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Trump’s Science Adviser Wants to Overhaul “Increasingly Calcified” U.S. Science Enterprise While Science Funding Lags

Thu, 07/23/2026 - 15:05
body {background-color: #D2D1D5;} Research & Developments is a blog for brief updates that provide context for the flurry of news regarding law and policy changes that impact science and scientists today.

23 July: This article was updated to include comments from Jennifer Jones and Colette Delawalla.

A report released this week directs the U.S. government to spark a “new golden age” of science by ushering funds toward artificial intelligence, fostering closer relationships with private industry, and dismantling and rebuilding the federal science funding process.

The report was written by Michael Kratsios, director of the White House Office of Science and Technology Policy. He outlined his recommendations to Congress at a hearing of the House Committee on Science, Space, and Technology on 22 July. 

Kratsios intended the report to emulate a letter written to President Franklin D. Roosevelt by Vannevar Bush in 1945, called Science, the Endless Frontier, which set the foundation for the current U.S. federal science process in which federal funds support university research. “As we celebrate the United States’ 250th anniversary, we have the responsibility to renew our foundations once more,” he wrote.

Kratsios listed four goals to guide this approach to U.S. science: to “prioritize the individual scientist over legacy institutions,” to “fundamentally change how research dollars are allocated, distributed, and assessed,” to “set clear scientific goals and build the industrial muscle to translate scientific discovery into technological strength,” and to “prepare our research enterprise for the AI revolution.”

“If you think about this report in the context of everything else this administration has done, it really is about weakening independence, weakening accountability, [and removing] scientific integrity protections in favor of empowering political appointees,” said Jennifer Jones, director of the Center for Science and Democracy at the Union of Concerned Scientists.

Science-A-New-Golden-Age_EosDownload

The report recommends a handful of federal priorities to achieve these goals, including the Genesis Mission, a “national effort to harness AI for scientific discovery at a scale no other nation can match” led by the Department of Energy (DOE).

At the 22 July hearing, Kratsios said the Genesis Mission “is the crown jewel of American AI for science” and announced that federal agencies have committed more than $5 billion to the project. So far, 278 awards have been made, the largest being a three-year, $60 million grant for a project that will “help deliver nuclear facilities faster and safer” with the use of AI, according to the DOE. 

“There’s no mention of scientific integrity, no mention of protections for independence, it’s just the opposite.”

“There are some examples in STEM where AI is valuable,” such as increasing power in computational modeling or identifying new Earth-like planets at scale, for example, wrote Colette Delawalla, founder of science advocacy group Stand Up for Science, in an email. “But AI will never replace curiosity-driven scientific advancement,” she wrote. 

Some scientists viewed the report as a way for the government to justify steering research funds toward private industry and increasing political interference in science. “I think they’re trying to turn it into a venture capital model,” Jeremy M. Berg, a computational biologist and former director of the National Institute of General Medical Sciences at the National Institutes of Health, told The New York Times

“Under the hood,” the report is a “vision for faster technology development and commercialization while underinvesting in the fundamental research, expert peer review, and scientific workforce that make those advances possible,” Keivan Stassun, an astrophysicist and member of the National Science Board prior to its dissolution by the Trump administration, told Science.

What’s interesting about the report, Jones said, is what it doesn’t mention. “There’s no mention of scientific integrity, no mention of protections for independence, it’s just the opposite,” she said. “There are no clear systems of accountability” explained in the report, and its suggestion to funnel funds to individual researchers rather than institutions such as universities also means more research could occur outside of universities’ established and robust systems of accountability, she added.

The recommendations in the document largely align with recommendations made by former National Academy of Sciences president Marcia McNutt in June. In the annual president’s address, McNutt encouraged the scientific community to “better understand the needs of industry” and embrace the use of AI to increase research efficiency. 

At the hearing, however, Kratsios agreed with Rep. Brian Babin (R-TX), chair of the committee, that the National Academies of Science, Engineering, and Medicine required more federal oversight, especially in light of its recent report on climate attribution science that Babin said raised “transparency concerns.” Kratsios said he looked forward to working with Congress to codify the recommendations made in the “new golden age” report.

Funding the Golden Age

The vision the report presents is accompanied by recommendations from Kratsios and Russell Vought, director of the Office of Management and Budget, for the FY 2028 budget. These recommendations include prioritizing funding for physical sciences, including quantum physics, chemistry and materials sciences, mathematics and computer sciences, engineering, and biological sciences. 

For FY 2028, “agencies should align their R&D investments, where appropriate, with the Administration’s national missions,” the report states, listing those “national missions” as AI, quantum computing, fusion power, the construction of a lunar base and return of humans to the Moon, autonomous robotics, and semiconductor technology. 

 
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At the 22 July hearing, Democrats argued that the Trump administration’s actions have worked against the stated goals of Kratsios’s report. “Big new initiatives and promises mean nothing when agencies act capriciously, canceling grants midway, delaying awards for months, even after they’ve been selected through the rigorous merit review process, and blacklisting educational and research institutions,” said Rep. Zoe Lofgren (D-CA).

The report did not mention the Trump administration’s proposed FY 2027 budget, which, if finalized, would reduce the National Science Foundation’s budget by 53%, the U.S. Geological Survey’s budget by 37%, the NASA science budget by 42%, and NOAA’s budget by 28%.

“I anticipate the report will be used as the rationale for making further cuts in the budgets and staffing of federal research agencies while limiting their authority and accountability to the American people,” Neal Lane, former director of the NSF, told Science

The report also did not mention recent sweeping cuts to the NSF’s FY 2026 budget, the fact that the NSF currently has no director, or a June proposal from the Office of Management and Budget that, if finalized, would give political appointees final approval power for scientific grants.

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

These updates are made possible through information from the scientific community. Do you have a story about how changes in law or policy are affecting scientists or research? Send us a tip at eos@agu.org. Text © 2026. AGU. CC BY-NC-ND 3.0
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Small Faults Add to Seattle’s Quake Story

Thu, 07/23/2026 - 13:09

The winter earthquake of 923 or early 924 CE remains the benchmark event in the Seattle Fault Zone. It lifted shorelines around Puget Sound and gave geologists one of the most decisive records of the fault’s power.

But that shoreline-lifting earthquake is only part of the zone’s history. A recent Geological Society of America Bulletin study led by Stephen J. Angster, a geologist with the U.S. Geological Survey, looks past the most famous Seattle fault earthquake to examine evidence of earthquakes on lesser-known secondary faults.

At Lytle Beach on Bainbridge Island and at Vasa Park near Bellevue, subtle landforms and trench records suggest evidence of smaller ruptures has been preserved in the landscape but not fully recognized.

At Lytle Beach, the first clue was a small, raised surface. Angster described the “localized uplifted terrace” as “the first feature we saw that drew our eye to that area.” Similar features had already helped geologists read other secondary faults in the Seattle Fault Zone.

For instance, Angster said the Toe Jam Hill fault became one of the better-known examples when lidar helped reveal its scarp through dense vegetation. Later work found smaller uplifted terraces near similar secondary structures, which Angster said may indicate separate earthquake events focused on smaller faults rather than the larger regional rupture.

However, Lytle Beach stood out in a different way, as its fault dips south, in contrast to the zone’s better-known secondary faults, which dip north.

Faults Hidden in the Fold

Finding the localized uplifted terrace was only the beginning for Angster, who used lidar to uncover scarps and lineaments through the region’s forest cover.

His team also utilized ground-based magnetic transects across the Lytle Beach fault to look for changes that may reveal displacement beneath the surface. In addition, they gained a more direct view of disturbed sediments by excavating the Rose Hip trench across the newly identified Lytle Beach scarp and analyzing evidence from the earlier Vasa Park trench.

In the Rose Hip trench at Lytle Beach, Angster said the team found glacial deposits dating to roughly 15,000 years ago. Above them were lake sediments left behind as ice retreated. The trench also preserved an old layer of soil that formed after the lake dried. “That whole package was folded,” he said. “The only way you could fold those is mostly by a tectonic fault.”

A regional map of the Seattle Fault Zone shows the Lytle Beach and Vasa Park fault scarps, along with the uplifted shore platform associated with the 923 CE earthquake. A new study used mapping, geophysics, trenching, and dating methods to investigate secondary faults within the broader fault zone. Credit: Angster et al., 2026, https://doi.org/10.1130/B38333.1, CC-BY-4.0

The trench record showed evidence of two surface-rupturing earthquakes on the Lytle Beach fault. The older event occurred between 11,240 and 10,430 calibrated years before present, whereas the younger event occurred after 1663 CE, likely in the early nineteenth century. (“Calibrated years before present” refers to dates arrived at via radiocarbon dating, relative to the year 1950 as the “present.”)

“I thought the trenching on Lytle Beach was surprising, that we found two events, because it was such a relatively subtle feature that wasn’t really identified before,” Angster said.

At Vasa Park, the team found evidence of one past earthquake that occurred sometime between 11,380 and 7,400 calibrated years before present. That range overlaps with the older Lytle Beach event and raises the possibility of a longer rupture along the Blakely Harbor fault. However, the evidence in Angster’s study better supports separate ruptures on the two secondary faults.

A Longer Record of Smaller Ruptures

Harold Tobin, an earthquake scientist at the University of Washington who was not involved in the study, called the work “exciting new research.”

