Wednesday, April 16, 2025

 SPACE/COSMOS

Crystal clues on Mars point to watery and possibly life-supporting past



Queensland University of Technology

QUT research team 

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A new QUT-led study using data collected by NASA’s Perseverance Rover mission has revealed compelling evidence that could help scientists answer whether life ever existed on Mars. l/r- Dr Michael Jones, Associate Professor Christoph Schrank, Mr Peter Nemere and Mr Brendan Orenstein.

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Credit: Use with credit QUT




A QUT-led study analysing data from NASA’s Perseverance rover has uncovered compelling evidence of multiple mineral-forming events just beneath the Martian surface – findings that bring scientists one step closer to answering the profound question: did life ever exist on Mars?

The QUT research team led by Dr Michael Jones, from the Central Analytical Research Facility and the School of Chemistry and Physics, includes Associate Professor David FlanneryAssociate Professor Christoph Schrank, Brendan Orenstein and Peter Nemere, together with researchers from North America and Europe.

The findings were published in the prestigious journal Science Advances.

“Sulphate minerals exist with different amounts of water in most regions on Mars and allow us to understand how water moved around the planet, which is key to understanding its past habitability,” Dr Jones said.

“However, we don’t yet fully understand how or when these minerals formed. Our team found a way to measure the internal crystal structure of these minerals directly in the rock, which had thought to be impossible on the surface of Mars.”

The team adapted a new analytical method called X-ray Backscatter Diffraction Mapping (XBDM) developed by Dr Jones and Professor Schrank at the Australian Synchrotron to Perseverance’s onboard PIXL instrument developed by QUT alumna Abigail Allwood.

This allowed the team to determine the orientation of the crystal structures, essentially providing a fingerprint of how and when they grew, and what the environment on Mars was like at that time.

Two separate generations of calcium-sulphate minerals were uncovered at Hogwallow Flats and Yori Pass in the Shenandoah formation, part of the sedimentary fan in Jezero crater: one formed just beneath the surface and the other formed deeper underground, at least 80 meters down.

“This discovery highlights the diversity of environments that existed in the Shenandoah formation’s history — indicating multiple potential windows when life might have been possible on Mars,” Dr Jones said.

Since its landing in Jezero Crater in February 2021, the Perseverance rover has been exploring a wide variety of Martian rock types, from ancient lava flows to sedimentary layers left behind by a long-vanished lake and river delta.

One of its key mission goals is to study environments that could have supported microbial life – and collect samples that might someday be returned to Earth.

The QUT research team is part of the multidisciplinary QUT Planetary Surface Exploration Research Group which focuses on interplanetary science and is actively involved in projects within NASA and the Australian Space Agency.

Professor Flannery, long-term planner for the NASA Perseverance mission, said QUT is at the forefront of planetary science in Australia.

“Experience gained by QUT researchers exposed to the cutting edge of the robotics, automation, data science and astrobiology fields has the potential to kick start Australia’s space industry,” he said.

Read the full paper, In-situ crystallographic mapping constrains sulphate precipitation and timing in Jezero crater, Mars, published in Science Advances online.

Strongest hints yet of biological activity outside the solar system




University of Cambridge

Artist's impression of the exoplanet K2-18b 

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Astronomers have detected the most promising signs yet of a possible biosignature outside the solar system, although they remain cautious.

Using data from the James Webb Space Telescope (JWST), the astronomers, led by the University of Cambridge, have detected the chemical fingerprints of dimethyl sulfide (DMS) and/or dimethyl disulfide (DMDS), in the atmosphere of the exoplanet K2-18b, which orbits its star in the habitable zone.

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Credit: A. Smith, N. Madhusudhan (University of Cambridge)




Astronomers have detected the most promising signs yet of a possible biosignature outside the solar system, although they remain cautious.

Using data from the James Webb Space Telescope (JWST), the astronomers, led by the University of Cambridge, have detected the chemical fingerprints of dimethyl sulfide (DMS) and/or dimethyl disulfide (DMDS), in the atmosphere of the exoplanet K2-18b, which orbits its star in the habitable zone.

On Earth, DMS and DMDS are only produced by life, primarily microbial life such as marine phytoplankton. While an unknown chemical process may be the source of these molecules in K2-18b’s atmosphere, the results are the strongest evidence yet that life may exist on a planet outside our solar system.

The observations have reached the ‘three-sigma’ level of statistical significance – meaning there is a 0.3% probability that they occurred by chance. To reach the accepted classification for scientific discovery, the observations would have to cross the five-sigma threshold, meaning there would be below a 0.00006% probability they occurred by chance.

The researchers say between 16 and 24 hours of follow-up observation time with JWST may help them reach the all-important five-sigma significance. Their results are reported in The Astrophysical Journal Letters.

