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How Greenland’s Glacial Troughs Influence Ocean Circulation

EOS - Thu, 05/29/2025 - 13:02
Source: Journal of Geophysical Research: Oceans

The Atlantic Meridional Overturning Circulation (AMOC) serves as the Atlantic Ocean’s conveyor belt, transporting warm water north toward the Arctic Circle and returning cold, dense water back to the tropics. Nearshore areas off Greenland are critical sites in AMOC, influencing the redistribution of heat and nutrients around the world.

The continental shelf along Greenland’s coast is marked by deep grooves called glacial troughs that extend from the mouths of glacially carved fjords to the open ocean. Research in Antarctica suggests glacial troughs there enhance the mixing of cold and warm waters, but few observations have been collected to determine whether the same is true of Greenland’s troughs.

Aboard R/V Neil Armstrong in late summer 2022, as part of an Overturning in the Subpolar North Atlantic Program cruise funded by the National Science Foundation, Nelson et al. explored how troughs influence ocean circulation around Greenland. They collected data in southwestern Greenland at the Narsaq Trough, which is 30 kilometers wide at its mouth and reaches 600 meters at its deepest point—about 4 times deeper than the average surrounding continental shelf. Gathering measurements along multiple ship tracks allowed the researchers to compare water mass properties in and outside the trough, describe flows in and around it, and estimate the mixing of waters with different temperatures and nutrient concentrations.

The results showed that the Narsaq Trough provides a pathway for warm, salty Atlantic Water to intrude onto the continental shelf and mix with cold, fresh polar waters. Consequently, waters in the trough are fresher, richer in oxygen, less rich in nutrients, and sometimes colder than nearby offshore waters. These changes in water conditions may slightly limit melting of glacial ice in the adjacent fjord. Furthermore, the trough creates subsurface circulation that likely exports the modified water from the trough, which may increase stratification and decrease deepwater formation off the continental shelf.

The study offers new insights into Greenland’s understudied glacial troughs and their role in modulating the climate system, the authors say. They note, however, that more work is needed to establish the troughs’ cumulative effects on global ocean circulation. (Journal of Geophysical Research: Oceans, https://doi.org/10.1029/2024JC022246, 2025)

—Aaron Sidder, Science Writer

Citation: Sidder, A. (2025), How Greenland’s glacial troughs influence ocean circulation, Eos, 106, https://doi.org/10.1029/2025EO250205. Published on 29 May 2025. Text © 2025. AGU. 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.

The Late, Great Gaia Helps Reveal Asteroid Masses

EOS - Thu, 05/29/2025 - 13:01

“Everyone benefits from more accurate [orbital tracking] of the asteroids, from missions that are going there to observers on the ground that want to look at them from various telescopes.”

Data from the spacecraft that created the most accurate map of the Milky Way are being used to study objects in our own solar system. Information provided by the European Space Agency’s Gaia satellite have now enabled astronomers to measure the masses of hundreds of asteroids, allowing for improved orbital calculations.

“Everyone benefits from more accurate [orbital tracking] of the asteroids, from missions that are going there to observers on the ground that want to look at them from various telescopes,” said Oscar Fuentes-Muñoz, a NASA postdoctoral fellow at the Jet Propulsion Laboratory in California. Fuentes-Muñoz presented the masses of 231 asteroids he and his colleagues determined using Gaia last month at the Lunar and Planetary Sciences Conference in Houston.

The new research more than doubles the number of known asteroid masses, and the results are only the beginning.

“This work…is really pushing for high precision with novel techniques,” said Kevin Walsh, a solar system dynamicist who studies asteroids at the Southwest Research Institute in Colorado. Walsh was not part of the study.

Gravity Assist Asteroids

The new research relied on a familiar staple of Newtonian physics, taught in high schools everywhere: When two objects interact, each mass exerts a gravitational force on the other. The result is often negligible—the gravitational force of your phone isn’t going to pull you across the room.

But if the objects are moving and the mass difference is large enough, the more massive object will change, or perturb, the path of the less massive one. Fuentes-Muñoz called the phenomenon a “gravitational assist” and compared the relationship between massive and less massive asteroids to the way Earth’s mass perturbs the orbit of a satellite. “The mass of the satellite doesn’t affect the motion of the Earth,” he explained, but the path of the satellite can be dramatically altered.