He said the study shows there is “room to accommodate smaller earthquakes” that do not reshape shorelines like the 923 or 924 event but are “still big enough to be damaging earthquakes.” The Angster paper, he said, examines “additional earthquakes not accounted for in the shoreline uplift record centered on the 923 or 924 event. These smaller earthquakes may have happened more recently or more often.”

“Subtle features, relatively small or fault traces that we might have ignored before, can be an important part of the story.”

For Tobin, the value also extends beyond Puget Sound. The study “shines a light for other people working in cities and urbanized settings,” he said, because it shows that “subtle features, relatively small or fault traces that we might have ignored before, can be an important part of the story.”

By comparing the dated events at Lytle Beach, Vasa Park, and other secondary faults, the authors estimated that these faults may have ruptured roughly every few hundred years during the late Holocene. Angster cautioned that it’s not quite clockwork. “The secondary faults appear, especially within the last 2,500 years, to rupture more frequently, and that’s where that 350-year interval comes from,” he said. But the estimate rests on a limited record.

Though the work doesn’t forecast the next earthquake, it gives scientists more of the past to weigh as they assess the Puget Lowland. Tobin said the paper “certainly beg[s] more research” because the Seattle Fault Zone contains many strands that still need to be studied. Earthquake hazards should remain “something real” for the public and civil planners.

“We don’t know when they are going to come,” Tobin said. “Obviously, we can go decades without any significant earthquakes, as we have since 2001. But when we least expect it, one will happen, and we just have to be prepared.”

Angster framed the findings more conservatively: “This study doesn’t really change the hazard with the Seattle Fault. It just provides more insight into how it behaves.”

—Jason Collins, Science Writer

Citation: Collins, J. (2026), Small faults add to Seattle’s quake story, Eos, 107, https://doi.org/10.1029/2026EO260238. Published on 23 July 2026. Text © 2026. 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.

Scientists Might Have Detected the First Moon Outside Our Solar System… It Just Depends How You Define “Moon.”

Wed, 07/22/2026 - 15:01
body {background-color: #D2D1D5;} Research & Developments is a blog for brief updates that provide context for the flurry of news that impacts science and scientists today.

What exactly is a moon? It’s an existential question lunar researchers found themselves pondering when they discovered an exosatellite at least 90% the size of Jupiter, orbiting a brown dwarf in a system about 73 light-years away from Earth.

 
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Depending on how exactly one defines “moon,” the object could be the first moon definitively discovered outside our solar system.

If a moon is a body orbiting another body that is orbiting a star, then yes, we’ve got a moon on our hands. But this exosatellite is orbiting a brown dwarf, a body far larger than most planets but too small to sustain hydrogen fusion as stars do, instead of a planet. And it’s enormous in a way our local moons aren’t.

The whole system is really weird, explained lead author Kevin Hoy in an email to Eos. Hoy is a European Southern Observatory astrophysics Ph.D. student who is also affiliated with the Instituto de Estudios Astrofísicos at the Universidad Diego Portales in Chile and its Millennium Nucleus of Young Exoplanets and their Moons research center.

“The host star is much smaller than the Sun, the brown dwarf is much heavier than our most massive planet, and the satellite is much heavier than any of the moons in our system,” Hoy said. “No part of this system has an obvious comparison to any object in the Solar System.”

The researchers published their findings today in Nature.

When Words Fail

The scientists detected the maybe-moon in the CD-35 2722 system using the radial velocity method, which is often used to detect exoplanets. The brown dwarf moves slightly in response to the exosatellite’s orbit, as the exosatellite exerts a slight gravitational pull. These movements can be seen from Earth as small changes in the brown dwarf’s light spectrum. Scientists observed 26 of these changes from the European Southern Observatory’s Very Large Telescope (VLT) in Chile between October 2023 and February 2026.

The scientists ran several models to see what could explain the periodic changes, including a model in which the brown dwarf actually had two exosatellites. The best explanation to fit the data, they found, was one satellite at least 90% as massive as Jupiter orbiting the brown dwarf approximately every 170 days. (The brown dwarf itself is about 37 times as massive as Jupiter, meaning that although the proposed exomoon is huge, it could be proportionally much less massive compared to its primary than the Moon is to Earth.)

The combination of techniques the researchers used were first proposed for detecting exomoons in 2018, in a paper coauthored by Andrew Vanderburg, now an astronomer at Harvard University.

“I never would have imagined that this technique would reveal such an unusual object!” Vandenburg said in an email to Eos. He added that he wondered what exactly the exosatellite was, how it formed, and how big it was. “Regardless, it’s an amazing discovery and I’m super excited to see what else we can find by observing planets like this!”

Researchers have discovered more than 6,200 confirmed exoplanets so far, but only a few candidates for exomoons have been detected, and none have been confirmed. Such a discovery could help us learn more about how various parts of the universe were formed, and how they function today, the paper suggests.

Though it’s possible some unknown variable in the brown dwarf itself could be responsible for the periodic changes in radial velocity the team observed, “we can’t think of any physical mechanism that could reproduce the signal we see,” said Hoy, the lead author of the study. “That’s why we think a satellite is the most likely explanation.”

In this case, the scientists are confident about what they’ve found. They’re just not sure exactly what to call it.

“Perhaps we are approaching the limit of language invented to describe the Solar System, which is entirely unlike CD-35 2722,” the paper reads.

—Emily Gardner, Deputy Editor (@emfurd.bsky.social)

These updates are made possible through information from the scientific community. Do you have a story about science or scientists? Send us a tip at eos@agu.org. Text © 2026. AGU. CC BY-NC-ND 3.0
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Why Healthy Soils Matter More Than Ever

Wed, 07/22/2026 - 14:19
Editors’ Vox is a blog from AGU’s Publications Department.

Protecting soil health is essential to achieving the United Nations Sustainable Development Goals (SDGs) since it has direct impacts on food and water security, ecosystem health, and socio-economic activities. However, human-induced drivers and pressures heighten the susceptibility of soils to degradation.

A new article in Reviews of Geophysics explores the drivers, impacts, and efforts to combat soil degradation. Here, we asked the authors to give an overview of soil degradation, practices being implemented to combat it, and what questions remain.

What is soil degradation and why is it important to study?

Soil degradation refers to the deterioration of soil quality resulting from unsustainable human activities most commonly associated with agricultural, pastoral, industrial, and urban land use. It involves a dynamic reduction in the physical, chemical, and biological properties of soil that diminishes its structural integrity, functional capacity, and overall resilience over time.

Studying soil degradation is important because it is a major global environmental challenge that threatens soil security, ecosystem services, agricultural productivity, and human well-being. It also makes land more susceptible to droughts, floods, landslides, and climate extremes. Soil degradation often develops gradually and may remain unnoticed until critical thresholds are reached, after which recovery can be extremely slow, costly, or even impossible. Understanding the causes, processes, and consequences of soil degradation is therefore essential for preventing long-term environmental and socio-economic damage and for supporting sustainable land management and ecosystem resilience.

What are the key processes that degrade soil?

The key processes of soil degradation can be grouped into physical, chemical, and biological degradation. Physical degradation includes the breakdown of soil structure, aggregate loss, compaction, reduced porosity and pore connectivity, and erosion caused by water, wind, tillage, or crop harvesting. These processes remove topsoil, nutrients, and organic matter while reducing the capacity of soil to retain water. Chemical degradation includes acidification, alkalization, nutrient depletion or excess nutrient accumulation, loss of soil organic matter and soil organic carbon, salinization, sodicity, and contamination by toxic chemicals or pollutants. Biological degradation involves declines in soil biodiversity, microbial activity, and overall biological functioning. These processes rarely occur independently; rather, they interact and reinforce each other thus increasing the susceptibility of soil to further degradation.

What are the major drivers of soil degradation and how do they differ from perturbations?

The major drivers of soil degradation are long-term natural or anthropogenic forces that initiate or accelerate the physical, chemical, and biological processes of soil degradation. These include deforestation, unsustainable agricultural practices, land-use change, industrial and mining activities, climate change, and overgrazing. These drivers place continuous pressure on the environment and gradually reduce soil functioning. In contrast, perturbations are typically short-term disturbances such as floods, droughts, extreme weather events, wildfires, or sudden land-use changes that temporarily disrupt soil ecosystems and their resilience. The distinction between drivers and perturbations lies primarily in their duration and persistence. When disturbances occur repeatedly or continue over long periods, they can become long-term drivers of degradation.

Drivers and pressures contributing to soil degradation, indicating the complex socio‐economic and environmental interactions that contribute. Credit: Shokri et al. [2026], Figure 1

How do scientists measure soil degradation at different spatial scales?

Scientists quantify soil degradation using complementary approaches across multiple spatial scales. At local or field scales, direct surveys and monitoring quantify physical, chemical, and biological indicators of soil health and degradation. These measurements are supported by expert assessments and land-user knowledge gathered from interviews or questionnaires. Analytical frameworks then combine these indicators to evaluate soil functions and ecosystem services under different land management practices. While field observations provide detailed and localized evidence, they are difficult to scale, require repeated monitoring, and depend on context-specific indicator thresholds.

At regional, national, continental, and global scales, assessments combine bottom-up, top-down, and hybrid methods including expert mapping, soil sampling, modeling, and remote sensing. High-resolution satellite imagery and remote sensing technologies enable continuous, large-scale monitoring of land cover, vegetation dynamics, erosion, soil moisture, and other indicators associated with soil degradation. These assessments are increasingly supported by big data analytics, high-performance computing, and advanced machine learning models that integrate diverse datasets and improve the detection and prediction of degradation patterns.

