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    Rapid melting is eroding vulnerable cracks in Thwaites Glacier’s underbelly

    Antarctica’s most vulnerable climate hot spot is a remote and hostile place — a narrow sliver of seawater, beneath a slab of floating ice more than half a kilometer thick. Scientists have finally explored it, and uncovered something surprising.

    “The melt rate is much weaker than we would have thought, given how warm the ocean is,” says Peter Davis, an oceanographer at the British Antarctic Survey in Cambridge who was part of the team that drilled a narrow hole into this nook and lowered instruments into it. The finding might seem like good news — but it isn’t, he says. “Despite those low melt rates, we’re still seeing rapid retreat” as the ice vanishes faster than it’s being replenished.

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    Davis and about 20 other scientists conducted this research at Thwaites Glacier, a massive conveyor belt of ice about 120 kilometers wide, which flows off the coastline of West Antarctica. Satellite measurements show that Thwaites is losing ice more quickly than at any time in the last few thousand years (SN: 6/9/22). It has accelerated its flow into the ocean by at least 30 percent since 2000, hemorrhaging over 1,000 cubic kilometers of ice — accounting for roughly half of the ice lost from all of Antarctica.

    Much of the current ice loss is driven by warm, salty ocean currents that are destabilizing the glacier at its grounding zone — the crucial foothold, about 500 meters below sea level at the drilling location, where the ice lifts off its bed and floats (SN: 4/9/21).

    Now, this first-ever look at the glacier’s underbelly near the grounding zone shows that the ocean is attacking it in previously unknown and troubling ways.

    When the researchers sent a remote-operated vehicle, or ROV, down the borehole and into the water below, they found that much of the melting is concentrated in places where the glacier is already under mechanical stress — within massive cracks called basal crevasses. These openings slice up into the underside of the ice.

    Even a small amount of melting at these weak spots could inflict a disproportionately large amount of structural damage on the glacier, the researchers report in two papers published February 15 in Nature.

    These results are “a bit of a surprise,” says Ted Scambos, a glaciologist at the University of Colorado Boulder who was not part of the team. Thwaites and other glaciers are monitored mostly with satellites, which make it appear that thinning and melting happen uniformly under the ice.

    As the world continues to warm due to human-caused climate change, the shrinking glacier itself has the potential to raise global sea level by 65 centimeters over a period of centuries. Its collapse would also destabilize the remainder of the West Antarctic Ice Sheet, triggering an eventual three meters of global sea level rise.

    With these new results, Scambos says, “we’re seeing in much more detail processes that will be important for modeling” how the glacier responds to future warming, and how quickly sea level will rise.

    A cold, thin layer shields parts of Thwaites Glacier’s underside

    Simply getting these observations “is kind of like a moon shot, or even a Mars shot,” Scambos says. Thwaites, like most of the West Antarctic Ice Sheet, rests on a bed that is hundreds of meters below sea level. The floating front of the glacier, called an ice shelf, extends 15 kilometers out onto the ocean, creating a roof of ice that makes this spot almost entirely inaccessible to humans. “This might represent the pinnacle of exploration” in Antarctica, he says.

    These new results stem from a $50 million effort — the International Thwaites Glacier Collaboration — conducted by the United States’ National Science Foundation and United Kingdom’s Natural Environment Research Council. The research team, one of eight funded by that collaboration, landed on the snowy, flat expanse of Thwaites in the final days of 2019.

    The researchers used a hot water drill to melt a narrow hole, not much wider than a basketball, through more than 500 meters of ice. Below the ice sat a water column that was only 54 meters thick.

    When Davis and his colleagues measured the temperature and salinity of that water, they found that most of it was about 2 degrees Celsius above freezing — potentially warm enough to melt 20 to 40 meters of ice per year. But the underside of the ice seems to be melting at a rate of only 5 meters per year, researchers report in one of the Nature papers. The team calculated the melt rate based on the water’s salinity, which reveals the ratio of seawater, which is salty, to glacial meltwater, which is fresh.

