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Perpendicular acceleration of near-equatorially mirroring protons by electromagnetic ion cyclotron (EMIC) waves

Publication date: 1 November 2025

Source: Advances in Space Research, Volume 76, Issue 9

Author(s): Su Zhou, Yongzhi Cai, Shunli Li, Zongxian Wu, Ying Hou

Aerodynamic shape optimization of hypersonic vehicle based on improved class-shape-transformation method

Publication date: 1 November 2025

Source: Advances in Space Research, Volume 76, Issue 9

Author(s): Menghan Yin, Erming He, Yongzhi Li, Cong Zhang

Landslide susceptibility mapping using advanced ensemble learning techniques integrating a reduced error pruning tree

Publication date: 1 November 2025

Source: Advances in Space Research, Volume 76, Issue 9

Author(s): Junpeng Huang, Zizhao Zhang, Sixiang Ling, Kai Chen, Guangming Shi, Yanyang Zhang

What are a geospace storm and a pan-planetary storm?

Publication date: 1 November 2025

Source: Advances in Space Research, Volume 76, Issue 9

Author(s): L.F. Chernogor

Correlation between ballistic coefficients and natural decay times of space debris in very low Earth orbit

Publication date: 1 November 2025

Source: Advances in Space Research, Volume 76, Issue 9

Author(s): Jungseon Lee, Jinah Lee, Chandeok Park, Hancheol Cho, Dongwon Jung

Modeling and vibration analysis of a long and flexible arm applied to realize the space docking process

Publication date: 1 November 2025

Source: Advances in Space Research, Volume 76, Issue 9

Author(s): Jiahe Yan, Haifei Zhu, Hanzhen Xiao

Analysis of a conceptual multi-node flexible small body lander: Bounce suppression and active control

Publication date: 1 November 2025

Source: Advances in Space Research, Volume 76, Issue 9

Author(s): Jingxuan Chai, Jie Mei, Youmin Gong, Xinyu Wu, Guangfu Ma, Weiren Wu

Distributed prescribed-time attitude consensus tracking control for multiple flexible spacecraft under time-varying actuator faults

Publication date: 1 November 2025

Source: Advances in Space Research, Volume 76, Issue 9

Author(s): Shilei Cao, Man Yang, Jian Liu

Multiple source characteristics in coseismic ionospheric disturbances for the April 2, 2024 Hualien earthquake from GNSS observations

Publication date: 1 November 2025

Source: Advances in Space Research, Volume 76, Issue 9

Author(s): Qingshan Ruan, Hang Liu, Jianghe Chen

Optical tracklet association with a defined probabilistic correlation measure

Publication date: 1 November 2025

Source: Advances in Space Research, Volume 76, Issue 9

Author(s): Pei Chen, Zihan Zhou, Xuejian Mao

Preliminary investigation of multi-body orbit architectures for Mars surface positioning, navigation, and timing

Publication date: 1 November 2025

Source: Advances in Space Research, Volume 76, Issue 9

Author(s): Kaitlin R. Roberts, Robert A. Bettinger

Fuel-optimal boost-back guidance algorithms for reusable launch vehicles

Publication date: 1 November 2025

Source: Advances in Space Research, Volume 76, Issue 9

Author(s): Byeong-Un Jo, Seungyeop Han, Jaemyung Ahn

Peatlands' 'huge reservoir' of carbon at risk of release, researchers warn

Phys.org: Earth science - Thu, 10/23/2025 - 18:00
Peatlands make up just 3% of Earth's land surface but store more than 30% of the world's soil carbon, preserving organic matter and sequestering its carbon for tens of thousands of years. A new study sounds the alarm that an extreme drought event could quadruple peatland carbon loss in a warming climate.

Tiny ocean organisms missing from climate models may hold the key to Earth's carbon future

Phys.org: Earth science - Thu, 10/23/2025 - 18:00
The ocean's smallest engineers, calcifying plankton, quietly regulate Earth's thermostat by capturing and cycling carbon. However, a new review published in Science by an international team led by the Institute of Environmental Science and Technology at the Universitat Autònoma de Barcelona (ICTA-UAB) (Spain) finds that these organisms, coccolithophores, foraminifers, and pteropods, are oversimplified in the climate models used to predict our planet's future.

How Hurricane Helene changed groundwater chemistry

Phys.org: Earth science - Thu, 10/23/2025 - 17:58
Late at night on 26 September 2024, Hurricane Helene made landfall on Florida's big bend. The physical damage was devastating and well-documented, but an additional, unseen potential impact lurked underfoot.

The island split in two by time: How ancient rifting reshaped Madagascar's landscape

Phys.org: Earth science - Thu, 10/23/2025 - 17:10
Madagascar's landscape tells a story of deep time: ancient rifting and geological tilting sculpted the island's dramatic topography and steered its rivers, setting the stage for the evolution of its extraordinary biodiversity.

Ancient 'salt mountains' in southern Australia once created refuges for early life

Phys.org: Earth science - Thu, 10/23/2025 - 15:58
Salt is an essential nutrient for the human body. But hundreds of millions of years before the first humans, salt minerals once shaped entire landscapes. They even determined where early life on Earth could thrive.