Earlier observations of K2-18b — which is 8.6 times as massive and 2.6 times as large as Earth, and lies 124 light years away in the constellation of Leo — identified methane and carbon dioxide in its atmosphere. This was the first time that carbon-based molecules were discovered in the atmosphere of an exoplanet in the habitable zone. Those results were consistent with predictions for a ‘Hycean’ planet: a habitable ocean-covered world underneath a hydrogen-rich atmosphere.

However, another, weaker signal hinted at the possibility of something else happening on K2-18b. “We didn’t know for sure whether the signal we saw last time was due to DMS, but just the hint of it was exciting enough for us to have another look with JWST using a different instrument,” said Professor Nikku Madhusudhan from Cambridge’s Institute of Astronomy, who led the research.

To determine the chemical composition of the atmospheres of faraway planets, astronomers analyse the light from its parent star as the planet transits, or passes in front of the star as seen from the Earth. As K2-18b transits, JWST can detect a drop in stellar brightness, and a tiny fraction of starlight passes through the planet’s atmosphere before reaching Earth. The absorption of some of the starlight in the planet’s atmosphere leaves imprints in the stellar spectrum that astronomers can piece together to determine the constituent gases of the exoplanet’s atmosphere.

The earlier, tentative, inference of DMS was made using JWST’s NIRISS (Near-Infrared Imager and Slitless Spectrograph) and NIRSpec (Near-Infrared Spectrograph) instruments, which together cover the near-infrared (0.8-5 micron) range of wavelengths. The new, independent observation used JWST’s MIRI (Mid-Infrared Instrument) in the mid-infrared (6-12 micron) range.

“This is an independent line of evidence, using a different instrument than we did before and a different wavelength range of light, where there is no overlap with the previous observations,” said Madhusudhan. “The signal came through strong and clear.”

“It was an incredible realisation seeing the results emerge and remain consistent throughout the extensive independent analyses and robustness tests,” said co-author MÃ¥ns Holmberg, a researcher at the Space Telescope Science Institute in Baltimore, USA. 

DMS and DMDS are molecules from the same chemical family, and both are predicted to be biosignatures. Both molecules have overlapping spectral features in the observed wavelength range, although further observations will help differentiate between the two molecules.

However, the concentrations of DMS and DMDS in K2-18b’s atmosphere are very different than on Earth, where they are generally below one part per billion by volume. On K2-18b, they are estimated to be thousands of times stronger - over ten parts per million.

“Earlier theoretical work had predicted that high levels of sulfur-based gases like DMS and DMDS are possible on Hycean worlds,” said Madhusudhan. “And now we’ve observed it, in line with what was predicted. Given everything we know about this planet, a Hycean world with an ocean that is teeming with life is the scenario that best fits the data we have.”

Madhusudhan says that while the results are exciting, it’s vital to obtain more data before claiming that life has been found on another world. He says that while he is cautiously optimistic, there could be previously unknown chemical processes at work on K2-18b that may account for the observations. Working with colleagues, he is hoping to conduct further theoretical and experimental work to determine whether DMS and DMDS can be produced non-biologically at the level currently inferred.

“The inference of these biosignature molecules poses profound questions concerning the processes that might be producing them” said co-author Subhajit Sarkar of Cardiff University.

“Our work is the starting point for all the investigations that are now needed to confirm and understand the implications of these exciting findings,” said co-author Savvas Constantinou, also from Cambridge’s Institute of Astronomy.

“It’s important that we’re deeply sceptical of our own results, because it’s only by testing and testing again that we will be able to reach the point where we’re confident in them,” Madhusudhan said. “That’s how science has to work.”

While he is not yet claiming a definitive discovery, Madhusudhan says that with powerful tools like JWST and future planned telescopes, humanity is taking new steps toward answering that most essential of questions: are we alone?

“Decades from now, we may look back at this point in time and recognise it was when the living universe came within reach,” said Madhusudhan. “This could be the tipping point, where suddenly the fundamental question of whether we’re alone in the universe is one we’re capable of answering.”

The James Webb Space Telescope is a collaboration between NASA, ESA and the Canadian Space Agency (CSA). The research is supported by a UK Research and Innovation (UKRI) Frontier Research Grant.

To learn more about Hycean worlds, visit hycean.group.cam.ac.uk


Transmission spectrum of the exoplanet K2-18b

 

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Astronomers find rare twist in exoplanet’s twin star orbit

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DOI

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"Big surprise": astronomers find planet in perpendicular orbit around pair of stars

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DOI

Cosmic twist: New study suggests the universe could be spinning




University of Hawaii at Manoa

Whirlpool Galaxy 

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The Whirlpool Galaxy, M51, is a spiral galaxy located 31 million light-years away. (Image credit: NASA)

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Credit: NASA




A new study in Monthly Notices of the Royal Astronomical Society by researchers including István Szapudi of the University of HawaiÊ»i Institute for Astronomy suggests the universe may rotate—just extremely slowly. The finding could help solve one of astronomy’s biggest puzzles.

