth’s exosphere, or outermost atmospheric layer. The lunar surface still shines in Lyman-alpha because its rocky surface reflects all wavelengths of sunlight — one reason it is important to compare Lyman-alpha images with the broad ultraviolet filter. The far ultraviolet light imagery from the Narrow Field Imagery also captured two background stars, whose surface temperatures must be approximately twice as hot as the our Sun’s to be so bright in this wavelength of light.
NASA/Carruthers Geocorona Observatory

When Carruthers captured these images, the Moon was also in its field of view and slightly closer to the spacecraft than Earth was, making the Moon appear larger and closer to Earth than usual.

The specific wavelength Carruthers observed in two of the images, called Lyman-alpha, is light emitted by atomic hydrogen. The faint glow of Lyman-alpha from hydrogen in Earth’s outer atmosphere is called the “geocorona,” Latin for “Earth crown.”

In the broad-spectrum images, the Moon and Earth look similar: both are spheres with well-defined edges. However, in the Lyman-alpha filter, the Moon still appears as a crisp, sharp sphere while Earth appears surrounded by a bright “fuzz” extending out to space. This glow is the geocorona, the primary focus of the Carruthers mission. It is the only way to “see” Earth’s outermost atmospheric layer, although the light of the geocorona has only been photographed a handful of times in history. Carruthers will be the first mission to image it repeatedly, and from far enough away to see its great extent and discover how it changes over time.

These first images also offer a rare treat: sunlight reflected off the far side of the Moon, a view impossible to capture from Earth.




Original
Annotated

An interactive slider image allowing the user to swipe between two versions of an image, one with annotations and one without. The image shows a spacecraft’s view of Earth (at center) and the Moon (lower left) in ultraviolet light. The image includes a circular heatmap with a bright yellow center (Earth) fading to green and blue at the edges, showing Earth’s geocorona. A smaller bright spot appears near the bottom edge (the Moon). A vertical color bar labeled

An interactive slider image allowing the user to swipe between two versions of an image, one with annotations and one without. The image shows a spacecraft’s view of Earth (at center) and the Moon (lower left) in ultraviolet light. The image includes a circular heatmap with a bright yellow center (Earth) fading to green and blue at the edges, showing Earth’s geocorona. A smaller bright spot appears near the bottom edge (the Moon). A vertical color bar labeled

An interactive slider image allowing the user to swipe between two versions of an image, one with annotations and one without. The image shows a spacecraft’s view of Earth (at center) and the Moon (lower left) in ultraviolet light. The image includes a circular heatmap with a bright yellow center (Earth) fading to green and blue at the edges, showing Earth’s geocorona. A smaller bright spot appears near the bottom edge (the Moon). A vertical color bar labeled
An interactive slider image allowing the user to swipe between two versions of an image, one with annotations and one without. The image shows a spacecraft’s view of Earth (at center) and the Moon (lower left) in ultraviolet light. The image includes a circular heatmap with a bright yellow center (Earth) fading to green and blue at the edges, showing Earth’s geocorona. A smaller bright spot appears near the bottom edge (the Moon). A vertical color bar labeled

Original

Annotated

Carruthers Geocorona ObservatorY

A View of Earth’s Geocorona

Narrow Field Imager/Lyman-alpha filter


This view of the Earth, Moon, and Earth’s geocorona was captured by the Carruthers Geocorona Observatory’s Narrow Field Imager on Nov. 17, 2025. Move the slider to switch between the original version and one with overlaid annotations. In the annotated version, labels for Earth, the Moon, and Earth’s geocorona are overlaid on the image. The circle around Earth represents Earth’s surface, and the arc around Earth’s middle represents the orientation of Earth’s equator. The arrow pointing up and slightly to the left from Earth represents Earth’s rotational axis. The arrow pointing out to the right from Earth represents the direction to the Sun. The color scale indicates brightness, with brighter light appearing more yellow and dimmer light appearing more blue. The ‘glow’ that extends beyond Earth’s surface and out into space is Earth’s geocorona, which is emitted by hydrogen atoms in Earth’s exosphere in a wavelength of ultraviolet light known as Lyman-alpha.

These initial images were taken with short, five-minute exposures — just long enough to confirm that the instrument is performing well. During the main science phase, Carruthers will take 30-minute exposures, allowing it to reveal even fainter details of the geocorona and trace how Earth’s outer atmosphere responds to the changing Sun.

Carruthers launched on Sept. 24 and is just a few weeks from completing its journey to the Sun-Earth Lagrange point 1, a point of gravitational balance roughly 1 million miles closer to the Sun than Earth is. Carruthers will begin its primary science phase in March 2026, when it will begin sending back a steady stream of ultraviolet portraits of our planet’s ever-shifting outer atmosphere.

By Miles Hatfield
NASA’s Goddard Space Flight Center, Greenbelt, Md.