Although they were not part of its primary mission, the star mapper Gaia was developed with solar system observations in mind and was able to tease out such interactions in incredible detail before being decommissioned in March. According to Gaia team member Mikael Granvik of the University of Helsinki, the telescope’s precision was comparable to observing a 2-euro coin on the Moon while standing on Earth.

As asteroids interacted, Gaia captured how their orbits shifted over 66 months. Fuentes-Muñoz and his colleagues used that information to determine the gravitational mass of the larger objects. Gravitational mass is a way to measure an object’s mass on the basis of how it moves in gravity, rather than calculating the object’s absolute mass in kilograms, for example. This type of measurement is commonly used to estimate the masses of solar system bodies as well as Earth-orbiting satellites and spacecraft.

Most of the 1.4 million known asteroids are too small to have their masses measured, however. “We can estimate things that are maybe…a thousand times smaller than Ceres, but not a million times,” Fuentes-Muñoz said.

Of the more than 1,000 large asteroids they observed, the researchers were able to more precisely calculate the gravitational masses of nearly 300 previously discovered objects. This calculation significantly increases the precision of asteroid orbits.

The dwarf planet Ceres is the largest object in the asteroid belt, and Fuentes-Muñoz calculated its gravitational mass, providing “ground truth” to previous measurements. The new research puts Ceres’s gravitational mass at 62.650 cubic kilometers per square second, which closely matches previous estimates and demonstrates the accuracy of the researchers’ technique. (For comparison, Earth’s gravitational mass is 398,600 cubic kilometers per square second.)

Gaia Is the Gift That Keeps Giving

Gaia wrapped up its mission after more than a decade in space, but new results continue to pour in. That’s due in part to the strict scrutiny the Gaia team uses before releasing data publicly.

Fuentes-Muñoz used the focus product release (FPR), sort of a halfway step between Gaia’s data release (DR) 3, released in 2022, and DR4. DR4 will be released no sooner than this summer, and DR5 won’t be released before the end of 2030.

“It was interesting to see that they got so many accurate masses already from just the FPR,” said Granvik, who reported the first observations of asteroid mass using Gaia in 2022.

“It’s a significant change overall. We’re going to get hundreds of asteroid masses.”

Granvik said Gaia will eventually provide “up to a tenfold increase in the sheer number of objects that we have masses” for.

Walsh said increased precision “will just really help nail down masses and the perturbative effects down to smaller and smaller asteroids.”

“It’s a significant change overall,” Fuentes-Muñoz said. “We’re going to get hundreds of asteroid masses.”

—Nola Taylor Tillman (@astrowriter.bsky.social), Science Writer

Citation: Tillman, N. T. (2025), The late, great Gaia helps reveal asteroid masses, Eos, 106, https://doi.org/10.1029/2025EO250204. Published on 29 May 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.

Keeping Soil Healthy: Why It Matters and How Science Can Help

EOS - Thu, 05/29/2025 - 12:00
Editors’ Vox is a blog from AGU’s Publications Department.

Healthy soils are vital for sustaining life on Earth. They are essential for ecosystems, agricultural production, and clean water, and even help to regulate climate.

A new article in Reviews of Geophysics explores the latest scientific methods for monitoring soil health, including innovative tools like digital twins and satellite-enabled programs, while highlighting persistent gaps in linking indicators to soil functions across scales. Here, we asked the authors to give an overview of the topic.

What is soil health, and how is it different from soil quality?

A healthy soil is a thriving ecosystem: it feeds plants, filters water, stores carbon, and supports worms, microbes, and other tiny lifeforms.

Think of soil health as the soil’s ability to “stay alive” and do its job. A healthy soil is a thriving ecosystem: it feeds plants, filters water, stores carbon, and supports worms, microbes, and other tiny lifeforms. Soil quality, on the other hand, usually refers to how good soil is for growing crops. Soil health is the bigger picture—it’s about keeping soil thriving not just for farms, but for nature and our planet.

Why does soil health matter?

Healthy soil is a multifunctional linchpin of terrestrial ecosystems. It secures food production by nurturing crops, acts as a natural water filter by retaining pollutants, and serves as a massive carbon sink, sequestering atmospheric CO₂ to mitigate climate change—a process monitored at continental scale through EU’s initiatives such as LUCAS, which tracks soil carbon through satellite and field data. Simultaneously, it harbors diverse subterranean communities, from bacteria to earthworms, that drive nutrient cycling and enhance ecosystem resilience against droughts, floods, and pathogens.

How do we measure soil health?