“To paraphrase the Greek philosopher Heraclitus of Ephesus, who famously said “Panta Rhei”—everything moves, we thought that perhaps Panta Kykloutai—everything turns,” said Szapudi.

Current models say the universe expands evenly in all directions, with no sign of rotation. This idea fits most of what astronomers observe. But it doesn’t explain the so-called “Hubble tension”—a long-standing disagreement between two ways of measuring how fast the universe is expanding.

Supernovae, Big Bang

One method looks at distant exploding stars or supernovae, to measure the  distances to galaxies, and gives an expansion rate for the universe throughout the past few billion years. The other method uses the relic radiation from the Big Bang and gives the expansion rate of the very early Universe, about 13 billion years ago. Each gives a different value for the expansion rate.

Szapudi’s team developed a mathematical model of the universe. First, it followed standard rules. Then they added a tiny amount of rotation. That small change made a big difference.

“Much to our surprise, we found that our model with rotation resolves the paradox without contradicting current astronomical measurements. Even better, it is compatible with other models that assume rotation. Therefore, perhaps, everything really does turn. Or, Panta Kykloutai! ” noted Szapudi.

Their model suggests the universe could rotate once every 500 billion years—too slow to detect easily, but enough to affect how space expands over time.

The idea doesn’t break any known laws of physics. And it might explain why measurements of the universe’s growth don’t quite agree.

The next step is turning the theory into a full computer model—and finding ways to spot signs of this slow cosmic spin.

The most distant twin of the Milky Way ever observed



An international team led by UNIGE has discovered a massive, Milky Way-like spiral galaxy that formed just 1 billion years after the Big Bang, revealing an unexpectedly mature structure 


Peer-Reviewed Publication

Université de Genève

The most distant cousin of Milky Way ever observed 

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The image of Zhúlóng shows its spiral arms, an old central bulge and a large star-forming disc, which resembles the Milky Way.

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Credit: © NASA/CSA/ESA, M. Xiao (University of Geneva), G. Brammer (Niels Bohr Institute), Dawn JWST Archive






An international team led by the University of Geneva (UNIGE) has discovered the most distant spiral galaxy candidate known to date. This ultra-massive system existed just one billion years after the Big Bang and already shows a remarkably mature structure, with a central old bulge, a large star-forming disk, and well-defined spiral arms. The discovery was made using data from the James Webb Space Telescope (JWST) and offers important insights into how galaxies can form and evolve so rapidly in the early Universe. The study is published in Astronomy & Astrophysics.


Large spiral galaxies like the Milky Way are expected to take several billion years to form. During the first billion years of cosmic history, galaxies are thought to be small, chaotic, and irregular in shape. However, the JWST is beginning to reveal a very different picture. Its deep infrared imaging is uncovering surprisingly massive and well-structured galaxies at much earlier times than previously expected – prompting astronomers to reassess how and when galaxies take shape in the early Universe.


A Milky Way Twin in the Early Universe

Among these new findings is Zhúlóng, the most distant spiral galaxy candidate identified to date, seen at a redshift of 5.2 – just 1 billion years after the Big Bang. Despite this early epoch, the galaxy exhibits a surprisingly mature structure: a central old bulge, a large star-forming disk, and spiral arms – features typically seen in nearby galaxies.


‘‘We named this galaxy Zhúlóng, meaning ‘Torch Dragon’ in Chinese mythology. In the myth, Zhúlóng is a powerful red solar dragon that creates day and night by opening and closing its eyes, symbolizing light and cosmic time,’’ says Dr. Mengyuan Xiao, postdoctoral researcher at the Department of Astronomy of the Faculty of Science of UNIGE and lead author of the study.


“What makes Zhúlóng stand out is just how much it resembles the Milky Way – both in shape, size, and stellar mass,” she adds.  Its disk spans over 60,000 light-years, comparable to our own galaxy, and contains more than 100 billion solar masses in stars. This makes it one of the most compelling Milky Way analogues ever found at such an early time, raising new questions about how massive, well-ordered spiral galaxies could form so soon after the Big Bang.


A serendipitous discovery 

Zhúlóng was discovered in deep imaging from JWST’s PANORAMIC survey (GO-2514), a wide-area extragalactic program led by Christina Williams (NOIRLab) and Pascal Oesch (UNIGE). PANORAMIC exploits JWST’s unique “pure parallel” mode – an efficient strategy to collect high-quality images while JWST’s main instrument is taking data on another target. “This allows JWST to map large areas of the sky, which is essential for discovering massive galaxies, as they are incredibly rare,” says Dr. Christina Williams, assistant astronomer at NOIRLab and principal investigator of the PANORAMIC program. “This discovery highlights the potential of pure parallel programs for uncovering rare, distant objects that stress-test galaxy formation models.”