At the microscopic scale, a wide range of experimental and modeling techniques can be employed to characterize the parameters and processes governing the physical, chemical, and biological properties of soils, thereby providing insights into the mechanisms that contribute to soil degradation.

What are some of the restoration efforts or practices being implemented to combat soil degradation?

Efforts to restore degraded soils range from large-scale policy initiatives to practical land management strategies. At the national level, restoration projects such as China’s rehabilitation program on the Loess Plateau have successfully restored millions of hectares of degraded land. In Europe, international agreements to reduce transboundary air pollution have decreased acid deposition and promoted the recovery of acidified soils.

Global distribution of improved land management and restoration measures as applied in restoration scenarios (van der Esch et al., 2021). Credit: Shokri et al. [2026], Figure 4a

At the field scale, restoration focuses on minimizing further degradation while rebuilding soil health. Reducing vehicle traffic is encouraged to minimize soil disturbance and prevent compaction. Agricultural practices include reduced or no-tillage farming, crop rotation, agroforestry, cover crops, compost and manure application, integrated pest management, and efficient irrigation methods such as drip irrigation and rainwater harvesting. These practices improve soil structure, enhance soil fertility, reduce erosion, increase organic matter, and strengthen the long-term resilience of agricultural soils while supporting sustainable land management.

Why is combating soil degradation essential for achieving the United Nations Sustainable Development Goals?

Combating soil degradation is recognized as a fundamental prerequisite for achieving the United Nations Sustainable Development Goals (SDGs) due to the extensive socio-economic and ecological impacts of soil health. Healthy soils provide natural capital and ecosystem service delivery that directly support human well-being. Preventing soil degradation is essential for ensuring global food security, maintaining agricultural productivity, supporting livelihoods, and reducing hunger and poverty. Furthermore, maintaining soil functionality is strictly necessary for preserving water security, regulating the climate, and supporting overall ecosystem health. Consequently, sustainable soil management contributes directly to several SDGs, including SDG 2 (Zero Hunger), SDG 6 (Clean Water and Sanitation), SDG 13 (Climate Action), and SDG 15 (Life on Land). Failure to combat soil degradation can lead to severe socio-economic consequences such as health crises driven by desert dust storms and widespread human migration, which would completely undermine the environmental resilience demanded by the SDGs.

What are the remaining questions or knowledge gaps where additional research is needed?

Several important knowledge gaps remain in our understanding of soil degradation. One major challenge is the lack of a universally accepted definition of soil degradation. This inconsistency makes it difficult to compare studies and establish standardized indicators and assessment methods. In addition, many global and national assessments are fragmented, outdated, or lack long-term monitoring data.

Global climate simulations help scientists understand how the atmosphere, oceans, and land interact. These high-resolution models improve our ability to study environmental processes and assess how climate may influence soil degradation and ecosystem health. Credit: Shokri et al. [2026], Figure 31

Further research is needed to improve understanding of how multiple drivers interact, how quickly degradation develops, and whether soils can fully recover after pressures are removed. Scientists also need a better understanding of the links between climate, land use, and soil processes, as well as the socio-economic impacts on livelihoods, inequality, and migration. Improving monitoring methods, data sharing, and standardized protocols will help produce more reliable assessments and support more effective soil management and restoration strategies.

—Nima Shokri (nima.shokri@tuhh.de, 0000-0001-6799-4888), Institute of Geo-Hydroinformatics, Hamburg University of Technology, Germany; Mehdi Afshar (0000-0002-4411-3299), Institute of Geo-Hydroinformatics, Hamburg University of Technology, Germany; and Milad Aminzadeh (0000-0002-0074-3600), Institute of Geo-Hydroinformatics, Hamburg University of Technology, Germany

Citation: Shokri, N., M. Afshar, and M. Aminzadeh (2026), Why healthy soils matter more than ever, Eos, 107, https://doi.org/10.1029/2026EO265026. Published on 22 July 2026. 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 © 2026. 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.

Stratospheric Aerosol Injection Might Make Flights Smoother

Wed, 07/22/2026 - 13:14
https://serc.carleton.edu/teachearth/eos-activities.html?url=EOSURL

Stomach-churning dips and swerves can be the most unpleasant—and dangerous—part of flying. To travelers’ chagrin, climate change has already begun to make such aircraft turbulence more common, as it alters the movement of air masses at the heights where planes fly.

Researchers wondered whether stratospheric aerosol injection (SAI), a controversial climate intervention strategy to cool the planet by injecting sunlight-blocking aerosols into the stratosphere, could help. In a study published last month in Environmental Research Letters, a team modeled aircraft turbulence under future climates with and without SAI. The researchers found that climate intervention could, indeed, reduce aircraft turbulence, even below modern-day levels.

“SAI is very important, but on the other hand, it’s very dangerous,” said study author Hye-Yeong Chun, an atmospheric scientist at Yonsei University in Seoul, South Korea. “These results show that aviation turbulence is quite significantly reduced [with SAI]—so this is one merit, at least, on the SAI side.”

A Bumpy Future

Climate change isn’t warming the planet evenly; the poles are heating up faster than the equator. This imbalance shrinks the temperature difference between the rising masses of cool and warm air that meet to form the jet stream, a fast-moving current of air that swirls like a river around the globe near 9,100 meters (30,000 feet) in elevation. The lower temperature difference weakens the jet stream, making it wavier and prone to wind shear, or changes in wind speed or direction over short distances. Because wind shear is one of the primary causes of aircraft turbulence, plane rides are getting bumpier, explained Chun.

“[Turbulence is] a very intermittent and localized phenomenon. Even current weather forecasting models and high-resolution numerical models cannot directly predict turbulence.”

But turbulence is also one of the trickiest weather elements to predict, she said. Unlike turbulence from storms or clouds, which is visible and easier to forecast, so-called clear-air turbulence can’t be seen by pilots. “It’s a very intermittent and localized phenomenon,” said Chun. “Even current weather forecasting models and high-resolution numerical models cannot directly predict turbulence.”

Understanding turbulence and how the jet stream is changing is important “not only for comforting people, but also for reduction of greenhouse emissions,” said Tommaso Alberti, a physicist at Italy’s Istituto Nazionale di Geofisica e Vulcanologia who was not involved with the study. Turbulence can increase a plane’s fuel requirements as it readjusts, while taking advantage of a strong jet stream can shrink flight times and associated carbon emissions.

Since the phenomenon can’t be directly predicted, scientists like Chun use proxies—other measurements that indicate potential regions where turbulence might occur. In the new study, she and her colleagues used a measure called the Ellrod index, which combines data on vertical wind shear and the stretchiness of masses of air.

The researchers modeled how the Ellrod index would change across seven climate futures with varying amounts of greenhouse gas emissions, three of which had no human intervention and four of which had SAI. They found that although climate change should increase aircraft turbulence across nearly all latitudes, SAI could reduce such increases by up to 60%. And to Chun’s surprise, SAI was powerful enough not only to counteract future turbulence but also to reverse modern-day levels of climate-driven turbulence. One possible explanation is that depending on where the aerosols get injected, SAI cools the tropics more strongly than the poles, counteracting the shrinking temperature difference that forces the jet stream out of balance.

Global Tactics, Global Implications

“We have to find the optimal way to reduce temperature but, on the other hand, reduce any potential side effects.”

Though the study results are promising, they are far from a green light to conduct climate intervention, said Chun. Still, the goal set forth in the Paris Agreement of limiting global warming to 2°C above preindustrial levels will not be easy to achieve, she said. “We have to find the optimal way to reduce temperature but, on the other hand, reduce any potential side effects.”

With global climate interventions such as SAI, a top concern is that any side effects will occur throughout the world, ranging from changes in rainfall to disruptions to the ozone layer. The most commonly proposed aerosol, sulfur dioxide, can also cause acid rain as it falls out of the atmosphere.

Ramalingam Saravanan, an atmospheric scientist at Texas A&M University who was not involved with the study, said that researching SAI in “controlled and safe conditions” had its merits. But as a longtime modeler, he said, “There are all kinds of errors in models that we are still working with…saying ‘This is what will happen’ in a model may not exactly be what will happen in the real world.”

In turn, Saravanan worried that private individuals or companies pushing to enact climate intervention might overstate the benefits to airplane turbulence. “Focusing on potential modest benefits of a radical and uncertain mitigation approach, as this study does, risks deflecting attention away from the inherently large dangers of climate intervention,” he clarified in an email.

Alberti noted that artificial intelligence models may eventually be able to forecast clear-air turbulence, providing a less risky solution for dealing with the hazard. However, he noted that would only be a way to adapt to climate-driven turbulence, not mitigate it.

Chun said that she was not yet advocating for the actual implementation of SAI but that researching it is critical if global leaders are to consider such a strategy. AGU’s Ethical Framework Principles for Climate Intervention Research acknowledges that such geoengineering approaches shouldn’t move forward without an internationally agreed-upon ethical governance structure but states that “more knowledge about climate intervention approaches and their consequences will help society make informed, just decisions about the deployment of climate intervention.”

“The risk is quite significant,” Chun said. “Scientists have to work very hard to save lives, to save our planet.”