Plastic pollution could linger at ocean surfaces for over a century, new research finds

Phys.org: Earth science - Thu, 10/23/2025 - 13:38
Scientists from the Department of Geography and Environmental Science at Queen Mary University of London have developed a simple model to show how buoyant plastic can settle through the water column and they predict it could take over 100 years to remove plastic waste from the ocean's surface.

New Satellite Data Reveal a Shift in Earth’s Once-Balanced Energy System

EOS - Thu, 10/23/2025 - 13:22

Years ago, scientists noted something odd: Earth’s Northern and Southern Hemispheres reflect nearly the same amount of sunlight back into space. The reason why this symmetry is odd is because the Northern Hemisphere has more land, cities, pollution, and industrial aerosols. All those things should lead to a higher albedo—more sunlight reflected than absorbed. The Southern Hemisphere is mostly ocean, which is darker and absorbs more sunlight.

New satellite data, however, suggest that symmetry is breaking.

From Balance to Imbalance

In a new study published in the Proceedings of the National Academy of Sciences of the United States of America, Norman Loeb, a climate scientist at NASA’s Langley Research Center, and colleagues analyzed 24 years of observations from NASA’s Clouds and the Earth’s Radiant Energy System (CERES) mission.

They found that the Northern Hemisphere is darkening faster than the Southern Hemisphere. In other words, it’s absorbing more sunlight. That shift may alter weather patterns, rainfall, and the planet’s overall climate in the decades ahead.

Since 2000, CERES has recorded how much sunlight is absorbed and reflected, as well as how much infrared (longwave) radiation escapes back to space. Loeb used these measurements to analyze how Earth’s energy balance changed between 2001 and 2024. The energy balance tells scientists whether the planet is absorbing more energy than it releases and how that difference varies between hemispheres.

“Any object in the universe has a way to maintain equilibrium by receiving energy and giving off energy. That’s the fundamental law governing everything in the universe,” said Zhanqing Li, a climate scientist at the University of Maryland who was not part of the study. “The Earth maintains equilibrium by exchanging energy between the Sun and the Earth’s emitted longwave radiation.”

The team found that the Northern Hemisphere is absorbing about 0.34 watt more solar energy per square meter per decade than the Southern Hemisphere. “This difference doesn’t sound like much, but over the whole planet, that’s a huge number,” said Li.

Results pointed to three main reasons for the Northern Hemisphere darkening: melting snow and ice, declining air pollution, and rising water vapor.

To figure out what was driving this imbalance, the scientists applied a technique called partial radiative perturbation (PRP) analysis. The PRP method separates the influence of factors such as clouds, aerosols, surface brightness, and water vapor from calculations of how much sunlight each hemisphere absorbs.

The results pointed to three main reasons for the Northern Hemisphere darkening: melting snow and ice, declining air pollution, and rising water vapor.

“It made a lot of sense,” Loeb said. “The Northern Hemisphere’s surface is getting darker because snow and ice are melting. That exposes the land and ocean underneath. And pollution has gone down in places like China, the U.S., and Europe. It means there are fewer aerosols in the air to reflect sunlight. In the Southern Hemisphere, it’s the opposite.”

“Because the north is warming faster, it also holds more water vapor,” Loeb continued. “Water vapor doesn’t reflect sunlight, it absorbs it. That’s another reason the Northern Hemisphere is taking in more heat.”

Curiosity About Cloud Cover

One of the study’s interesting findings is what didn’t change over the past 20 years: cloud cover.

“The clouds are a puzzle to me because of this hemispheric symmetry,” Loeb said. “We kind of questioned whether this was a fundamental property of the climate system. If it were, the clouds should compensate. You should see more cloud reflection in the Northern Hemisphere relative to the Southern Hemisphere, but we weren’t seeing that.”

Loeb worked with models to understand these clouds.

“We are unsure about the clouds,” said Loeb.

“Understanding aerosol and cloud interactions is still a major challenge,” agreed Li. “Clouds remain the dominant factor adjusting our energy balance,” he said. “It’s very important.”

Still, Li said that “Dr. Norman Loeb’s study shows that not only does [the asymmetry] exist, but it’s important enough to worry about what’s behind it.”

Loeb is “excited about the new climate models coming out soon” and how they will further his work. “It’ll be interesting to revisit this question with the latest and greatest models.”

—Larissa G. Capella (@CapellaLarissa), Science Writer

Citation: Capella, L. G. (2025), New satellite data reveal a shift in Earth’s once-balanced energy system, Eos, 106, https://doi.org/10.1029/2025EO250399. Published on 23 October 2025. Text © 2025. The authors. CC BY-NC-ND 3.0
Except where otherwise noted, images are subject to copyright. Any reuse without express permission from the copyright owner is prohibited.

Melting Cylinders of Ice Reveal an Iceberg’s Tipping Point

EOS - Thu, 10/23/2025 - 13:22

The titanic dangers icebergs pose to ships are well documented. Sometimes, however, icebergs themselves can capsize, creating earthquakes and tsunamis or even pushing entire glaciers backward. Most of those dramatic events occur right after the chunk of floating ice splits off from its source, but sometimes icebergs flip over in the open ocean.