Rewriting the Story 

Spiral structures were previously thought to take billions of years to develop, and massive galaxies were not expected to exist until much later in the universe, because they typically form after smaller galaxies merged together over time.  “This discovery shows how JWST is fundamentally changing our view of the early Universe,” says Prof. Pascal Oesch, associate professor in the Department of Astronomy at the Faculty of Science of UNIGE and co-principal investigator of the PANORAMIC program.


Future JWST and Atacama Large Millimeter Array (ALMA) observations will help confirm its properties and reveal more about its formation history. As new wide-area JWST surveys continue, astronomers expect to find more such galaxies – offering fresh insights into the complex processes shaping galaxies in the early Universe.

On Jupiter, it's mushballs all the way down


Strange as it may seem, slushy hailstones of ammonia and water may form on all gas giant planets




University of California - Berkeley

3D view of an area of Jupiter's upper atmosphere 

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A cross section of the upper atmosphere, or troposphere, of Jupiter, showing the depth of storms in a north-south swath that crosses the planet's equator, or equatorial zone (EZ). Blue and red represent, respectively, higher- and lower-than-normal abundances of ammonia gas. By tracking the ammonia, two new UC Berkeley studies show that the rapidly changing weather systems on Jupiter are mostly very shallow (left), though two types of storms — rapidly rising plumes of ammonia (center) and tornado-like vortices — punch more deeply and are responsible for unmixing atmospheric gases. Large-scale storms produce mushballs that rain downward even deeper than the plumes and vortices.

 

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Credit: Chris Moeckel, UC Berkeley






Imagine a Slushee™ composed of ammonia and water encased in a hard shell of water ice. Now picture these ice-encrusted slushballs, dubbed "mushballs," raining down like hailstones during a thunderstorm, illuminated by intense flashes of lightning.

Planetary scientists at the University of California, Berkeley, now say that hailstorms of mushballs accompanied by fierce lightning actually exist on Jupiter. In fact, mushball hailstorms may occur on all gaseous planets in the galaxy, including our solar system's other giant planets, Saturn, Uranus and Neptune.

The idea of mushballs was initially put forth in 2020 to explain nonuniformities in the distribution of ammonia gas in Jupiter's upper atmosphere that were detected both by NASA's Juno mission and by radio telescopes on Earth.

At the time, UC Berkeley graduate student Chris Moeckel and his adviser, Imke de Pater, professor emerita of astronomy and of earth and planetary science, thought the theory too elaborate to be real, requiring highly specific atmospheric conditions.

"Imke and I both were like, ‘There's no way in the world this is true,’" said Moeckel, who received his UC Berkeley Ph.D. last year and is now a researcher at UC Berkeley's Space Sciences Laboratory. "So many things have to come together to actually explain this, it seems so exotic. I basically spent three years trying to prove this wrong. And I couldn't prove it wrong."

The confirmation, reported March 28 in the journal Science Advances, emerged together with the first 3D visualization of Jupiter's upper atmosphere, which Moeckel and de Pater recently created and describe in a paper that is now undergoing peer review and is posted on the preprint server arXiv.

The 3D picture of Jupiter's troposphere shows that the majority of the weather systems on Jupiter are shallow, reaching only 10 to 20 kilometers below the visible cloud deck or “surface” of the planet, which has a radius of 70,000 km. Most of the colorful, swirling patterns in the bands that encircle the planet are shallow.

Some weather, however, emerges much deeper in the troposphere, redistributing ammonia and water and essentially unmixing what was long thought to be a uniform atmosphere. The three types of weather events responsible are hurricane-like vortices, hotspots coupled to ammonia-rich plumes that wrap around the planet in a wave-like structure, and large storms that generate mushballs and lightning.

"Every time you look at Jupiter, it's mostly just surface level," Moeckel said. "It's shallow, but a few things — vortices and these big storms — can punch through."

"Juno really shows that ammonia is depleted at all latitudes down to about 150 kilometers, which is really odd," said de Pater, who discovered 10 years ago that ammonia was depleted down to about 50 km. "That's what Chris is trying to explain with his storm systems going much deeper than we expected."

Inferring planet composition from observations of clouds

Gas giants like Jupiter and Saturn and ice giants like Neptune and Uranus are a major focus of current space missions and large telescopes, including the James Webb Space Telescope, in part because they can help us understand the formation history of our solar system and ground truth observations of distant exoplanets, many of which are large and gaseous. Since astronomers can see only the upper atmospheres of faraway exoplanets, knowing how to interpret chemical signatures in these observations can help scientists infer details of exoplanet interiors, even for Earth-like planets.