—Hannah Richter (@hannah-richter.bsky.social), Science Writer

This news article is included in our ENGAGE resource for educators seeking science news for their classroom lessons. Browse all ENGAGE articles, and share with your fellow educators how you integrated the article into an activity in the comments section below.

Citation: Richter, H. (2026), Stratospheric aerosol injection might make flights smoother, Eos, 107, https://doi.org/10.1029/2026EO260237. Published on 22 July 2026. Text © 2026. 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.

Redesigning Farmland Through Community Collaboration in California

Wed, 07/22/2026 - 12:00
Editors’ Highlights are summaries of recent papers by AGU’s journal editors. Source: Community Science

California is experiencing major changes in how farmland is used as recent policies seek to protect groundwater resources. These changes are reshaping both the landscape and the lives of rural residents, especially in communities like Fairmead in Madera County, which is surrounded by water-intensive almond orchards.

In Community Science’s special collection on Transdisciplinary Collaboration for Sustainable Agriculture, Katrak-Adefowora et al. [2026] describe a project that engaged Fairmead residents and farmers in redesigning a small almond farm into a landscape that reflects multiple community priorities. The new landscape includes a basin that captures stormwater to reduce flooding and help replenish groundwater, native plants that improve habitat, and a walking path for community recreational use. Community members and farmers were engaged through workshops, outreach, and educational activities, with the project team remaining flexible and responsive to local input.

This paper shows how involving communities in landscape decisions from the beginning can lead to solutions that are both environmentally beneficial and responsive to local priorities. It also offers a practical collaborative model for other regions facing similar land-use and water challenges, demonstrating how partnerships among residents, farmers, nonprofits, businesses, local governments, and scientists can support more resilient communities.

Citation: Katrak-Adefowora, R., Massell, A., Ortiz, V., Vizcarra, A., Nelson, B., & Fernandez-Bou, A. S. (2026). Community-driven solutions for groundwater resilience in California. Community Science,5, e2025CSJ000167. https://doi.org/10.1029/2025CSJ000167

—Claire F. Beveridge, Editor, Community Science Exchange

Text © 2026. 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.

Fatal landslides in May 2026

Wed, 07/22/2026 - 05:57

In May 2026 I recorded 51 fatal landslides causing 185 fatalities. 2026 is proving to be atypical in terms of the temporal pattern of fatal landslides.

This is my regular update for the number of fatal global landslides, focusing on May 2026. As usual, this data has been collected in line with the methodology described in Froude and Petley (2018) and in Petley (2012). References are listed below – please cite these articles if you use this analysis. Data presented in these updates should be treated as being provisional at this stage as I will reanalyse them prior to formal publication, and other events will emerge.

Note that this data excludes landslides triggered by earthquakes (see below).

The headline figures are as follows:

May 2026: 51 fatal landslides causing 185 fatalities.

This is the monthly number of landslides by month in 2026 to the end of May:-

The number of global fatal landslides in 2026 by month to the end of May.

Last month I noted that 2026 was proving to be atypical in terms of the pattern of fatal landslides. This has continued through May, with the total number recorded in this month being lower than for both February and March. This may indicate that patterns of rainfall this year are different from the norm. More research is needed.

My preferred way of presenting this data us to use the cumulative total by pentad. This graph is to pentad 30, which ends on 30 May:-

The cumulative total number of global fatal landslides in 2026 by pentad to the end of May.

So, to 30 May 2026 the cumulative total number of fatal landslides was very significantly higher than the long term mean and above the exceptional year of 2024. However, note that the cumulative total was very close to the 2024 total – this year did not experience the early acceleration in the rate of cumulative landslides that we saw in 2024.

As always the final annual total will heavily depend upon rainfall patterns in East and South Asia in the northern hemisphere summer months.

Major events included the multiple landslides in Yongchuan, Chongqing, China on 24 May.

The 8 June 2026 M=7.8 earthquake in the Philippines also triggered landslides – to date I have recorded six separate events causing 31 fatalities, but this may be incomplete.

I am now working on the June 2026 data.

References

Froude, M. and Petley, D.N. 2018.  Global fatal landslide occurrence from 2004 to 2016.  Natural Hazards and Earth System Sciences 18, 2161-2181.

Petley, D.N. 2012. Global patterns of loss of life from landslidesGeology 40 (10), 927-930.

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Slums are bearing the brunt of the climate crisis—and devising solutions

Tue, 07/21/2026 - 13:11

This story was originally published by Knowable Magazine.

Reporting for this story was supported by the Pulitzer Center.

Since moving into a public housing project in Mumbai nearly 20 years ago, Parveen Shaikh has grown familiar with the ravages of extreme heat. She has acquired a new vocabulary, adding terms like “low blood pressure”—which she has learned is a consequence of blood vessels dilating to keep the body cool and causes dizziness, vomiting and irritability. “Little kids,” she observes, “get angry faster than they used to.”

Shaikh doesn’t remember low blood pressure being a problem when she was growing up in poverty on the city’s sidewalks, though there were plenty of others. It was a victory of sorts when she moved into her home as part of a government relocation program. But as India’s seasons have become less predictable, and its hot periods hotter, the flaws in the housing project’s construction have become apparent.

There isn’t much space between the tenements here, and many apartments lack natural light and ventilation. The heat, when it arrives, is inescapable, as are its physiological consequences. On the day in late January when I met Shaikh, summer was more than a month away, but a team of medics was already testing people’s blood pressure in the shade of a residential block.

Heat is now a major and growing problem across the Global South. Under the highest emissions trajectory, rising temperatures will cause an additional 6 million deaths per year by 2100, according to estimates from the University of Chicago’s Climate Impact Lab. That’s comparable to today’s annual deaths from infectious diseases. The vast majority of those deaths will happen in the poorest countries, where the most vulnerable of all are those who live or work informally—those who make their homes in slums or on the street, or who are employed in the gig economy.

Indeed, climate change “is already profoundly affecting the lives of poor people worldwide—A, because they live in places that are already hot, and B, because they are not able to protect themselves as well,” the Nobel Prize-winning economist Esther Duflo of the Massachusetts Institute of Technology and the Collège de France told me at the Jaipur Literature Festival in India in January.

Duflo, coauthor of the book Poor Economics, whose second edition addresses climate change, sees a vicious cycle at work: Climate change pushes more and more people off the land as that land becomes increasingly uncultivable, and exposes them to a new set of risks in the cities to which they gravitate.

“There is no way to think about how to cope with climate change that doesn’t put the poor at the very center of the conversation,” Duflo says.

So far that conversation has ignored the poor, with the result that cities are ill prepared to undertake the massive infrastructure projects needed to accommodate an accelerating influx of people, says Duflo. That’s especially true in the Global South, which is the fastest urbanizing region and where most of the growth is informal—meaning that it is uncoordinated and happening outside of any legal framework. But it won’t be long before all urbanites—who already account for more than half of humanity—feel the strain.

Yet precisely because it has been the first to inhabit the climate crisis, the Global South has also been generating the first, albeit ad hoc, solutions. Heat, flooding and a surge in infectious diseases are forcing the poor, in particular, to be creative to survive. They are finding ways to keep cool and dry, building resilience from the bottom up—largely without the help of official institutions.

It’s a piecemeal resilience for now, but others are learning from their solutions, and in some cases scaling them up. Researchers are even realizing that despite being marginalized, informal settlements may have structural advantages over formal ones, since many of them combine high density and strong social and economic networks with a relatively small carbon footprint.

A new ethos is emerging—that informal urban growth may not just be inevitable but also may hold lessons in resilience for the cities of the future.

Mapping Heat and Health

Slums were long shown as “blank spots” on the world’s maps, UN-Habitat noted in 2003. Partly due to satellite and drone technology, and partly thanks to efforts by informal communities to map themselves, that is no longer true.

As the informal city swam into view, so did the negative effects of climate change on the urban poor. Now researchers are systematically studying those effects, to understand which solutions will bring the greatest benefits.

For example, in an ongoing study run by Indian grassroots organizations in collaboration with Harvard University, female tenant farmers and piece-rate workers received Fitbits to wear, and environmental sensors were fitted in their homes and workplaces to monitor the heat and humidity there. They showed that these people literally have no place to hide.

At the peak of summer, those who work outside, which is the majority, are exposed to near-intolerable temperatures—35° Celsius (95° Fahrenheit) and higher. “Even the water gets so hot that we feel that we are having tea,” said Subhiben, a study participant from Gujarat who works raking brine in the region’s enormous salt flats. And often, the sensor data show, the heat doesn’t let up when they return home.

Among the negative health outcomes that these women report are cardiac stress, gynecological problems including miscarriage, and mental health issues, says Sahil Hebbar, a doctor with the Self Employed Women’s Association (SEWA) in the Gujarati city of Ahmedabad and one of the coordinators of the study.

The research is revealing unsuspected interactions too, including between heat and malnutrition. According to Hebbar, up to half of SEWA’s members suffer from anemia, which can be caused by iron deficiency. That anemia correlates with much poorer cardiovascular outcomes in response to extreme heat, according to an as-yet unpublished finding of the study.

Other researchers are documenting the infectious diseases spreading in informal settlements, helped along by crowding and inadequate ventilation. Tuberculosis remains endemic in India where, according to the World Health Organization, two deaths from TB occur every three minutes. It is a major problem at Shaikh’s housing project, as it is at many others across the country.