Scientists assess three core dimensions:

  1. Physical properties: Structure (e.g., root penetration, water retention).
  2. Chemical properties: Nutrient availability and pH balance.
  3. Biological properties: Microbial and macrofaunal activity (e.g., decomposition rates).

Emerging tools, such as satellite spectral imaging and AI-driven digital twins, integrate landscape-scale data (e.g., erosion patterns, vegetation cover) to contextualize field measurements. However, challenges persist in scaling microscale processes (e.g., nutrient cycling) to predict landscape-level outcomes.

Why are soil microbes so important?

Soil microbial communities (bacteria, fungi, archaea) are indispensable biogeochemical agents. They decompose organic matter, recycle nutrients, and secrete substances that stabilize soil aggregates, reducing erosion. Microbial communities also suppress plant pathogens and form symbiotic relationships with roots, enhancing crop resilience. Their absence leads to soil degradation, compromising biophysical integrity and triggering cascading declines in ecosystem functionality.

How does water affect soil health?

Water is the lifeblood of soil ecosystems.

Water is the lifeblood of soil ecosystems. Optimal moisture sustains plant hydration and microbial activity. Excess water, however, induces hypoxia, impairing root respiration and promoting anaerobic processes like methanogenesis. Prolonged drought destabilizes soil structure, increasing erosion risks. Healthy soils counteract these extremes through stable aggregates and organic matter, acting like sponges to store water during droughts and absorb rainfall during floods.

Can satellites truly monitor soil health?

Yes. Programs like the EU’s LUCAS integrate satellite data (e.g., Copernicus Sentinel-2’s multispectral imaging for organic carbon) with ground surveys—more than 100,000 soil samples collected between 2009 and 2022 for physical, chemical, and biological analysis. This hybrid approach identifies degraded zones, evaluates restoration efforts, and scales localized data (e.g., nutrient cycles) to landscape processes. These datasets also feed into digital twins, enabling predictive models that inform policies like the EU Soil Monitoring Law.

What’s a “digital twin” for the soil-plant system?

A digital twin is a dynamic, computer-based replica of a physical system – in this case, the soil-plant-environment continuum. It simulates critical processes like water, nutrient, and energy flows (e.g., using models like STEMMUS-SCOPE) and continuously improves its accuracy by assimilating real-time sensor data. This creates a virtual laboratory where we can test responses to challenges like drought or pollution without risking real ecosystems. While the concept originated in aerospace, digital twins now drive major initiatives like the EU’s Destination Earth for modeling climate extremes. Leveraging recent advances in AI and satellite data, we can now perform continent-scale soil health monitoring and scenario modeling, optimizing and transforming land management practices.

What critical gaps remain in our understanding of soil health?

Safeguarding soil health is not just an ecological imperative but a cornerstone of humanity’s future.

Key unknowns include feedback loops between soil structure and microbial communities, scaling microscale processes (e.g., nutrient cycling) to landscapes, and predicting climate impacts on soil carbon and microbial symbioses. Practical hurdles include fragmented global datasets, limited integration of microbial traits in models, and cost-effective tools for farmers. Collaborative platforms like the EU Soil Observatory bridge research and policy, but challenges like modeling root-water-nutrient dynamics in heterogeneous soils or fusing satellite-ground data persist. Addressing these gaps requires interdisciplinary innovation—an urgent task, as safeguarding soil health is not just an ecological imperative but a cornerstone of humanity’s future.

—Yijian Zeng (y.zeng@utwente.nl, 0000-0002-2166-5314), University of Twente, Enschede, The Netherlands; and Bob Su (0000-0003-2096-1733), University of Twente, Enschede, The Netherlands

Editor’s Note: It is the policy of AGU Publications to invite the authors of articles published in Reviews of Geophysics to write a summary for Eos Editors’ Vox.

Citation: Zeng, Y., and B. Su (2025), Keeping soil healthy: why it matters and how science can help, Eos, 106, https://doi.org/10.1029/2025EO255016. Published on 29 May 2025. This article does not represent the opinion of AGU, Eos, or any of its affiliates. It is solely the opinion of the author(s). 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.

The 28 May 2025 catastrophic failure of the Birch Glacier and the partial burial of Blatten

EOS - Thu, 05/29/2025 - 05:58

The Landslide Blog is written by Dave Petley, who is widely recognized as a world leader in the study and management of landslides.