"We're basically showing that the top of the atmosphere is actually a pretty bad representative of what is inside the planet," Moeckel said.

That's because storms like those that create mushballs unmix the atmosphere so that the chemical composition of the cloud tops does not necessarily reflect the composition deeper in the atmosphere. Jupiter is unlikely to be unique.

"You can just extend that to Uranus, Neptune — certainly to exoplanets as well," de Pater said.

The atmosphere on Jupiter is radically different from that on Earth. It's primarily made of hydrogen and helium gas with trace amounts of gaseous molecules, like ammonia and water, which are heavier than the bulk atmosphere. Earth's atmosphere is mainly nitrogen and oxygen. Jupiter also has storms, like the Great Red Spot, that last for centuries. And while ammonia gas and water vapor rise, freeze into droplets, like snow, and rain down continually, there is no solid surface to hit. At what point do the raindrops stop falling?

"On Earth, you have a surface, and rain will eventually hit this surface," Moeckel said. "The question is: What happens if you take the surface away? How far do the raindrops fall into the planet? This is what we have on the giant planets."

That question has piqued the interest of planetary scientists for decades, because processes like rain and storms are thought to be the main vertical mixers of planetary atmospheres. For decades, the simple assumption of a well-mixed atmosphere guided inferences about the interior makeup of gas giant planets like Jupiter.

Observations by radio telescopes, much of it conducted by de Pater and colleagues, show that this simple assumption is false.

"The turbulent cloud tops would lead you to believe that the atmosphere is well mixed," said Moeckel, invoking the analogy of a boiling pot of water. "If you look at the top, you see it boiling, and you would assume that the whole pot is boiling. But these findings show that even though the top looks like it’s boiling, below is a layer that really is very steady and sluggish."

The microphysics of mushballs

On Jupiter, the majority of water rain and ammonia snow appears to cycle high up in the cold atmosphere and evaporate as it falls, Moeckel said. Yet, even before Juno's arrival at Jupiter, de Pater and her colleagues reported an upper atmosphere lacking in ammonia. They were able to explain these observations, however, through dynamic and standard weather modeling, which predicted a rainout of ammonia in thunderstorms down to the water layer, where water vapor condenses into a liquid.

But radio observations by Juno traced the regions of poor mixing to much greater depths, down to about 150 km, with many areas puzzlingly depleted of ammonia and no known mechanism that could explain the observations. This led to proposals that water and ammonia ice must form hailstones that fall out of the atmosphere and remove the ammonia. But it was a mystery how hailstones could form that were heavy enough to fall hundreds of kilometers into the atmosphere.

To explain why ammonia is missing from parts of Jupiter’s atmosphere, planetary scientist Tristan Guillot proposed a theory involving violent storms and slushy hailstones called mushballs. In this idea, strong updrafts during storms can lift tiny ice particles high above the clouds — more than 60 kilometers up. At those altitudes, the ice mixes with ammonia vapor, which acts like antifreeze and melts the ice into a slushy liquid. As the particles continue to rise and fall, they grow larger — like hailstones on Earth — eventually becoming mushballs the size of softballs.

These mushballs can trap large amounts of water and ammonia with a 3 to 1 ratio. Because of their size and weight, they fall deep into the atmosphere — well below where the storm started — carrying the ammonia with them. This helps explain why ammonia appears to be missing from the upper atmosphere: it’s being dragged down and hidden deep inside the planet, where it leaves faint signatures to be observed with radio telescopes.

However, the process depends on a number of specific conditions. The storms need to have very strong updrafts, around 100 meters per second, and the slushy particles must quickly mix with ammonia and grow large enough to survive the fall.

"The mushball journey essentially starts about 50 to 60 kilometers below the cloud deck as water droplets. The water droplets get rapidly lofted all the way to the top of the cloud deck, where they freeze out and then fall over a hundred kilometers into the planet, where they start to evaporate and deposit material down there," Moeckel said. "And so you have, essentially, this weird system that gets triggered far below the cloud deck, goes all the way to the top of the atmosphere and then sinks deep into the planet."

Unique signatures in the Juno radio data for one storm cloud convinced him and his colleagues that this is, indeed, what happens.

"There was a small spot under the cloud that either looked like cooling, that is, melting ice, or an ammonia enhancement, that is, melting and release of ammonia," Moeckel said. "It was the fact that either explanation was only possible with mushballs that eventually convinced me."

The radio signature could not have been caused by water raindrops or ammonia snow, according to paper co-author Huazhi Ge, an expert in cloud dynamics on giant planets and a postdoctoral fellow at the California Institute of Technology in Pasadena.