The situation is reminiscent of the disease-ridden slums of New York, London and other northern cities in the early 20th century, except that today the disease is preventable. “We have the tools to diagnose and treat 100 percent of people with TB,” says Guy Marks, a respiratory physician at the University of New South Wales in Sydney and president of the International Union Against Tuberculosis and Lung Disease.

Cholera and other waterborne diseases typically surge in the wake of floods, and a 2025 study showed that one in three informal settlers in the Global South live in floodplains and are at risk of a “disastrous flood.” But such diseases are now a problem outside of floods, too. Meanwhile, vector-borne diseases, such as those carried by mosquitoes, are on the rise. Health geographer Olivier Telle of the CNRS in Paris reports that dengue, which is transmitted by the Aedes aegypti mosquitois thriving in informal settlements where heat is increasing and people stock water because they don’t have access to a running source—providing ideal conditions for mosquitoes to breed.

And rather than staying in these settlements, which are often on the edges of cities, dengue is creeping toward the city centers, following human mobility and employment opportunities. Telle’s team found that in Delhi, for example, the wealthiest neighborhoods had an incidence of dengue similar to impoverished ones, probably because more infected people from the periphery worked there. “You need to protect the least well-off to protect the community as a whole,” Telle says.

Cooling Begins at Home

As data on climate-driven health problems accumulate, researchers are beginning to discern which grassroots solutions are most protective. One of the most effective ways to protect workers from extreme heat is to ensure that they can keep their homes cool, the India-Harvard study found. Simply painting a roof with white reflective paint, for example, can reduce indoor temperatures in summer by around 2° Celsius. Since WHO estimates that more than half of the urban housing stock that India will need by 2070 has yet to be built, Hebbar hopes that such simple fixes will feed into that future formal development, producing more climate-adapted homes and workplaces.

Others are thinking along similar lines. Mumbai-based Sheela Patel, former chair of the grassroots federation Slum Dwellers International, is leading a project called Roof Over Our Heads (ROOH) in which slum dwellers—mainly women—collaborate with architects and engineers to build climate-resilient, affordable homes. One ROOH house I visited under construction in Mumbai had floor tiles made of plastic collected by informal garbage collectors and recycled. It was about to receive a roof of pre-painted galvanized iron sheeting, which reflects heat.

To date ROOH has built around 250 houses in a dozen countries, and Patel’s hope is that seeing these, other slum dwellers will borrow elements or copy them entirely. The project’s aim is to bring together broadly applicable solutions in a single place, eventually a web-based platform, so that people all over the Global South can access them and adapt them as needed. For her, it’s critical that the solutions come from the people closest to the problem, so that when the authorities finally decide to act, those solutions—tried and tested—will be waiting for them.

Others are devising plans for retrofitting whole settlements to make them more climate-resilient—the kind of solution that needs to be implemented top down, by city or state authorities. In Nairobi, Kenya, for example, a low-cost scheme to connect residents of the informal settlement Mukuru to the city’s sewage system has been put in place. This “simplified sewer,” which uses smaller pipes and shallower excavation, has already led to a significant drop in cholera , even though it’s only partially complete.

Such in situ upgrading is generally considered the gold standard for improving slums, because inhabitants stay put and their social and economic connections are preserved. But it isn’t always possible, according to urbanist José Núñez Collado of Victoria University of Wellington, New Zealand. For some informal settlements, relocation of the entire community is the best or only option—and that will be true more often, he says, as the climate crisis intensifies.

For now, such relocations tend to happen without much consultation with the inhabitants. This was the case, for example, with La Barquita—a flood-prone informal settlement in Santo Domingo in the Dominican Republic, whose inhabitants were relocated to a social housing project in 2016. Collado’s decade-long study of that relocated community shows that they feel more secure in their new home, La Nueva Barquita, but that many people have either lost their jobs or must now travel farther to work.

Projects like India’s ROOH are attempts to stimulate a more collaborative approach to improving informal settlements—one that combines bottom-up and top-down initiatives, taking account of the needs and expertise of their inhabitants. For ROOH’s Patel, such an approach is long overdue. “We believe that extreme weather is going to impact 2 billion people living informally in the future, a quarter of the global population,” she says. “No government, no industry, is looking at this.”

What is clear is that the informal city can’t be eliminated. As more data accrue, researchers like complex systems scientist and urbanist Luís Bettencourt of the University of Chicago are using it to show that informal settlements emerge in fast-growing cities as a bottom-up measure by which people build housing in the absence of adequate supply. “They provide a pathway to development,” he says.

Given this, Bettencourt thinks that governments should be working with the urban poor, not only to retrofit informal settlements, but also to plan prospectively—making sure that future cities are fit for habitation, and not just by the rich. His research, which builds on half a century of efforts by informal communities to map and survey themselves, has revealed one principle that he feels should guide all future policy. He distills it into two words: “Informal’s normal.”

—Laura Spinney (@laurainparis.bsky.social) Knowable Magazine

This article originally appeared in Knowable Magazine, a nonprofit publication dedicated to making scientific knowledge accessible to all. Sign up for Knowable Magazine’s newsletter.

Read the original article here.

太阳风暴如何影响地球天气?一项新研究探讨其作用机制

Tue, 07/21/2026 - 13:10
Source: Geophysical Research Letters

This is an authorized translation of an Eos article. 本文是Eos文章的授权翻译。

影响地球气候和天气模式的因素多种多样,从人为温室气体排放到火山活动,再到太阳活动的变化,不一而足。

随着太阳经历短期和长期的活动变化,包括众所周知的11年太阳黑子周期,太阳向地球大气层输送着不同量的总太阳能量。大量证据表明,太阳活动的长期变化与降雨量、地表温度和其他气候指标的变化之间存在相关性。然而,这些大气变量相互交织,难以辨别其背后的物理机制。

Raeder 报告了首个明确的证据,表明地磁暴,即由太阳活动爆发引起的持续数小时的地球磁层扰动,会影响地球上的天气状况。这些发现有助于科学家缩小太阳活动变化影响天气的可能机制范围。

该分析整合了67年来北美地区逐小时记录的地磁暴强度数据,以及同期逐小时记录的大气数据。后者的数据集得益于大气建模技术的进步,是近期才得以获取的。

数据显示,地磁暴会在数小时到数天内显著影响大气压力、温度和降水。地磁暴的强度似乎与其大气影响的严重程度密切相关。此外,这些影响还会因地区和季节而异。例如,冬季地磁暴似乎会提升美国西海岸的气温,而美国其他大部分地区的气温则会下降。

这些发现与先前提出的一些潜在机制吻合良好,但与其他一些机制则存在较大差异。他们排除了被称为宇宙射线云假说的机制,但总体上支持自上而下的机制,即从高层大气传播到对流层,而对流层正是我们大部分天气现象发生的区域。

基于这项分析,作者认为,先前观测到的太阳活动与地球天气之间的长期相关性,很可能是由类似本研究中分析的太阳风暴等短暂的太阳活动爆发造成的,而非缓慢的持续变化。

这项研究还可以为天气和气候模型的更新提供参考,目前这些模型在准确捕捉地磁暴对地球大气层的影响方面仍存在困难。

—科学撰稿人Sarah Stanley

This translation was made by Wiley. 本文翻译由Wiley提供。

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Southeast Tibet Grew in Pulses, Not All at Once

Tue, 07/21/2026 - 12:47
Editors’ Highlights are summaries of recent papers by AGU’s journal editors. Source: Tectonics

The gently sloping southeastern margin of the Tibetan Plateau preserves an important record of when and how the plateau expanded, yet its growth history remains contentious. By dating the cooling histories of minerals from the northern Jinsha River fold-and-thrust belt (a region where rock layers were compressed, folded, and thrust over one another), Shen et al. [2026] identify three episodes of accelerated exhumation, when tectonic uplift and surface erosion brought deeply buried rocks toward the surface: approximately 80–68 million years ago, 38–34 million years ago, and from about 19 million years ago to the present.

The oldest episode coincided with sediment accumulation in the adjacent Gonjo Basin, linking early mountain building to sedimentary basin development. The second episode records renewed compression along the Jinsha suture, a former tectonic plate boundary, and forms part of a broader southeastward propagation of crustal shortening across northern Southeast Tibet. The youngest episode primarily reflects incision by the Jinsha River, although continued fault activity may also have contributed to exhumation. Together, these results indicate that Southeast Tibet grew through multiple tectonic pulses over the past ~80 million years, rather than predominantly during a single phase driven by the southeastward flow of weak lower-crustal rock and consequent surface uplift.

Citation: Shen, X., Liu-Zeng, J., Shen, X., van der Beek, P., Cao, K., Xing, Y., & Zeng, X. (2026). Multi-stage tectonic growth of Southeast Tibet since the late cretaceous: Insights from the Jinsha suture zone in the three rivers region. Tectonics, 45, e2025TC009246. https://doi.org/10.1029/2025TC009246

—Djordje Grujic, Editor, Tectonics

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Making Weather and Climate Information Reach the Communities that Need It

Mon, 07/20/2026 - 19:29
Editors’ Highlights are summaries of recent papers by AGU’s journal editors. Source: Community Science 

Information about the weather is crucial for life, property, and work. Many people take it for granted. Yet, despite the centuries of sharing such information, especially when it is critical to provide warning, it does not reach all communities. There are many communities for which barriers of language, access, and trust lead to underutilization of information.