Over the course of the last few days, I have been blogging about the evolving situation on the slopes above Blatten in Switzerland. I documented that attention slowly transitioned from worries about the stability of the slope on Kleine Nesthorn (Petit Nesthorn in French) to concerns about the stability of the Birch Glacier due to increased loading from the rockslide debris. Yesterday, I outlined three scenarios and emphasised that we were in unknown territory.

On 28 May 2025, the Birch Glacier catastrophically collapsed, generating the massive landslide that had been the source of concern. The move by the authorities to evacuate the village proved to be the correct call, but tragically a 64 year old resident appears to have been buried in the landslide. Assuming that he was indeed in the area, their prospects are bleak.

Others have covered the failure event better that can I, and once again I recommend two Bluesky accounts that have provided amazing insights. First, there is Melaine Le Roy, who has posted this for example:-

https://bsky.app/profile/subfossilguy.bsky.social/post/3lqaup44u6k2l

And second is Jan Beutel, who is new to Bluesky (a well timed introduction, sir!), who has posted this before and after comparison that is simply awesome:-

Birchgletscher collapse, before and after.

Jan Beutel (@janbeutel.bsky.social) 2025-05-28T15:29:58.028Z

These two scientists will be really good sources of information over the coming days. Reuters also has a nice summary news video of the events:-

So, was the final collapse my scenario 1 (a further failure of Kleine Nesthorn that triggered failure of the Birch Glacier) or scenario 2 (a catastrophic failure of the glacier itself)? At this stage, I am not sure. The seismic data will reveal all in due course – this event will have been extremely well captured in this dataset. Jan Beutel posted seismic record soon after the failure – look at the scale of the signal that the landslide generated:-

What an inaugural post on bsky.app. A (the) major glacier collapse at Bichgletscher/Kleines Nesthorn.

Jan Beutel (@janbeutel.bsky.social) 2025-05-28T13:43:41.174Z

I am certainly no expert in analysing this data, so I can only speculate, but it is interesting that there was an elevated signal in the two minutes or so before the catastrophic failure began. What was this? Was movement starting to occur in the Birch Glacier, or was there an event on the slope above (or am I misreading the signal)?

So, for now, attention will focus on three things:

First, the valley of the Lonza river is dammed and a substantial lake is starting to develop. This has the potential to inundate the remaining properties in Blatten and, of course, to release a major flood. Two further communities downstream have been evacuated. There is a good Youtube video of this situation:

This will need to be addressed with urgency, but Switzerland is well placed in terms of expertise and resource to mitigate the threat.

Second, attention will need to be paid to the Birch Glacier and the slopes on the Kleine Nesthorn. Is there the potential for a further failure? Massive though this collapse has been, it is unlikely to have included all of the mass on the slope. What is the state of the remaining material? This will be a critical question in terms of the safety of those charged with managing the flood hazard.

And finally, many people have lost their homes, and more may do so in the coming days. This is a devastating event for them, and they will need considerable help.

As a final comment, I have to pay tribute to those individuals who have managed this hazard. The situation was immensely unpredictable, but they acted quickly and decisively. Whilst it is a tragedy that someone is missing, their actions saved many lives.

In due course, I’m sure that there will be a series of papers about this remarkable event. There are many lessons to be learnt from an absolutely amazing case study. As always, please remember that my posts here are provisional and speculative – the definitive analyses comes from the on site experts and from rigorous scientific study in due course.

Return to The Landslide Blog homepage Text © 2023. 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.

El Niño and La Niña transitions affect tropical cyclone development half a world away

Phys.org: Earth science - Wed, 05/28/2025 - 19:30
The butterfly effect suggests that small changes in a system can have a large impact on eventual outcomes. One metaphor used to illustrate this concept is a butterfly flapping its wings only to cause a hurricane across the ocean. While meteorologists' current cause-and-effect understanding of weather isn't this granular, researchers are actively investigating how changes in temperature, rainfall, wind patterns, etc. can impact weather phenomena halfway across the world.

Chinese researchers release Tianshan watershed streamflow dataset

Phys.org: Earth science - Wed, 05/28/2025 - 19:20
A recent study led by Prof. Chen Yaning from the Xinjiang Institute of Ecology and Geography (XIEG) of the Chinese Academy of Sciences has released the Tianshan watershed streamflow (TSWS) dataset (1901–2019). The dataset compiles daily streamflow data for 56 watersheds and monthly data for 89 watersheds in the Tianshan Mountains.