    The reason for that slow melt quickly emerged: Just beneath the ice sat a layer of cold, buoyant water, only 2 meters thick, derived from melted ice. “There is pooling of much fresher water at the ice base,” says Davis, and this cold layer shields the ice from warmer water below. 

    Those measurements provided a snapshot right at the borehole. Several days after the hole was opened, the researchers began a broader exploration of the unmapped ocean cavity under the ice.

    Workers winched a skinny, yellow and black cylinder down the borehole. This ROV, called Icefin, was developed over the last seven years by a team of engineers led by Britney Schmidt, a glaciologist at Cornell University.

    A remote-operated vehicle called Icefin was lowered down a borehole, through more than 500 meters of ice, to measure ocean currents and ice melting rates under Thwaites Glacier.Icefin/ITGC/Schmidt

    Schmidt and her team piloted the craft from a nearby tent, monitoring instruments while she steered the craft with gentle nudges to the buttons of a PlayStation 4 controller. The smooth, mirrorlike ceiling of ice scrolled silently past on a computer monitor — the live video feed piped up through 3½ kilometers of fiber-optic cable.

    As Schmidt guided Icefin about 1.6 kilometers upstream from the borehole, the water column gradually tapered, until less than a meter of water separated the ice from the seafloor below. A few fish and shrimplike crustaceans called amphipods flitted among otherwise barren piles of gravel.

    This new section of seafloor — revealed as the ice thins, lifts and floats progressively farther inland — had been exposed “for less than a year,” Schmidt says.

    Now and then, Icefin skimmed past a dark, gaping cleft in the icy ceiling, a basal crevasse. Schmidt steered the craft into several of these gaps — often over 100 meters wide — and there, she saw something striking.

    Melting of Thwaites’ underbelly is concentrated in deep crevasses

    The vertical walls of the crevasses were scalloped rather than smooth, suggesting a higher rate of melting than that of the flat icy ceiling. And in these places, the video became blurry as the light refracted through vigorously swirling eddies of salty water and freshwater. That turbulent swirling of warm ocean water and cold meltwater is breaking up the cold layer that insulates the ice, pulling warm, salty water into contact with it, the scientists think.

    Schmidt’s team calculated that the walls of the crevasses are melting at rates of up to 43 meters per year, the researchers report in the second Nature paper. The researchers also found rapid melt in other places where the level ceiling of ice is punctuated by short, steep sections.

    The greater turbulence and higher melt also appear driven by ocean currents within the crevasses. Each time Schmidt steered Icefin up into a crevasse, the ROV detected streams of water flowing through it, as though the crevasse were an upside-down ditch. These currents moved up to twice as fast as the currents outside of crevasses.

    The fact that melting is concentrated in crevasses has huge implications, says Peter Washam, an oceanographer on Schmidt’s team at Cornell: “The ocean is widening these features by melting them faster.”

    This could greatly accelerate the years-long process by which some of these cracks propagate hundreds of meters up through the ice until they break through at the top — calving off an iceberg that drifts away. It could cause the floating ice shelf, which presses against an undersea mountain and buttresses the ice behind it, to break apart more quickly than predicted. This, in turn, could cause the glacier to spill ice into the ocean more quickly (SN: 12/13/21). “It’s going to have an impact on the stability of the ice,” Washam says.

    [embedded content]
    This video, captured by a remote-operated vehicle called Icefin, shows the underside of Thwaites Glacier where it flows off the coastline of West Antarctica. Horizontal sections of the ice are smooth, indicating slow melting. But on steep ice surfaces — especially along the walls of deep cracks in the ice — the surfaces are scalloped, suggesting a much higher rate of melt, driven by turbulent swirling of warm, salty ocean water and cold, fresh meltwater. An example of the difference between those two surfaces is clearly visible from 0:11 to 0:13 in the video, when Icefin captures a scalloped vertical surface intersecting with a smooth horizontal one.