Earlier lab experiments using simulated plastic icebergs showed that the energy released in capsize events can rival nuclear weapon blasts. But beyond an understanding that capsize events are likely related to melting induced by ocean warming, knowing why icebergs flip is a question that’s harder to answer. Large variations in iceberg size and shape, along with slow drifting across wide distances, make studying icebergs expensive and challenging.

One solution: make miniature icebergs in the lab and watch them melt under controlled conditions.

“Understanding the mathematics and the physics of what’s going on at a base level is important in order to scale up.”

“We wanted to study the simplest capsize problem we could come up with,” said Bobae Johnson, a physicist and Ph.D. student at the Courant Institute at New York University. She and her colleagues simplified and standardized iceberg shape to a cylinder of pure water ice 8 centimeters in diameter and 24 centimeters long. In their article for Physical Review Fluids, they described how each cylinder flipped several times over the course of a 30-minute experiment.

“It is good to look at these things on smaller scales because even what we were doing in the simplest setting gave us something very complex,” Johnson said. “Understanding the mathematics and the physics of what’s going on at a base level is important in order to scale up.”

From their experiments, Johnson and her colleagues linked the different rates of ice melt above and below the waterline to dynamic changes in the shape of the iceberg—including the location of the center of mass, which makes them flip. Despite the small scale of the experiments, the implications could be enormous.

“Icebergs play a key role in the climate system,” said Sammie Buzzard, a glaciologist at the Centre for Polar Observation and Modelling and Northumbria University who was not involved in the experiments. “When they melt, they add fresh, cold water to the ocean, which can impact currents.”

Icebergs, Soda Pop, and Cheerios

Real-world icebergs range in size from about 15 meters to hundreds of kilometers across, rivaling the size of some small nations. Tolkienesque mountain-like structures (“iceberg” literally means “ice mountain”) split off from glaciers, whereas flat slablike icebergs tend to break off from ice sheets like those surrounding Antarctica.

“An iceberg’s shape determines how it floats in the water and which parts are submerged and which parts sit above the ocean’s surface,” Buzzard said, adding that icebergs change shape as they melt or erode via wind and wave action. But the precise manner of this change is uncertain because in situ measurements are challenging. “If this erosion changes the shape enough that the iceberg is no longer stable in the water, [the iceberg] can suddenly flip over into a position in which it is stable.”

“Even if lab experiments aren’t exactly the same as a natural system, they can go a long way to improving our understanding of [iceberg capsizing].”

Whatever their major differences in shape and size, because they are fresh water floating on salt water, icebergs all exhibit the similar property that roughly 10% off their mass is above water, with the remaining 90% beneath. The similarities provided the starting point for the cylindrical iceberg experiments performed by Johnson and her collaborators.

A sphere or irregular body can rotate in many different directions, but a cylinder with a length greater than the diameter of its circular face floating in water will rotate along only one axis, effectively reducing the problem from three dimensions to two.

Standardizing the shape of the icebergs wasn’t the only simplification the team made. Under natural conditions, ice freezes from the outside in, which traps a lot of air. As icebergs melt, they sometimes release enough trapped air bubbles to make the surrounding water fizz like an opened can of soda pop. This effect can create chaotic motion in samples, so Johnson and collaborators opted to eliminate bubbles entirely in their experiment. To do so, they froze water in cylindrical molds suspended in extremely cold brine and stirred the water to drive residual air out—a process that took 24 to 48 hours for each cylinder.

This video depicts the flow of water beneath the surface of a melting model iceberg. Credit: New York University’s Applied Mathematics Laboratory

Finally, to keep the cylinders from drifting randomly in the ocean simulation tank, the researchers exploited the “Cheerios effect.” Floating cereal pieces tend to group together because of surface tension, so the team 3D printed pieces of flat plastic and coated them with wax. Placing those objects in the tank created a meniscus on either side of the cylinder, keeping it in place so the only motion it exhibited was the rotation they were looking for.

“The ice melts very slowly in the air and very quickly underwater,” Johnson said. In the experiment, that difference resulted in a gravitational instability as the center of mass shifted upward, making the whole cylinder flip. “Every time the ice locks into one position, it carves out a facet above the water and very sharp corners at the waterline, giving you a shape that looks quasi pentagonal about halfway through the experiment. We ran many, many experiments, and this happened across all of them.”

Buzzard emphasized the need for this sort of work. “Even if lab experiments aren’t exactly the same as a natural system, they can go a long way to improving our understanding of [iceberg capsizing],” she said. Every flip of a simulated iceberg could help us understand the effects on the warming ocean and the connection between small occurrences and global consequences.

—Matthew R. Francis (@BowlerHatScience.org), Science Writer

Citation: Francis, M. R. (2025), Melting cylinders of ice reveal an iceberg’s tipping point, Eos, 106, https://doi.org/10.1029/2025EO250390. Published on 23 October 2025. Text © 2025. The authors. CC BY-NC-ND 3.0
Except where otherwise noted, images are subject to copyright. Any reuse without express permission from the copyright owner is prohibited.

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