Pollution from the Tijuana river affects air quality in San Diego, finds study

Phys.org: Earth science - Wed, 05/28/2025 - 18:00
The 120-mile Tijuana River flows from Baja California into the United States and discharges millions of gallons of wastewater—including sewage, industrial waste and runoff—into the Pacific Ocean every day, making it the dominant source of coastal pollution in the region.

Underground water channels preserve ancient climate records in their shape

Phys.org: Earth science - Wed, 05/28/2025 - 16:56
Water reshapes Earth through slow, powerful erosion, carving intricate landscapes like caves and pinnacles in soluble rocks such as limestone. An international team from the Faculty of Physics at the University of Warsaw, the University of Florida, and the Institute of Earth Sciences in Orléans has discovered that vertical channels, known as karstic solution pipes, preserve a record of Earth's climatic history.

Water density shifts can drive rapid changes in AMOC strength

Phys.org: Earth science - Wed, 05/28/2025 - 16:28
In the Atlantic Ocean, a system of currents carries vast amounts of warm, salty surface water northward. As this water reaches higher latitudes and becomes colder, it sinks and joins a deep, southward return flow. This cycle, known as the Atlantic Meridional Overturning Circulation (AMOC), plays an important role in Earth's climate as it redistributes heat, nutrients, and carbon through the ocean.

Why slower-sinking microorganisms are bad news for the climate

Phys.org: Earth science - Wed, 05/28/2025 - 14:16
Organic particles that settle on the seabed ensure CO2 stays locked. However, natural gel-like substances slow down this process. Such microscale mechanisms play a crucial role in enhancing climate predictions.

Groundwater is rapidly declining in the Colorado River Basin, satellite data show

Phys.org: Earth science - Wed, 05/28/2025 - 13:55
As the Colorado River's giant reservoirs have declined during the last two decades, even larger amounts of water have been pumped and drained from underground, according to new research based on data from NASA satellites.

As Climate Changes, So Do Gardens Across the United States

EOS - Wed, 05/28/2025 - 13:44

Pine Hollow Arboretum’s founder, John W. Abbuhl, began planting trees around his Albany, N.Y., home in the 1960s. He planted species native to surrounding ecosystems but also made ambitious choices—bald cypresses, magnolias, pawpaws, sweetgums—that were more climatically suited to the southeastern United States.

Now, those very trees are thriving, said Dave Plummer, a horticulturalist at Pine Hollow. 

Other Pine Hollow trees, such as balsam firs native to New York, have struggled with this century’s warming winters. “We’re noticing they’re not doing as well as they were maybe 5 to 10 years ago,” Plummer said. “These are trees that are just meant to be in more northern climates where the winters are harsher, and we just don’t have those winters [anymore].”

Pine Hollow Arboretum is one of many botanical gardens rethinking their planting strategies as the climate warms. These strategies range from testing out new, warmth-loving plants to putting more resources toward pest and invasive species management. 

Planting Zones Shift North

The U.S. Department of Agriculture recognizes 13 plant hardiness zones based on a region’s coldest annual temperatures, averaged over a period of 30 years. These zones guide gardeners’ planting decisions by advising which species of plants, especially perennials, are most likely to thrive in a specific zone.

A new report from Climate Central, a climate change research and communication nonprofit, lays out stark changes to these zones.

Scientists compared 30-year coldest temperature averages from the past (1951–1980) and present (1995–2024) at 247 locations across the United States using NOAA’s Applied Climate Information System dataset. They found that 67% of locations have shifted to warmer zones since the 1951–1980 period.

“The effects of a changing climate on plants and plant communities will be significant and, unfortunately, without precedent.”

They also used the most recently released phase of the Coupled Model Intercomparison Project (CMIP) to simulate how planting zones might shift by mid-century. In the CMIP6 scenario they used, carbon emissions decline but do not stay under Paris Agreement limits, a framework consistent with the Shared Socioeconomic Pathway 2-4.5 “middle of the road” scenario.

The models predict that the mid-century average annual coldest temperatures during the 2036–2065 time period will warm in 100% of the country by an average of 3.1°C (5.6°F). Coldest annual temperatures in the Upper Midwest, Alaska, the Northern Rockies and Plains, and the Northeast and Ohio Valley were projected to warm the most. 

Plant hardiness zones have shifted northward in much of the United States. Credit: Climate Central Longer Seasons, Looming Threats

The results match what staff at Pine Hollow and Mount Auburn Cemetery in Cambridge, Mass., have seen. At the cemetery (which is also a botanical garden), staff have begun to test whether plants that traditionally couldn’t survive cold Massachusetts winters can now thrive. For example, staff there have begun testing crepe myrtles and paperbush, two flowering shrubs that have survived recent winters.