    These new data will improve scientists’ ability to predict the future retreat of Thwaites and other Antarctic glaciers, says Eric Rignot, a glaciologist at NASA’s Jet Propulsion Laboratory in Pasadena, Calif., who assisted the team by providing satellite measurements of changes in the glacier. “You just cannot guess what the water structure might look like in these zones until you observe it,” he says.

    But more work is needed to fully understand Thwaites and how it will further change as the world continues to warm. The glacier consists of two side-by-side fast-moving lanes of ice — one moving 3 kilometers per year, the other about 1 kilometer per year. Due to safety concerns, the team visited the slower lane — which still proved extremely challenging. Rignot says that scientists must eventually visit the fast lane, whose upper surface is more cracked up with crevasses — making it even harder to land aircraft and operate field camps.

    The research reported today “is a very important step, but it needs to be followed by a second step,” the investigation of the glacier’s fast lane, he says. “It doesn’t matter how hard it is.” More

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    Smash or pass? This computer can tell

    Engineers at the University of Cincinnati say the technology might not be far off. They trained a computer — using data from wearable technology that measures respiration, heart rates and perspiration — to identify the type of conversation two people were having based on their physiological responses alone.
    Researchers studied a phenomenon in which people’s heart rates, respiration and other autonomic nervous system responses become synchronized when they talk or collaborate. Known as physiological synchrony, this effect is stronger when two people engage deeply in a conversation or cooperate closely on a task.
    “Physiological synchrony shows up even when people are talking over Zoom,” said study co-author Vesna Novak, an associate professor of electrical engineering in UC’s College of Engineering and Applied Science.
    In experiments with human participants, the computer was able to differentiate four different conversation scenarios with as much as 75% accuracy. The study is one of the first of its kind to train artificial intelligence how to recognize aspects of a conversation based on the participants’ physiology alone.
    The study was published in the journal IEEE Transactions on Affective Computing.

    Lead author and UC doctoral student Iman Chatterjee said a computer could give you honest feedback about your date — or yourself.
    “The computer could tell if you’re a bore,” Chatterjee said. “A modified version of our system could measure the level of interest a person is taking in the conversation, how compatible the two of you are and how engaged the other person is in the conversation.”
    Chatterjee said physiological synchrony is likely an evolutionary adaptation. Humans evolved to share and collaborate with each other, which manifests even at a subconscious level, he said.
    “It is certainly no coincidence,” he said. “We only notice physiological synchrony when we measure it, but it probably creates a better level of coordination.”
    Studies have shown that physiological synchrony can predict how well two people will work together to accomplish a task. The degree of synchrony also correlates with how much empathy a patient perceives in a therapist or the level of engagement students feel with their teachers.
    “You could probably use our system to determine which people in an organization work better together in a group and which are naturally antagonistic,” Chatterjee said.
    This aspect of affective computing holds huge potential for providing real-time feedback for educators, therapists or even autistic people, Novak said.
    “There are a lot of potential applications in this space. We’ve seen it pitched to look for implicit bias. You might not even be aware of these biases,” Novak said. More

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    Atom-thin walls could smash size, memory barriers in next-gen devices