"The Science Advances paper shows, observationally, that this process apparently is true, against my best desire to find a simpler answer," Moeckel said.

Coordinated observations of Jupiter

Scientists around the world observe Jupiter regularly with ground-based telescopes, timed to coincide with Juno's closest approach to the planet every six weeks. In February 2017 and April 2019 — the periods covered by the two papers — the researchers used data from both the Hubble Space Telescope (HST) and the Very Large Array (VLA) in New Mexico to complement Juno observations in an attempt to create a 3D picture of the troposphere. The HST, at visible wavelengths, provided measurements of reflected light off the cloud tops, while the VLA, a radio telescope, probed tens of kilometers below the clouds to provide global context. Juno's Microwave Radiometer explored the deep atmosphere of Jupiter over a limited region of the atmosphere.

"I essentially developed a tomography method that takes the radio observations and turns them into a three-dimensional rendering of that part of the atmosphere that is seen by Juno," Moeckel said.

The 3D picture of that one swath of Jupiter confirmed that most of the weather is happening in the upper 10 kilometers.

"The water condensation layer plays a crucial role in controlling the dynamics and the weather on Jupiter," Moeckel said. “Only the most powerful storms and waves can break through that layer.

Moeckel noted that his analysis of Jupiter’s atmosphere was delayed by the lack of publicly available calibrated data products from the Juno mission. Given the current level of data released, he was forced to independently reconstruct the mission team’s data processing methods — tools, data and discussions that, if shared earlier, could have significantly accelerated independent research and broadened scientific participation. He has since made these resources publicly available to support future research efforts.

The work was funded in part by a Solar System Observations (SSO) award from NASA (80NSSC18K1003).


An illustration depicting how violent storms on Jupiter — and likely other gas giants — generate mushballs and shallow lightning. The mushballs are created by thunderstorm clouds that form about 40 miles beneath the cloud tops and fuel a strong updraft that carries water ice upward to extreme altitudes, occasionally above the visible cloud layer. Once they reach altitudes of about 14 miles below the visible cloud layer, ammonia acts like an antifreeze, melting the ice and combining with it to form a slushy ammonia-water liquid that gets coated with water ice — a mushball. The mushballs keep rising until they become too heavy and fall back through the atmosphere, growing until they reach the water condensation layer, where they evaporate. This ends up redistributing ammonia and water from the upper atmosphere (green and blue layer) to layers deep below the clouds, creating areas of depleted ammonia visible in radio observations.

Credit

NASA/JPL-Caltech/SwRI/CNRS

 

Binghamton University, State University of New York to establish Institute for AI and Society



New initiative taps into the power of Empire AI, a consortium of public and private universities in New York



Binghamton University

Associate Professor Jeremy Blackburn 

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Associate Professor Jeremy Blackburn, director of Binghamton University’s Institute for AI and Society.

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Credit: Binghamton University, State University of New York




BINGHAMTON, N.Y. -- Thanks to funding from New York state, Binghamton University, State University of New York will establish an Institute for AI and Society that taps into the power of Empire AI, the most powerful academic research computer in the country.

Gov. Kathy Hochul has announced a new program providing $5 million to eight SUNY campuses, including Binghamton, to engage diverse disciplines and communities, broaden AI development to prepare students for the future, and advance the use of AI for the public good.

“The progression of AI research in New York state is going to inspire other states to follow our path,” Hochul said. “Investing in AI within the SUNY system is an investment in our students to expand their knowledge about what the future will bring. We are not just preparing students for AI – we’re shaping how AI serves society, ensuring it strengthens communities and our economy.”

Other SUNY schools receiving funding are University at Albany, University at Buffalo, SUNY Downstate, SUNY ESF, SUNY Polytechnic Institute, Stony Brook University and Upstate Medical University.

Binghamton University is conducting research on large language models and antisemitism on social media to detect hateful content. Another project creates 3D foundation models for high-throughput characterization of metal-organic frameworks for climate-change applications.

“I’m proud to see New York leveraging the power of Binghamton University’s expert faculty in striving to make the state a leader in artificial intelligence,” said President Harvey Stenger. “The University’s researchers are already doing tremendous work in AI. By sharing resources across the state, we’re going to solve real-world problems and create new opportunities in economic development and in academic research.”

Empire AI is a consortium of public and private universities in New York — CUNY, SUNY, Cornell University, Columbia University, New York University and Rensselaer Polytechnic Institute — building a state-of-the-art artificial intelligence computing center at University at Buffalo, scheduled to open in 2026.

In October, Empire AI launched Phase Alpha, a smaller but still powerful version of the final supercomputer. 