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Miles Hatfield

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NASA’s IMAP Mission Captures ‘First Light,’ Looks Back at Earth 

NASA’s IMAP Mission Captures ‘First Light,’ Looks Back at Earth 

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NASA’s IMAP Mission Captures ‘First Light,’ Looks Back at Earth 

All 10 instruments aboard NASA’s newly launched IMAP (Interstellar Mapping and Acceleration Probe) mission have successfully recorded their first measurements in space. With these “first light” observations, the spacecraft is now collecting preliminary science data as it journeys to its observational post at Lagrange point 1 (L1), about 1 million miles from Earth toward the Sun. 

“We are extremely pleased with the initial in-flight performance of the IMAP mission. All instruments have successfully powered on and our commissioning remains on track. We have already collected useful data including exercising our near-real-time space weather data stream,” said Brad Williams, IMAP program executive at NASA Headquarters in Washington. “This successful milestone is quickly setting the stage for the start of our primary science operations.”

As a modern-day celestial cartographer, IMAP will chart the boundaries of the heliosphere — a huge bubble created by the Sun’s wind that encapsulates our entire solar system — and study how the heliosphere interacts with the local galactic neighborhood beyond.

To map the heliosphere’s boundaries, IMAP is equipped with three instruments that measure energetic neutral atoms: IMAP-Lo, IMAP-Hi, and IMAP-Ultra. These uncharged particles, called ENAs for short, are cosmic messengers formed at the heliosphere’s edge that allow scientists to study the boundary region and its variability from afar. 

An animated GIF shows a large oval that is initially filled with large rectangular pixels of different colors from dark blue, light blue, green, yellow, orange, red, and pink. The pixels change color rapidly. The oval then goes from filled to only having two large vertical bands of colored pixels and then two thinner vertical bands of pixels, with the rest of the oval becoming gray, with no data. At the center of the oval a white dot is labeled
These partial maps of the heliosphere’s boundaries were compiled from first-light data from the IMAP-Hi, IMAP-Lo, and IMAP-Ultra instruments. These initial looks offer a first glimpse at the detail NASA’s IMAP (Interstellar Mapping and Acceleration Probe) will be able to capture. The warmer colors show regions with more energetic neutral atoms (ENAs).
NASA

“It’s just astounding that within the first couple weeks of observations, we see such clear and consistent ENA data across the factor of 10,000 in energy covered collectively by the three imagers,” said David McComas, Princeton University professor and principal investigator for the IMAP mission. “This, plus excellent first light data from all seven of the other instruments, makes for a 10 out of 10, A-plus start to the mission.”

As IMAP travelled away from Earth, the IMAP-Ultra instrument looked back at the planet and picked up ENAs created by Earth’s magnetic environment. These terrestrially made ENAs, which overwhelm ENAs coming from the heliosphere in sheer numbers, is a reason why IMAP will be stationed at L1. There the spacecraft will have an unobstructed view of ENAs coming from the heliosphere’s boundaries.

An elongated, horizontal colorized map shows rectangular pixels of different colors, mostly blue and green but dominated by a large circular feature in red, orange, and yellow on the far left. The background is mostly blue but two large swatches of green appear near the top center and bottom center.
Earth’s magnetic environment can be seen glowing bright in this image taken by the IMAP-Ultra instrument, which includes ENA data as well as noise. Earth sits at the center of the red donut-shaped structure. This image was taken as IMAP left Earth for its post at Lagrange point 1.
NASA

The mission will also study the solar wind, a continuous flow of charged particles coming from the Sun. Solar wind observations from five of IMAP’s instruments will be used by the IMAP Active Link for Real-Time (I-ALiRT) system to provide roughly a half hour’s warning to voyaging astronauts and spacecraft near Earth about harmful space weather and radiation coming their way. The IMAP instruments are already making near-real-time solar wind measurements that can be used to support space weather forecasts. The I-ALiRT network is being exercised and will be ready for space weather forecasters when IMAP starts its regular science mission at L1.

With all of IMAP’s instruments up and running, the mission has nearly completed its commissioning stage and will arrive at L1 in early January. The mission is now working to complete the final commissioning steps and instrument calibration with the goal of being ready to take operational science data starting Saturday, Feb. 1, 2026. 

Here’s a look at IMAP’s instruments and what they’ve seen in their first-light observations.

By Mara Johnson-Groh
NASA’s Goddard Space Flight Center, Greenbelt, Md.

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NASA, Partners Share First Data From New US-European Sea Satellite

NASA, Partners Share First Data From New US-European Sea Satellite

5 min read

Preparations for Next Moonwalk Simulations Underway (and Underwater)

A map showing a portion of the North Atlantic Ocean, with the U.S. Eastern seaboard along the left side of the frame, is covered with wide yellow lines criss-crossing in X shapes. Written on the lines in black ink is either “S6MF” for Sentinel-6 Michael Freilich or “S6B” for Sentinel-6B, showing the orbital paths of each satellite. On the left side of the image, a legend labeled “sea level anomaly (cm)” shows a vertical, rainbow-hued graph ranging from dark blue at the bottom to dark red at the top; the colors correspond to blobs of each shade that cover the ocean on the map.
Sentinel-6B and Sentinel-6 Michael Freilich captured data on Nov. 26 of sea levels across a vast stretch of the Atlantic. Within the crisscrossing bands, red indicates higher water relative to the long-term average; blue indicates lower water. The tracks are layered atop the combined observations of other sea-level satellites.
EUMETSAT

Launched in November, Sentinel-6B will track ocean height with ultraprecision to advance marine forecasting, national security, and more.