    For all of the unparalleled, parallel-processing, still-indistinguishable-from-magic wizardry packed into the three pounds of the adult human brain, it obeys the same rule as the other living tissue it controls: Oxygen is a must.
    So it was with a touch of irony that Evgeny Tsymbal offered his explanation for a technological wonder — movable, data-covered walls mere atoms wide — that may eventually help computers behave more like a brain.
    “There was unambiguous evidence that oxygen vacancies are responsible for this,” said Tsymbal, George Holmes University Professor of physics and astronomy at the University of Nebraska-Lincoln.
    In partnership with colleagues in China and Singapore, Tsymbal and a few Husker alumni have demonstrated how to construct, control and explain the oxygen-deprived walls of a nanoscopically thin material suited to next-gen electronics.
    Unlike most digital data-writing and -reading techniques, which speak only the binary of 1s and 0s, these walls can talk in several electronic dialects that could allow the devices housing them to store even more data. Like synapses in the brain, the passage of electrical spikes sent via the walls can depend on which signals have passed through before, lending them an adaptability and energy-efficiency more akin to human memory. And much as brains maintain memories even when their users sleep, the walls can retain their data states even if their devices turn off — a precursor to electronics that power back on with the speed and simplicity of a light.
    The team investigated the barrier-smashing walls in a nanomaterial, named bismuth ferrite, that can be sliced thousands of times thinner than a human hair. Bismuth ferrite also boasts a rare quality known as ferroelectricity: The polarization, or separation, of its positive and negative electric charges can be flipped by applying just a pinch of voltage, writing a 1 or 0 in the process. Contrary to conventional DRAM, a dynamic random-access memory that needs to be refreshed every few milliseconds, that 1 or 0 remains even when the voltage is removed, granting it the equivalent of long-term memory that DRAM lacks.

    Usually, that polarization is read as a 1 or 0, and flipped to rewrite it as a 0 or 1, in a region of material called a domain. Two oppositely polarized domains meet to form a wall, which occupies just a fraction of the space dedicated to the domains themselves. The few-atom thickness of those walls, and the unusual properties that sometimes emerge in or around them, have cast them as prime suspects in the search for new ways to squeeze ever-more functionality and storage into shrinking devices.
    Still, walls that run parallel to the surface of a ferroelectric material — and net an electric charge usable in data processing and storage — have proven difficult to find, let alone regulate or create. But about four years ago, Tsymbal began talking with Jingsheng Chen from the National University of Singapore and He Tian from China’s Zhejiang University. At the time, Tian and some colleagues were pioneering a technique that allowed them to apply voltage on an atomic scale, even as they recorded atom-by-atom displacements and dynamics in real time.
    Ultimately, the team found that applying just 1.5 volts to a bismuth ferrite film yielded a domain wall parallel to the material’s surface — one with a specific resistance to electricity whose value could be read as a data state. When voltage was withdrawn, the wall, and its data state, remained.
    When the team cranked up the voltage, the domain wall began migrating down the material, a behavior seen in other ferroelectrics. Whereas the walls in those other materials had then propagated perpendicular to the surface, though, this one remained parallel. And unlike any of its predecessors, the wall adopted a glacial pace, migrating just one atomic layer at a time. Its position, in turn, corresponded with changes in its electrical resistance, which dropped in three distinct steps — three more readable data states — that emerged between the application of 8 and 10 volts.
    The researchers had nailed down a few W’s — the what, the where, the when — critical to eventually employing the phenomenon in electronic devices. But they were still missing one. Tsymbal, as it happened, was among the few people qualified to address it.