Staff at the Mount Auburn Cemetery in Cambridge, Mass., have tested various plants’ tolerances for warming winters, including this crepe myrtle. Credit: Mount Auburn Cemetery/Jessica Bussman

In Minnesota, plant hardiness zones have shifted by about half a zone since 1951–1980.

Laura Irish-Hanson, an educator and horticulturist at the University of Minnesota, tells students and local gardeners to pay attention to the hardiness map when shopping for perennials and to consider planting species more adapted to warmer climates. “Don’t just look at things that, 200-300 years ago, were native to Minnesota,” she said. “Try things that, historically, maybe are native to Iowa, or Illinois, or parts of Wisconsin that are warmer.”

Mount Auburn is also taking the long view. “The effects of a changing climate on plants and plant communities will be significant and, unfortunately, without precedent,” said Ronnit Bendavid-Val, vice president of horticulture and landscape at Mount Auburn Cemetery, in an email. “We can make informed guesses about a certain plant’s resiliency and toughness based on what is known about its adaptability to extremes in the habitats where its species evolved over millennia. However, horticulturally speaking, ‘plant hardiness’ and fitness can be a vexing subject.”

Anchorage, Alaska, is among the cities that have experienced the largest increase in average annual coldest temperatures, according to the Climate Central report, jumping from −29.8°C (−21.6°F) during 1951–1980 to −24.8°C (−12.6°F) during 1995–2024. 

At the Alaska Botanical Garden in Anchorage, hardiness zone changes aren’t the sole climate consequence affecting plants. Will Criner has been gardening there for 12 years as the garden and facilities manager. In that time, he’s noticed the growing season lengthen and, in turn, the time between the first and last frosts dwindle. “We’re definitely seeing a season extension,” he said. 

“We can be so frustrated, but then [we should] think of it as an opportunity to try something else, to do something new with that space, and not try to fight with the environment.”

While warming temperatures could expand growing ranges for some specialty, high-value crops like oranges, almonds, and kiwis, they could also expand the ranges of pests. In Alaska, for instance, warmer winters have made it easier for the spruce beetle, a native insect capable of decimating entire tree stands, to thrive, Criner said. And Plummer expects that the spotted lanternfly, an invasive species that threatens fruit and hardwood trees in particular, will become a problem in Albany as its range expands northward. 

Warmer temperatures may also make it easier for invasive plant species to establish themselves because they would be able to spread their seeds earlier in the year. Non-native species planted intentionally in gardens may more easily grow out of control, too.

Such non-native species could outcompete other garden plants for water, sunlight, and nutrients, forcing gardeners to change their planting strategies. “I could imagine, as we get longer seasons, that some of these [non-native] plants would have to be removed from our database and deaccessioned” for other plants to thrive, Criner said.

Planting for Precipitation

As the climate warms, gardeners and horticulturists across the country have begun to think about how to better protect their plots. 

In the Midwest, gardeners increasingly face oscillating weather conditions—extreme drought and extreme flooding—that can damage and drown plants. That makes gardening even more of a challenge, Irish-Hanson said. For areas facing intensifying rainstorms, water-loving plants can help mitigate damage to a garden, she said, but they must be planted in low-lying spots to receive adequate water.

These bald cypresses, historically adapted to humid climates of the southeastern United States, have thrived at Pine Hollow Arboretum in Albany, N.Y., for years. The tree to the left, toppled in a March 2024 ice and wind storm, was a white pine, a species indigenous to the region. Credit: Dave Plummer

Plummer, who grew up in Albany, said he’s seen less snow and more ice and wind storms than when he was a child. Those storms can damage plants—a March 2024 ice and wind storm at Pine Hollow Arboretum felled multiple trees, which harmed other specimens. Moving forward, the facility may begin planting species more suited to a warmer climate.

Irish-Hanson recommends gardeners adapt their mindset along with their planting decisions. “Even if we do everything perfectly right and choose the right plant for our environment, it can still die,” she said. “We can be so frustrated, but then [we should] think of it as an opportunity to try something else, to do something new with that space, and not try to fight with the environment.”

Criner has similar advice: “[We should] try to be mindful of the plant choices we make and how plants interact with the surrounding environment, not just if they look pretty or not.”