Sharma et al. [2026] address this challenge by considering how to design the information sharing process so it can get to the hard-to-reach communities. The study identifies where the information gets lost in translation. Considering this, the authors propose practical approaches to help ensure that all people, regardless of their location, language, or connectivity, can receive the information they need to prepare for and respond to high-impact weather events. This includes providing specific resources and staff that are dedicated to sharing this information with these communities. The study emphasizes the importance of designing information sharing processes that don’t assume that people will find the information—especially the most vulnerable.  

Citation: Sharma, S., Were, V., Farris, A., Joshi, A., Gerst, M. D., Sund, I., & Kenney, M. A. (2026). Information supply chain gaps for hard-to-reach communities: A solution-oriented framework from weather service insights. Community Science, 5, e2025CSJ000160. https://doi.org/10.1029/2025CSJ000160

—Muki Haklay, Editor, Community Science Exchange

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Students Enable Widespread Water Monitoring in India

Mon, 07/20/2026 - 12:58
Source: Community Science

When a local community gets involved in environmental monitoring, their efforts can build awareness of local environmental issues and provide more plentiful data than scientists can collect on their own. But how does the quality of the data compare to readings taken by professionals?

The state of Bihar, India, was the perfect place to find out. More than 90% of the population relies on groundwater for cooking and cleaning, but at times, that same groundwater has been reported to be contaminated with arsenic, iron, manganese, nitrate, and uranium, all of which can cause health problems. Richards et al. compared the results of community members’ efforts to monitor groundwater for contaminants with those of professional scientists.

The researchers recruited community members who were affiliated with one secondary school, three colleges, and one professional institution. Many participants were teenage students, but some were adult employees of the schools. All told, the team included 583 people. The participants collected water samples from places people access water during their daily lives, such as hand pumps that supply drinking water. The research team brought the samples back to the University of Manchester on commercial flights, then analyzed the samples at the Manchester Analytical Geochemistry Unit laboratories.

The results were broadly similar to those collected by professional scientists, showing that participatory science is an excellent way to increase the amount of data environmental scientists have to work with, the authors say. With more data, scientists can spot spatial patterns that might be overlooked with a smaller workforce. Participatory science can also generate interest in research, potentially bringing more women and minorities into the field. (Community Science, https://doi.org/10.1029/2025CSJ000136, 2026)

—Saima May Sidik (@saimamay.bsky.social), Science Writer

Citation: Sidik, S. M. (2026), Students enable widespread water monitoring in India, Eos, 107, https://doi.org/10.1029/2026EO260233. Published on 20 July 2026. Text © 2026. AGU. CC BY-NC-ND 3.0
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The 17 July 2026 landslide at Hanjia in Chongqing, China

Mon, 07/20/2026 - 06:17

Reports suggest 42 people were killed in a large rockslope failure. Imagery suggests that suspicion will fall on a cutting at the foot of the slope.

On Friday 17 July 2026, at 9:08 am local time, a large landslide occurred on the banks of the Wujiang River at Hanjia, located within of Pengshui Miao and Tujia Autonomous County in Chongqing, China. Media reports indicate that 42 people have been killed. Ten people were rescued.

Xinhua has released this image of the aftermath of the landslide:-

The aftermath of the 17 July 2026 landslide at Hanjia in Chongqing, China. Image from Xinhua.

There is some dramatic footage of the landslide in action and the immediate aftermath:-

The location of this landslide appears to be [29.27760, 108.16604]:-

Google Earth image of the site of the 17 July 2026 landslide at Hanjia in Chongqing, China.

The images and video suggest that this was a rockslope failure – note the size of the blocks – with a strong element of toppling. The very planar form of the rear scarp suggests to me that release has come from an existing joint or fault.

The media reports indicate that rainfall was the final trigger – this makes sense from a timing perspective – but the focus might be on the underlying causes. My attention is immediately drawn to the building beside the road on the slope side of the site. It appears that the slope has been cut to create the space for the building. The building was under construction in 2014, but this image from 2017 shows the cut more clearly. I have annotated the top of the cut slope:-

Annotated Google Earth image from 2018 showing the site of the 17 July 2026 landslide at Hanjia in Chongqing, China.

This would be my starting point in terms of likely causation of this landslide. Interestingly, there are other locations along this road with large cut slopes, so an immediate priority will need to be an assessment of the stability of those sites.

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Big Trouble from Little Wetlands

Fri, 07/17/2026 - 14:03

Wetlands are the largest natural source of methane on Earth. Though the waterlogged lands offer benefits that include hosting thriving ecosystems and protecting our shorelines from flooding, researchers are eager to better understand their contribution to the warming climate.

Researchers report that typical global wetlands surveys overlook an astronomical number of small wetlands: about 160 million of them.

In a paper published in Nature Climate Change, researchers report that typical global wetlands surveys overlook an astronomical number of small wetlands: about 160 million of them.

These small wetlands, which range in size from a large swimming pool to 100 hectares (250 acres), are responsible for 25% of the present global methane emissions, the research found. The results also revealed that these methane emissions increased by 9.9% from 2003 to 2022. This increase reflected both a growing number of small wetlands and climatic changes that spurred them to generate more emissions.

The work shows our current grasp on these environments is woefully incomplete.

The new research “points to the strong need to study these ecosystems further,” said Kyle Delwiche, a biogeochemical scientist at the University of California, Berkeley, who was not involved with the research.

Methane Mania

Wetlands come in myriad flavors and are found on every continent except Antarctica. Groundwater feeds peat-rich bogs and fens in places like Scotland and Scandinavia, and the Amazon and Congo Rivers support sprawling, forested swamps. Though the mechanisms underlying each wetland differ, the environments are united by a group of methane-producing microbes that thrive in their oxygen-starved soils.

Researchers have long known wetlands are major sources of global methane, a greenhouse gas with significantly more near-term warming potential for our climate than carbon dioxide. But quantifying these wetlands to assess their emissions is no simple task.

To study wetlands on a global scale, researchers typically use coarse-resolution satellite data, said Fa Li, an Earth system scientist at the University of Texas at Austin and lead author of the study. These data have a relatively low resolution (one pixel from these satellites represents 25 square kilometers) but can pierce through dense foliage, making them invaluable for wetlands research, Li said.

In the new research, Li and his colleagues turned to high-resolution satellite imagery. One pixel from these satellites is 30 square meters, which is just over half the size of an Olympic swimming pool. By combining this imagery with emissions data, the researchers were able to refine methane emissions calculations on a global scale.

Most of the 160 million small wetlands the survey revealed were concentrated in northern latitudes in places like Canada and Siberia.

“It’s really high, but I think this value [of 160 million] is certainly underestimated,” said Li.

Small tropical wetlands in particular tended to punch above their weight class, he added.

Such work will ultimately reveal “what level of atmospheric carbon dioxide and methane removal is needed to keep our planet hospitable.”

“Our results show that tropical small wetlands contribute disproportionately to methane emissions,” Li said. “Although tropical regions account for only 15.1% of global small-wetland area, they contribute 37% of methane emissions from small wetlands.”

Though higher-resolution satellite imagery can capture smaller wetlands, the technology is incapable of piercing through tree canopies. Because of this trade-off, forested swamps and other covered wetlands were excluded from the study.

“Methane emission rates are positively related to the temperature,” said Li. As the global temperature increases, these methane-emitting microbes become more productive. “It’s like a snowball that gets bigger and bigger,” he said. Rising global temperatures likely triggered the increased emissions and will continue to feed the tumbling snowball in the future.

Delwiche is excited about the new work and would like to see it extended to eventually cover forested wetlands. “We need accurate estimates of emissions and trends,” she said. Such work will ultimately reveal “what level of atmospheric carbon dioxide and methane removal is needed to keep our planet hospitable.”

—Taylor Mitchell Brown (@tmitchellbrown.bsky.social), Science Writer

Citation: Brown, T. M. (2026), Big trouble from little wetlands, Eos, 107, https://doi.org/10.1029/2026EO260232. Published on 17 July 2026. Text © 2026. The authors. CC BY-NC-ND 3.0
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We’re Getting Better at Knowing When Climate Change Is to Blame, National Academies Report Says

Thu, 07/16/2026 - 19:00
body {background-color: #D2D1D5;} Research & Developments is a blog for brief updates that provide context for the flurry of news regarding law and policy changes that impact science and scientists today.

Scientists have gotten much better at parsing how severe events are linked to climate change, a long-awaited report from the National Academies of Sciences, Engineering and Medicine has found. 

“A human influence is now being clearly detected in several important categories of extremes.”

The report was developed by 14 experts (including climatologists, meteorologists, and atmospheric scientists) and updates a 2016 report on the same subject. That report found that climate change was partly responsible for worsening heat waves, cold events, droughts, and heavy precipitation events, but that improvements to attribution science—a branch of climate science that aims to determine the extent to which individual extreme weather events are caused by climate change—were needed.

A decade later, the new report notes that advances in attribution science have allowed researchers to determine more effectively the link between climate change and specific weather events. In particular, improvements in observations of Earth systems, better satellite measurements, and longer observational records have “substantially increased our confidence” in attributing long-term changes in the frequency of extreme events to climate change, said Jim Hurrell, an atmospheric scientist at Colorado State University who was part of the panel that created the report, in a presentation about it. 