Associate Professor Jeremy Blackburn, who will serve as the director of Binghamton University’s Institute for AI and Society, sees AI as a tool to gain a large-scale, quantitative understanding of disinformation, harassment campaigns, extremism, risks to children and antisemitism. Previous hardware, however, made it impractical to analyze the sheer amount of data his work explores.

“My research can now be done at a speed I would have never had access to before,” said Blackburn, a faculty member at the Thomas J. Watson College of Engineering and Applied Science’s School of Computing.

“Previously, it would take nearly 20 years to run our experiments on even a sample of the billions of social media data points we collect yearly. By pooling resources from New York state and the six member universities to build something more powerful, I can complete my research on online antisemitism in a matter of weeks. It is hard to overstate just how much more this increase in computing power will allow me to accomplish.”

The Alpha computer is already running at maximum capacity, with 85 projects and more than 250 researchers across the state using it to do work for the public good. Other research at Binghamton includes protecting power systems from malicious attacks and developing a robotic seeing-eye dog for people who are visually impaired.

“Empire AI will also open unique doors for collaboration between disciplines,” Blackburn said. “Scientists and faculty in the humanities and the arts will have expanded access to computing power that was previously unavailable to public research institutions. This coalition will open doors to scholars, especially to those in public universities dedicated to establishing New York state as a leader in AI.”

 

Study links climate change to rising arsenic levels in paddy rice, increasing health risks



Findings suggest a higher incidence of lung, bladder, and skin cancer, as well as cardiovascular disease and diabetes




Columbia University's Mailman School of Public Health





Climate change may significantly impact arsenic levels in paddy rice, a staple food for millions across Asia, reveals a new study from Columbia University’s Mailman School of Public Health. The research shows that increased temperatures above 2°C, coupled with rising carbon dioxide (CO2) levels, lead to higher concentrations of inorganic arsenic in rice, potentially raising lifetime health risks for populations in Asia by 2050. Until now, the combined effects of rising CO2 and temperatures on arsenic accumulation in rice have not been studied in detail. The research done in conjunction with colleagues at John Hopkins Bloomberg School of Public Health and the Chinese Academy of Sciences is published in The Lancet Planetary Health.

“Our results suggest that this increase in arsenic levels could significantly elevate the incidence of heart disease, diabetes, and other non-cancer health effects,” said Lewis Ziska, PhD, Columbia Mailman School associate professor of Environmental Health Sciences. “As rice is a dietary staple in many parts of the world, these changes could lead to a substantial rise in the global burden of cancer, cardiovascular diseases, and other arsenic-related health issues.”

Ziska explained that the higher arsenic levels are likely due to climate-related changes in soil chemistry that favor arsenic that can more easily be absorbed into rice grain. 

“From a health perspective, the toxicological effects of chronic iAs exposure are well established; and include cancers of the lung, bladder, and skin, as well as ischemic heart disease, Emerging evidence also suggests that arsenic exposure may be linked to diabetes, adverse pregnancy outcomes, neurodevelopmental issues, and immune system effects.  In fact, “ingesting rice in regions like southern China and Southeast and South Asia is already a significant source of dietary arsenic and cancer risk,” said Ziska.

By measuring the effects of rising temperatures and CO2 on 28 rice strains over ten years in the field using FACE (Free-Air CO2 Enrichment) methodology, and combining advanced modeling techniques, the team estimated inorganic arsenic doses and health risks for seven Asian countries: Bangladesh, China, India, Indonesia, Myanmar, the Philippines, and Vietnam.

Health risks were calculated for cancer and non-cancer outcomes. Estimates of rice availability in 2021 by country, as reported in Food and Agriculture Organization of the United Nations (FAO) food balance sheets, were used as the starting point for estimating rice ingestion. The standard deviation of rice ingestion per kg bodyweight from the U.S. Environmental Protection Agency data was used to create a normal distribution for each country.

The study's projections for 2050 suggest a sharp rise in lifetime cancer cases, particularly lung and bladder cancers. China is projected to see the highest number of cases, with an estimated 13.4 million cancers linked to rice-based arsenic exposure.

“Based on our findings, we believe there are several actions that could help reduce arsenic exposure in the future,” Ziska noted. “These include efforts in plant breeding to minimize arsenic uptake, improved soil management in rice paddies, and better processing practices. Such measures, along with public health initiatives focused on consumer education and exposure monitoring, could play a critical role in mitigating the health impacts of climate change on rice consumption.”

“Our study underscores the urgent need for action to reduce arsenic exposure in rice, especially as climate change continues to affect global food security,” says Ziska.