—Grace van Deelen (@gvd.bsky.social), Staff Writer

Citation: van Deelen, G. (2025), As climate changes, so do gardens across the United States, Eos, 106, https://doi.org/10.1029/2025EO250203. Published on 28 May 2025. Text © 2025. AGU. 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.

Water Density Shifts Can Drive Rapid Changes in AMOC Strength

EOS - Wed, 05/28/2025 - 13:43
Source: Geophysical Research Letters

In the Atlantic Ocean, a system of currents carries vast amounts of warm, salty surface water northward. As this water reaches higher latitudes and becomes colder, it sinks and joins a deep, southward return flow. This cycle, known as the Atlantic Meridional Overturning Circulation (AMOC), plays an important role in Earth’s climate as it redistributes heat, nutrients, and carbon through the ocean.

Although scientists know that the strength of the AMOC—meaning how much water it transports—can vary over time and across regions, it has been unclear how changes in AMOC strength at high northern latitudes may or may not be linked to changes farther south.

Petit et al. applied high-resolution climate modeling to uncover connections between AMOC variability at the midlatitude of 45°N and the current’s behavior at higher subpolar latitudes. High-latitude AMOC observations used in the modeling were captured by the Overturning in the Subpolar North Atlantic Program (OSNAP) instrument array, a network of moorings and submersibles deployed across the Labrador Sea between Greenland and Scotland.

The researchers discovered that subpolar AMOC strength, as captured by OSNAP data, does not affect midlatitude AMOC strength. However, they did find that the density of the subpolar AMOC water beginning its journey back southward affected subsequent midlatitude AMOC strength.

Changes in the water’s density at high latitudes appear to be driven by changes in atmospheric pressure that affect wind stress and buoyancy at the sea surface. The team’s analysis indicates that within a time span of 1 year, these subpolar density changes propagate southward along the far western side of the North Atlantic, creating a steeper density gradient at midlatitudes and, ultimately, affecting AMOC strength there.

The findings suggest that OSNAP density measurements could be used to monitor midlatitude AMOC strength. The study’s results could also help inform the design of future ocean-observing systems to deepen understanding of the ocean’s role in Earth’s climate, according to the researchers. (Geophysical Research Letters, https://doi.org/10.1029/2025GL115171, 2025)

—Sarah Stanley, Science Writer

Citation: Stanley, S. (2025), Water density shifts can drive rapid changes in AMOC strength, Eos, 106, https://doi.org/10.1029/2025EO250202. Published on 28 May 2025. Text © 2025. AGU. 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.

Ion-beam plasma interaction in ion fast ignition nuclear fusion scheme: A systematic study of the hot-spot properties and gains

Physical Review E (Plasma physics) - Wed, 05/28/2025 - 10:00

Author(s): P. Rodríguez-Beltrán, J. M. Gil, R. Rodríguez, and G. Espinosa-Vivas

Ion fast ignition by laser-driven ion beams is an interesting approach within the inertial confinement fusion scheme to achieve nuclear fusion. In the ion fast ignition, once the precompression of the target is finished, a sphere of fully ionized deuterium-tritium (DT) is obtained. In this work, we …


[Phys. Rev. E 111, 055206] Published Wed May 28, 2025

The 28 May 2025 update on the landslide threatening Blatten in Switzerland

EOS - Wed, 05/28/2025 - 05:41

The Landslide Blog is written by Dave Petley, who is widely recognized as a world leader in the study and management of landslides.

Over the last 24 hours there have been further developments in the situation on the slopes above Blatten in Switzerland, with attention continuing to focus primarily on the Birch Glacier.

Yesterday evening (27 May 2025), the largest collapse to date occurred at the front of the glacier – as a reminder, this is currently moving at about 10 metres per day as a result of the loading, estimated at 9 millions tonnes, from the rockslide debris. The toe of the glacier abuts a steep slope, so these movements render it inevitable that collapses will occur.

There is a wonderful set of drone footage of the situation that has been posted to Youtube by Pomona Media:-

This still, from the Pomona Media video, captures the situation beautifully:-

The current situation on the Birch Glacier at Blatten. Note the rockslide in the background, the huge volume of debris on the ice at the bottom of this slope, the ice of the glacier itself and the steep lower slope down which collapses are occurring. Still from a drone video posted to Youtube by Pomona Media.

The active rock slope is very clearly visible in the background, with some dust from ongoing collapses. The huge volume of debris sitting on the glacier is evident in the middle of the image, with the ice of the mobile glacier in the foreground, above the steep lower slope.