According to the report, confidence in attributing events to climate change is still highest for extreme heat and cold events, followed by heavy precipitation events and drought. The report notes that “significant advances” have been made in the science of attributing tropical cyclones, but that scientists still have low confidence in attributing specific hurricanes or typhoons to climate change. Similarly, due to the many drivers of wildfires, there is still low confidence in scientists’ ability to attribute specific wildfire events to climate change. 

“A human influence is now being clearly detected in several important categories of extremes,” Hurrell said.

Attribution studies, the new report notes, may help improve public understanding of climate change, support governments’ risk management and planning, and inform policymakers about the effects of climate change.

Climate Litigation

The report’s findings could also be used to bolster dozens of legal cases against energy companies being pursued by states, municipalities, tribes, and even individuals. These lawsuits claim that fossil fuel and energy companies are directly to blame for harms resulting from climate-related events such as heat waves, fires, and storms. One wrongful death case, for example, seeks damages from ExxonMobil, BP, Chevron, Shell, and other companies for their role in fueling an extreme heat wave in the Pacific Northwest in 2021 that killed more than 1,400 people

“A report with the kind of gravitas that the National Academies can bring will be a huge boost to the plaintiff’s cases.”

“A report with the kind of gravitas that the National Academies can bring will be a huge boost to the plaintiff’s cases,” Patrick Parenteau, an emeritus professor at Vermont Law and Graduate School, told POLITCO

Because the report may be useful for such lawsuits, its release has faced criticism from skeptics of anthropogenic climate change. Such opposition, which included records requests to collect scientists’ emails and efforts to discredit attribution science, pressured two people to leave the group producing the report, according to POLITICO.

On the day of the first meeting of the National Academies’ panel to assemble the new attribution report, Roger Pielke Jr., a senior fellow at the American Enterprise Institute, a conservative think tank, called the project “institutionalized stealth advocacy in support of climate litigation.” 

The goal of such opposition is “to keep attribution science out of court,” Alice Hill, a former federal prosecutor who worked on climate policy in the Obama administration, told POLITICO. “And what is the ultimate reason for that? To shield the fossil fuel companies from liability.”

Advancing Attribution Science

The report’s authors write that further improvements to attribution science have “significant potential” to help researchers understand the economic, health, and other impacts of climate change-fueled extreme events. 

 
Related

To further strengthen attribution science and its usefulness in mitigating the effects of extreme weather, the report suggests a range of actions are needed, including producing higher-resolution global climate models, conducting more studies that apply multiple attribution science approaches to the same event, providing additional peer review of attribution studies, and making improvements to the observational datasets underlying attribution science, especially in the Global South.

“Continuing to improve observing systems remains a priority, because attribution science ultimately depends on reliable observations,” Hurrell said. “There are still vast regions of the world that just have mostly inadequate data records.”

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

These updates are made possible through information from the scientific community. Do you have a story about how changes in law or policy are affecting scientists or research? Send us a tip at eos@agu.org. Text © 2026. AGU. CC BY-NC-ND 3.0
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The “Eternity Glaciers” Are Almost Gone

Thu, 07/16/2026 - 13:18
At 4,884 meters (16,024 feet) tall, Puncak Jaya, in the Indonesian part of the island of New Guinea, is the tallest mountain in Oceania. Credit: Klaus Thymann

Now, as a pilot who flies over Central Papua’s Sudirman mountain range nearly every day, Belau is not seeing as much ice as he used to, even compared to when he first began flying 9 years ago.

“It’s really sad,” he said. “It’s not the eternity iceberg or the eternity glaciers anymore. It’s going to be ‘the 5-year glaciers’ or ‘10-year glaciers.’”

Alion Belau captured this footage as he flew a route over Puncak Jaya in 2016. Over the past 9 years, he’s watched the extent of the mountain’s glaciers shrink. Mapping What Remains

Klaus Thymann, an environmental scientist and explorer, as well as the founder and director of the nonprofit Project Pressure, recently created the first photogrammetry model of the glaciers on Puncak Jaya, aiming to document their current extent and raise awareness about their decline. Photogrammetry uses photography to gain information about the dimensions and location of an environment.

Past research has suggested that in 1850, about 18.8 square kilometers of Puncak Jaya were covered by glaciers. By 2002, that area had shrunk by 88.6%, to 2.14 square kilometers.

A still image from the final 3D photogrammetry model is seen here. In blue is the fragmented East Northwall Firn Glacier, which has decreased in area by approximately 95% since 2002. Model Credit: Klaus Thymann & Pix4D

Thymann has long been interested in documenting “white spots on the map,” or areas with little data. But he’s been particularly interested in equatorial glaciers. In 2024, he and a team of dozens trekked up Uganda’s Rwenzori Mountains to document the decline of glaciers on Mount Stanley.

“We think of palm trees, and furry animals, and warmth, and exotic fruit when we talk about the tropics, not ice,” Thymann said. “The [idea of] tropical glaciers is hugely fascinating.”

They aren’t just fascinating to people from other countries. Belau said one reason the decline of the glaciers is saddening is because their presence used to attract people from across Indonesia to his home province of Papua.

Ice once covered both of these ridges on Puncak Jaya, but now it is concentrated in the saddle between the two. Credit: Klaus Thymann “Just a Name Now”

Glaciers the world over are shrinking or disappearing altogether in the face of climate change. Since 2000, Earth’s glaciers (excluding the ice sheets of Greenland and Antarctica) have lost an average of 273 billion metric tons of ice per year, according to the European Space Agency. And the loss is accelerating: The amount of ice lost from 2012 to 2023 was 36% higher than the amount lost between 2000 and 2011.

This pair of images, captured by the Thematic Mapper on Landsat 5 in 1988 and by the Operational Land Imager on Landsat 8 in 2017, shows the loss of Puncak Jaya’s glaciers over the course of less than 3 decades. Credit: NASA Earth Observatory images by Joshua Stevens, using Landsat data from the U.S. Geological Survey

As the tallest peak in Oceania, Puncak Jaya is also one of the Seven Summits, or the highest peaks on each continent and a common goal for die-hard mountaineers. The climb up Puncak Jaya is a technical one, but part of what makes it so difficult to summit is the logistics. Thymann obtained a permit and coordinated with local authorities to fly into Timika, where he waited until conditions were safe for a helicopter to take him up the mountain.

“I called it the cloud lottery,” he said.

Even on the mountain, there were more cloud lotteries while Thymann waited for enough visibility. On its face, the work, done over the course of several days, was simple.

Thymann worked with a local military guard who had accompanied him to place colorful ground control targets around the area. These targets helped Thymann’s drone to calibrate its location as it captured hundreds of high-resolution images. These images were later combined to create the photogrammetry model.

Klaus Thymann used a drone to capture hundreds of photos of Puncak Jaya and what’s left of its glaciers. These images were combined to create a photogrammetry model. Credit: Klaus Thymann

“I was surprised to see there was still some ice left,” Thymann said. “But mountains are like fractals. It’s very difficult to judge scale. And, of course, it’s very very little that’s left.”

Francine Hematang, a forestry and environmental scientist at Papua University in Indonesia, was not involved with Project Pressure’s efforts but recently led a study that used satellite data to document the decline of Puncak Jaya’s glaciers from 1980 to 2024. The study’s results suggested that the glacier area atop the mountain declined by 97% in that 44-year period. Four of the mountain’s six glaciers disappeared completely. Hematang called Project Pressure’s survey “excellent.”

“It uses photogrammetry, which will certainly capture the details of the glacier much better than satellite imagery,” he told Eos in an email. “With photogrammetry, we might be able to see the glacier’s boundaries and slope gradients in detail, and perhaps estimate its volume as well.”

Belau said that the accurate mapping data could allow locals to share the stories of the glaciers with future generations. After all, he said, “eternity glaciers…is just a name now.”

Indigenous peoples living near Puncak Jaya, including the Moni, call the glaciers atop Puncak Jaya the “eternity glaciers.” “It’s just a name now,” said Alion Belau, a Moni pilot. Credit: Klaus Thymann

—Emily Gardner (@emfurd.bsky.social), Associate Editor

Citation: Gardner, E. (2026), The “eternity glaciers” are almost gone, Eos, 107, https://doi.org/10.1029/2026EO260228. Published on 16 July 2026. Text © 2026. 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.

These “Clumped” Molecules Could Offer Clues About Earth’s Climate

Wed, 07/15/2026 - 18:00

Methane is one of the most abundant greenhouse gases on Earth, and, when compared with carbon dioxide, it is 28 times more potent at trapping heat in the atmosphere.

As the climate warms, it’s increasingly urgent to understand where methane comes from. Researchers can analyze the ratios of different carbon isotopes within methane to learn whether that sample came from fossil fuels or from other sources, such as wetlands or agriculture.

“I think this could end up being a landmark study.”

Sometimes, though, even these isotopic fingerprints leave room for uncertainty. New research examined several hundred liters of air gathered from compacted snow in Greenland in an even more precise way. The study, which marks the first time researchers have reconstructed the clumped isotopologue signature of atmospheric methane from past air, was published today in Science Advances.

“I think this could end up being a landmark study,” Edwin Schauble, a geochemist at the University of California, Los Angeles, who was not involved in the research, told Eos via email. “Methane is such an important greenhouse gas and tracer of the carbon cycle that the prospect of getting a better understanding of its history and future is exciting.”