Sentinel-6B, a joint mission by NASA and its U.S. and European partners to survey 90% of the world’s oceans for the benefit of communities and commerce, has started sending back its first measurements since launching in November. A newly published map of the data shows sea levels across a vast stretch of the Eastern Seaboard and Atlantic Ocean. 

About the size of a pickup truck, Sentinel-6B extends a decades-long effort led by the United States and Europe to track ocean height down to fractions of an inch using radar altimetry. Once its instruments and algorithms are fully calibrated next year, Sentinel-6B will return actionable data for ship crews, weather forecasters, national security, and the millions of people who live and work near coastlines.  

“NASA does incredible science using the unique vantage point of space every day to deliver life-saving data directly into the hands of decision-makers for storms, navigation, flooding, and more,” said Nicky Fox, associate administrator, Science Mission Directorate, NASA Headquarters in Washington. “The ocean measurements that Sentinel-6B collected during its first months in orbit benefit all, providing key insights to ensure the prosperity and security of coastal communities around the globe.” 

In addition to measuring sea level, instruments aboard the satellite will gather information on wind speeds, wave heights, atmospheric temperature, and humidity. In turn, that data can be used by U.S. agencies as well as to refine the Goddard Earth Observing System atmospheric forecast models, which the NASA Engineering and Safety Center relies on to plan safer re-entry of astronauts returning from Artemis missions.  

Mission teams in recent weeks have verified that Sentinel-6B and all its instruments are in good health. That includes the Poseidon-4 Synthetic Aperture Radar altimeter, the Advanced Microwave Radiometer for Climate, the Global Navigation Satellite System – Radio Occultation, and the Precise Orbit Determination Package. 

In the visualization above, featuring data captured by Sentinel-6B on Nov. 26, the crisscrossing bands trace the satellite’s path as it orbits Earth. The image also shows data collected on the same day by the satellite’s twin, Sentinel-6 Michael Freilich, which launched in 2020. The data in those bands is layered over the combined observations of other sea-level satellites across the region shown. Red indicates higher water relative to the long-term average; blue areas indicate lower water. Because the spacecraft’s instruments have not been fully calibrated, the data is considered preliminary but also quite promising. 

Together, Sentinel-6B and Sentinel-6 Michael Freilich make up the Copernicus Sentinel-6/Jason-CS (Continuity of Service) mission developed by NASA, ESA (European Space Agency), EUMETSAT (European Organisation for the Exploitation of Meteorological Satellites), and the National Oceanic and Atmospheric Administration (NOAA). 

“These first light images from Sentinel-6B underscore the value of Earth science observations in providing life-saving and economic-empowering data to communities along our world’s coastlines, where a third of the globe’s population lives,” said Karen St. Germain, director, NASA Earth Science Division at the agency’s headquarters. “This achievement also highlights the power of partnerships with ESA, EUMETSAT, and our sister science agency NOAA in advancing our collective understanding of Earth systems and putting that Earth science understanding to work for the benefit of humanity.” 

Sentinel-6/Jason-CS adds to a continuous sea level rise dataset that began in the early 1990s. Since then, the rate of sea level rise globally has doubled and currently averages about 0.17 inches (4.3 millimeters) per year. The rate differs between locations, with implications for coastal infrastructure, trade routes, and storm formation. 

“The accuracy and precision of this mission’s gold-standard dataset speaks to the foresight, more than 30 years ago, of investing in the technology and expertise that make it possible,” said Dave Gallagher, director, NASA’s Jet Propulsion Laboratory in Southern California. “We’re proud to continue partnering to collect these critical measurements into another decade, and even prouder of the teams behind this most recent milestone.” 

Flying 830 miles (1,336 kilometers) above Earth, Sentinel-6B is about 30 seconds behind its twin, Sentinel-6 Michael Freilich, currently the official reference satellite for sea level. Eventually, Sentinel-6B will take over that role, and Sentinel-6 Michael Freilich will move into a different orbit.

More about Sentinel-6B 

Copernicus Sentinel-6/Jason-CS was jointly developed by ESA, EUMETSAT, NASA, and NOAA, with funding support from the European Commission and technical support from CNES. The mission, starting with Sentinel-6 Michael Freilich, marked the first international involvement in Copernicus, the European Union’s Earth Observation Programme. 

Managed for NASA by Caltech in Pasadena, JPL contributed three science instruments for each Sentinel-6 satellite: the Advanced Microwave Radiometer, the Global Navigation Satellite System – Radio Occultation, and the laser retroreflector array. NASA also contributed launch services, ground systems supporting operation of the NASA science instruments, the science data processors for two of these instruments, and support for the international ocean surface topography community. 

For more about Sentinel-6B, visit: 

https://science.nasa.gov/mission/sentinel-6B/

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