The start of the video, which captures a small collapse, also shows the heavy fracturing in the ice:-

The current situation on the Birch Glacier at Blatten, showing the heavy fracturing in the ice of the Birch Glacier. Still from a drone video posted to Youtube by Pomona Media.

RTS has a nice article reviewing the situation. This includes a video that captures one of the major collapses of the front of the glacier – it is rather spectacular.

There are probably three central scenarios at this point (to be clear, this is my interpretation, not that of the team on-site), although of course reality is rather more messy that this in general:-

  1. A further major collapse from the Kleine Nesthorn mobilises the debris on the glacier, and the glacier itself, to generate a major flow. This is probably the worst case scenario, but the likelihood looks to be lower than it was a week ago.
  2. The glacier itself collapses, creating a rock and ice avalanche, which cascades down the slope. This would be a major event, but would have the advantage of removing the hazard. There would be a risk to some of the houses in Blatten.
  3. There are continued smaller (although not trivial) collapses of the front of the glacier. This could continue for some time until a new equilibrium is reached. This is the scenario that leads to the lowest probability of damage, but it is also means that the risk to the village lasts longer.

I have no means to assess the likelihood of each of the above (and there will be other scenarios in play), but for me (based purely on experience) the most likely at this point is scenario 3.

At the time of writing, it is beautiful morning at Blatten, so the webcam is capturing good images.

As always, it is easy to fixate on the natural processes occurring above Blatten, but this is a very human story too. The population of the village is displaced indefinitely, with the possibility of losing their houses to the disaster. Fortunately, domestic property insurance in Switzerland includes a natural perils pool, so losses to a landslide are likely to be covered (this would not be the case in the UK). This will be of little comfort right now.

But, secondly, the expert team monitoring the slope will also be under immense pressure. They will be getting little sleep at the moment. They are under intense scrutiny, but are also working with many unknowns. No matter how good their data is, it will not be sufficient to accurately anticipate what is going to happen next.

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An experiment on earthquake size distribution estimations reveals unexpected large epistemic uncertainty across methods

Geophysical Journal International - Wed, 05/28/2025 - 00:00
AbstractThe earthquake size distribution is well described by the Gutenberg Richter Law, controlled by the b-value parameter. In recent decades, a great variety of methods for estimating the b-value have been proposed by the scientific community, despite the simplicity of this relationship. All these methods underlie the different views of individual modelers and, therefore, often generate inconsistent results. In this study, we perform a seismological experiment in which we compare different, commonly adopted, methodologies, to estimate the completeness magnitude and the b-value, for seismicity in Central Italy. The inter-method differences are on average equal to 0.4 and 0.3, for Mc and b, respectively, but reach much larger values, especially during more intense seismic activity. This shows that epistemic uncertainty in the b-value plays a more crucial role than intra-method uncertainties, opening new perspectives in the interpretation of discrepant, single studies.

Predicting underwater landslides before they strike

Phys.org: Earth science - Tue, 05/27/2025 - 20:51
Below ocean wind farms, oil rigs and other offshore installations are mammoth networks of underwater structures, including pipelines, anchors, risers and cables, that are essential to harnessing the energy source. But much like terrestrial structures, these subsea constructions are also vulnerable to natural events, like submarine landslides, that can hamper the productivity of installations below the sea.

Robotic floats quantify sinking carbon in the Southern Ocean

Phys.org: Earth science - Tue, 05/27/2025 - 17:00
Marine life plays a pivotal role in Earth's carbon cycle. Phytoplankton at the base of the aquatic food web take up carbon dioxide from the atmosphere, convert it to organic carbon, and move it around as they become food for other organisms. Much of this carbon eventually returns to the atmosphere, but some ends up sequestered in the deep ocean via a process called carbon export.

Scientists develop AI model to enhance seasonal Arctic sea ice prediction

Phys.org: Earth science - Tue, 05/27/2025 - 16:24
Predicting the extent of Arctic sea ice in September has significant implications for climate change and shipping in the Arctic. However, seasonal forecasts for September sea ice often encounter a challenge known as the "spring predictability barrier."

Rising soil nitrous acid emissions driven by climate change and fertilization accelerate global ozone pollution: Study

Phys.org: Earth science - Tue, 05/27/2025 - 14:04
Ozone pollution is a global environmental concern that not only threatens human health and crop production, but also worsens global warming. While the formation of ozone is often attributed to anthropogenic pollutants, soil emissions are revealed to be another important source.

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