Co-authors are Dongming Wang, Brent F. Kim, Keeve E. Nachman, Andrea A. Chiger, Julie Herbstman, Irakli Loladze, Fang-Jie Zhao, Chuan Chen, Axiang Gao, Yongguan Zhu,  Fangbai Li, Ren Fang Shen, Xiaoyuan Yan, Jiabao Zhang,  Chuang Cai, Lian Song, Min Shen, Chuanqi Ma, XiongYang, Wei Zhou, Yujun Wang, Haoye Tang, Yu Jiang, Yanfeng Ding, Wuxing Liu, Jianqiang Sun, Wei Zhou, Ana Navas-Acien, Chunwu Zhu.

 Author affiliations and sources of funding can be found in the paper.

Columbia University Mailman School of Public Health

Founded in 1922, the Columbia University Mailman School of Public Health pursues an agenda of research, education, and service to address the critical and complex public health issues affecting New Yorkers, the nation and the world. The Columbia Mailman School is the third largest recipient of NIH grants among schools of public health. Its nearly 300 multi-disciplinary faculty members work in more than 100 countries around the world, addressing such issues as preventing infectious and chronic diseases, environmental health, maternal and child health, health policy, climate change and health, and public health preparedness. It is a leader in public health education with more than 1,300 graduate students from 55 nations pursuing a variety of master’s and doctoral degree programs. The Columbia Mailman School is also home to numerous world-renowned research centers, including ICAP and the Center for Infection and Immunity. For more information, please visit www.mailman.columbia.edu.

 

 

Blood pressure: New research shows a changing climate may jeopardise global blood supply



A new study published in The Lancet Planetary Health suggests a changing climate threatens the continuous availability of safe blood across the world.



Australian Red Cross Lifeblood

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Credit: Red Cross Lifeblood




Blood pressure: New research shows a changing climate may jeopardise global blood supply   

A new study published in The Lancet Planetary Health suggests a changing climate threatens the continuous availability of safe blood across the world.

Researchers at the University of the Sunshine Coast and Australian Red Cross Lifeblood say health issues, the spread of infectious disease and extreme weather exacerbated by climate change will impact the ability of people to donate, and at the same time may trigger a rise in the need for blood.

Lifeblood researcher and UniSC Adjunct Research Fellow Dr Elvina Viennet said this threatened the safety and supply of life-saving blood products crucial for surgeries, trauma care, chronic disease management – and saving lives in emergency situations.

“Warmer temperatures and natural disasters such as heatwaves, floods, cyclones and bushfires are expected to become more frequent and severe,” Dr Viennet said.

“As well as limiting the mobility of large numbers of people, these events disrupt the storage, safety, and transportation of blood which has a short shelf life.

We experienced this recently with ex-Tropical Cyclone Alfred in Australia, when an extreme weather event drastically reduced national blood supplies for the first time.”

Lead researcher, UniSC Associate Professor Helen Faddy said the study was the first to globally examine how a changing climate could affect each stage of the blood supply chain, based on a comprehensive literature review of international studies.

“While many studies have explored the broader health effects of climate change, we sought to fill gaps in understanding the full extent of the risks – from donor health and collection logistics to the processing, storage and distribution of products,” she said.

The finding suggest climate change may impact some infectious diseases that can be transmitted via blood and can prevent people from donating.

“For example, predictions of increased rainfall and warmer temperatures in certain regions including Australia, could intensify mosquito-borne diseases such as Dengue Fever, West Nile Virus and Malaria, and potentially see them spread to new areas,” Dr Faddy said.

“At the same time, shifts in disease prevalence and natural disaster frequency could increase the demand for blood transfusions due to conditions such as pregnancy complications, cardiovascular disease and sickle cell disease.

“We could also face greater difficulty in finding the right blood for patients. With rising sea levels increasing migration rates, it’s essential to have more donors from a variety of ethnic backgrounds, and to increase the number of people who give blood.”

Less obvious health conditions and heat-related illness could also impact donors, staff, and volunteers.

“We could see new diseases emerge, health issues such as blood pressure and hydration that are exacerbated by heat, as well as psychological distress and ‘climate anxiety’, impact donors,” she said.

The study emphasises the need to reduce reliance on traditional blood supply chains and have adaptable strategies that offer rapid responses to climate-related challenges.

The researchers recommend Governments and blood services can prepare with critical tools such as early warning systems, disease surveillance, flexible approaches to donor eligibility and blood transport in emergencies, hospital preparation, and expanding collection services so donations can be relocated quickly.

“Recent global innovations include cell salvage techniques during surgery, the use of drones to transport blood when other transit is disrupted, and walking blood banks, which collect donations at the site of crises,” Dr Faddy said.

“As our environment evolves, we need to reduce reliance on traditional blood supply chains and have adaptable strategies that offer rapid responses to climate-related challenges.”

d emergency blood type

Flooding due to climate change 

Mozzie sucking blood

Donated blood at Australian Red Cross Lifeblood

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Australian Red Cross Lifeblood