    “There was a puzzle,” Tsymbal said. “Why does it happen? And this is where theory helped.”
    Most domain walls are electrically neutral, possessing neither a positive nor a negative charge. That’s with good reason: A neutral wall requires little energy to maintain its electric state, effectively making it the default. The domain wall the team identified in the ultra-thin bismuth ferrite, by contrast, possessed a substantial charge. And that, Tsymbal knew, should have kept it from stabilizing and persisting. Yet somehow, it was managing to do just that, seeming to flout the rules of condensed-matter physics.
    There had to be an explanation. In his prior research, Tsymbal and colleagues had found that the departure of negatively charged oxygen atoms, and the positively charged vacancies they left in their wake, could impede a technologically useful outcome. This time, Tsymbal’s theory-backed calculations suggested the opposite — that the positively charged vacancies were compensating for other negative charges accumulating at the wall, essentially fortifying it in the process.
    Experimental measurements from the team would later show that the distribution of charges in the material lined up almost exactly with the location of the domain wall, exactly as the calculations had predicted. If oxygen vacancies turn up in other ferroelectric playgrounds, Tsymbal said, they could prove vital to better understanding and engineering devices that incorporate the prized class of materials.
    “From my perspective, that was the most exciting,” said Tsymbal, who undertook the research with support from the university’s quantum-focused EQUATE project. “This links ferroelectricity with electrochemistry. We have some kind of electrochemical processes — namely, the motion of oxygen vacancies — which basically control the motion of these domain walls.
    “I think that this mechanism is very important, because what most people are doing — including us, theoretically — is looking at pristine materials, where polarization switches up and down, and studying what happens with the resistance. All the experimental interpretations of this behavior were based on this simple picture of polarization. But here, it’s not only the polarization. It involves some chemical processes inside of it.”
    The team detailed its findings in the journal Nature. Tsymbal, Tian and Chen authored the study with Ze Zhang, Zhongran Liu, Han Wang, Hongyang Yu, Yuxuan Wang, Siyuan Hong, Meng Zhang, Zhaohui Ren and Yanwu Xie, as well as Husker alumni Ming Li, Lingling Tao and Tula Paudel. More

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    Chiral phonons create spin current without needing magnetic materials

    Researchers from North Carolina State University and the University of North Carolina at Chapel Hill used chiral phonons to convert wasted heat into spin information — without needing magnetic materials. The finding could lead to new classes of less expensive, energy-efficient spintronic devices for use in applications ranging from computational memory to power grids.
    Spintronic devices are electronic devices that harness the spin of an electron, rather than its charge, to create current used for data storage, communication, and computing. Spin caloritronic devices — so-called because they utilize thermal energy to create spin current — are promising because they can convert waste heat into spin information, which makes them extremely energy efficient. However, current spin caloritronic devices must contain magnetic materials in order to create and control the electron’s spin.
    “We used chiral phonons to create a spin current at room temperature without needing magnetic materials,” says Dali Sun, associate professor of physics and member of the Organic and Carbon Electronics Lab (ORaCEL) at North Carolina State University.
    “By applying a thermal gradient to a material that contains chiral phonons, you can direct their angular momentum and create and control spin current.” says Jun Liu, associate professor of mechanical and aerospace engineering at NC State and ORaCEL member.
    Both Liu and Sun are co-corresponding authors of the research, which appears in Nature Materials.
    Chiral phonons are groups of atoms that move in a circular direction when excited by an energy source — in this case, heat. As the phonons move through a material, they propagate that circular motion, or angular momentum, through it. The angular momentum serves as the source of spin, and the chirality dictates the direction of the spin.

    “Chiral materials are materials that cannot be superimposed on their mirror image,” Sun says. “Think of your right and left hands — they are chiral. You can’t put a left-handed glove on a right hand, or vice versa. This ‘handedness’ is what allows us to control the spin direction, which is important if you want to use these devices for memory storage.”
    The researchers demonstrated chiral phonon-generated spin currents in a two-dimensional layered hybrid organic-inorganic perovskite by using a thermal gradient to introduce heat to the system.
    “A gradient is needed because temperature difference in the material — from hot to cold — drives the motion of the chiral phonons through it,” says Liu. “The thermal gradient also allows us to use captured waste heat to generate spin current.”
    The researchers hope that the work will lead to spintronic devices that are cheaper to produce and can be used in a wider variety of applications.
    “Eliminating the need for magnetism in these devices means you’re opening the door wide in terms of access to potential materials,” Liu says. “And that also means increased cost-effectiveness.”
    “Using waste heat rather than electric signals to generate spin current makes the system energy efficient — and the devices can operate at room temperature,” Sun says. “This could lead to a much wider variety of spintronic devices than we currently have available.”
    The research was supported by the National Science Foundation and the U.S. Department of Energy. Wei You, professor of chemistry at the University of North Carolina at Chapel Hill and a member of ORaCEL, is also a co-corresponding author of the study. More