The Nitty-Gritty

Methane (CH4) is made up of one carbon and four hydrogen molecules.

Isotopes, of course, refer to atoms of the same chemical element that have different numbers of neutrons. For instance, carbon naturally occurs in three isotopes: carbon-12, carbon-13, and carbon-14, with carbon-12 being the most common. Hydrogen has three naturally occurring isotopes, including deuterium (which has one proton and one neutron).

The word “isotopes,” explained Jiayang Sun, a geochemist who was a Ph.D. student at the University of Maryland when he coauthored the new paper, refers to elements at the atomic level.

“But when we say ‘isotopologue,’ it’s a word on the molecular level,” he said. “For clumped isotopologues, it’s two or more rare isotopes substituted into one molecule.”

This could mean that the carbon-12 in a methane molecule is replaced with a carbon-13 and one of the molecule’s hydrogens is replaced with deuterium, or it could mean that two of the hydrogens in the same molecule are replaced with two deuteriums.

“In some cases, the information from clumped isotopologues gives you information that’s independent from that provided by the straight isotopes,” said James Farquhar, a geochemist at the University of Maryland. “It gives us a little bit of a better understanding, or better constraints.”

Higher anthropogenic emissions result in lower clumped methane concentrations. However, clumped methane molecules take many years to reach equilibrium, so an increase in methane emissions might not show up in the clumped isotope signal for decades.

New Insights from Old Air

Modeling reflects that emissions of methane have changed over the course of the industrial era. NOAA data show that atmospheric methane levels have risen since the 1980s, with a plateau from 1999 to 2006. The new study’s researchers wanted to take a closer look at these changes by examining the clumped isotopes in air samples from the past.

“The overall trend is kind of clear, but when it comes to detailed allocation of total emissions to each source…the uncertainties related to that are still high,” Sun said.

Because methane makes up only about 2 parts per million of air, and clumped isotopes only represent part of that, the team would need a lot of air to undertake this investigation.

A team of researchers gathers a firn sample. Credit: Thomas Röckmann

But where do you get several hundred liters of decades-old air? One method is to use air found in firn, compacted snow that is the intermediate stage between snow and glacial ice. Researchers from Utrecht University, including atmospheric scientists Malavika Sivan and Thomas Röckmann, happened to have several hundred liters on hand.

The samples were gathered in 2018 as part of the East Greenland Ice-Core Project (EastGRIP). A team of researchers, including Röckmann, drilled a hole into the ice and inserted a 5-meter-long bladder and a set of three tubes. The bladder was inflated to seal the hole and prevent contamination. The tubes then pulled 30-year-old air out from the pores within the firn and pumped it into containers on the surface.

The Utrecht team was interested in examining the clumped isotope levels, but they didn’t have a mass spectrometer that could conduct such analysis on their relatively limited sample size. This made the University of Maryland researchers, who had the spectrometer but not the samples, a perfect partner.

After measuring the samples, the team used modeling to conclude that clumped methane reached a low in approximately 1993.

“Our model suggests that was caused by the increased anthropogenic methane emissions during the industrial period (the 1800s),” Sivan wrote in an email to Eos. “Clumped methane molecules take a very long time to equilibrate after such perturbations, hence the lag in the signal.”

Future Methane Levels

By helping us understand more about our past, this work could be combined with traditional bulk isotope measurements to improve modeling of future atmospheric methane levels.

“Not only do their results tell us much more about methane’s past history, their findings may also be very helpful in targeting pathways to bring methane’s rise under control.”

“It provides the data that would be needed to understand how we got here in terms of the isotopic compositions, and that’s a constraint that will be of value if we’re going to make interpretations about changes that happen in the future,” Farquhar said.

Euan Nisbet, an Earth scientist and professor emeritus at Royal Holloway University of London, said that clumped isotope research is “very much the forefront” of improving understanding of the global methane budget, and that this new work is “a very fine study.”

“Not only do their results tell us much more about methane’s past history, their findings may also be very helpful in targeting pathways to bring methane’s rise under control,” he said.

—Emily Gardner (@emfurd.bsky.social), Associate Editor

Citation: Gardner, E. (2026), These “clumped” molecules could offer clues about Earth’s climate, Eos, 107, https://doi.org/10.1029/2026EO260235. Published on 15 July 2026. Text © 2026. 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.

For the Birds: Solar Panels over Peatlands May Increase Avian Biodiversity

Wed, 07/15/2026 - 12:44

When Hanna Rae Martens visits the solar park she studies in northern Germany, she finds meadow pipits perched on the panels. They launch off to catch insects, then return, using the panels like tree branches.

This solar park, built on rewetted peatland, hosts a more diverse bird community than adjacent drained farmland, according to a new study in Ecological Solutions and Evidence. The findings suggest that combining peatland restoration with solar energy development could benefit birds.

Healthy peatlands hold large quantities of organic matter and, as a result, store more carbon than any other terrestrial ecosystem type.

In drained peatlands, on the other hand, that stored carbon is released to the atmosphere, presenting a major climate problem. In Germany, 95% of peatlands are degraded, and they account for 37% of all annual agricultural greenhouse gas emissions. Globally, drained peatlands emit 5% of all anthropogenic greenhouse gases. That is roughly twice what air travel produces.

Installing solar panels on rewetted peatland is one proposed [solution]: The land gets restored while landowners earn income from energy production.

Rewetting peatlands reduces emissions, but it also makes most crops impossible to grow, reducing the land’s economic prospects. Installing solar panels on rewetted peatland is one proposed way to resolve that: The land gets restored while landowners earn income from energy production.

Martens, a peatland ecologist at the University of Greifswald, led what she says is one of the first studies to examine what that setup means for birds. She and her colleagues tracked bird species at the solar park and at nearby drained grassland throughout the 2024 breeding season.

An Unusual Flock

The team used six low-cost AudioMoth recorders at the solar park and six at the drained grassland site. From March through October 2024, each recorder captured 40-second audio clips of the landscape every 4 minutes. The team generated a large dataset that was then run through BirdNet, an open-source neural network trained to identify bird species from their calls. To reduce false positives, the researchers applied species-specific confidence thresholds before counting any detection.

The solar park attracted a mix of species, including some typically found in wetlands, wooded edges, and urban areas. “The presence of wetland species like reed bunting and the endangered meadow pipit shows that the solar park is truly rewetted,” Martens said. “But we also recorded species like Eurasian tree sparrow and tree pipit, which are not typically found in peatlands. They all appear to use the structure of the solar panels.”

A solar park built on rewetted peatland hosts a more diverse bird community than adjacent drained farmland, new research suggests. Credit: Wattmanufactur, CC BY

Though the overall number of species was similar across both sites, the solar park scored significantly higher on two standard diversity indices—the Shannon and Simpson indices. In other words, it hosted a more even and consistently present community of common species.

Promising, with Caveats

Outside scientists said the results were worth attention but cautioned against reading too much into them.

“I think this is a great idea to study,” said Michael Schummer, an associate professor of wetland wildlife at the SUNY College of Environmental Science and Forestry who was not involved in the research. But he pointed to a methodological concern: The audio recorders inside the solar park were spaced as close as 90 meters apart, below the 250-meter minimum standard for bird monitoring surveys. At that distance, multiple recording stations may capture sounds from the same bird territory, potentially inflating diversity estimates.

“Just as we want more biodiversity in the world, I think we need more diversity in our landscapes.”

Guido Bakema, a soil scientist at Wageningen University who was also not part of the study, raised a separate issue. The study, he said, compared the rewetted solar park to drained grassland but not to a rewetted peatland without solar panels, raising the question of whether it was the rewetting or the solar panels that accounted for the change in bird diversity. “It would be better if they had separated this,” he said.

The authors acknowledged these limitations directly, agreeing that a lack of replicates in this study means that the effects of rewetting and the addition of solar panels cannot be isolated. However, at the time of the study, no other operational rewetted peatland solar park existed nearby for comparison.

Martens is already working to address those gaps. She has expanded her research to five sites this year and plans to examine how design choices such as panel height, spacing, and row width affect which species show up.

“Just as we want more biodiversity in the world, I think we need more diversity in our landscapes,” she said.

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

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Citation: Capella, L. G. (2026), For the birds: Solar panels over peatlands may increase avian biodiversity, Eos, 107, https://doi.org/10.1029/2026EO260229. Published on 15 July 2026. Text © 2026. 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.

How Tides and River Water Combine to Amplify Floods

Tue, 07/14/2026 - 12:43
Source: AGU Advances

Ocean tides push upstream along coastal rivers, in some cases reaching hundreds of kilometers inland. These inland stretches are known as tidal rivers, and they’re the scene of complex interactions between the river current and tidal oscillations. When rivers flood, tidal dynamics can sometimes add to a river’s height, increasing overall peak water levels and amplifying flooding.

This heightening mechanism occurred in China’s Yangtze River, where disastrous floods in both 1954 and 2020 were aided by tides. To learn more, Guo et al. combined data on river discharge and tides from both flood periods, along with a tidal model, to explore how interactions between the river and incoming tides conspired to create anomalously high water levels.

The authors found that peak water levels in both floods occurred around 1 to 2 weeks after peak river discharge during perigean spring tides when both the Sun and Moon are in optimal positions to create high tides. They hypothesize that peak river discharge rates suppress subharmonic tidal amplitudes, while intermediate rates of discharge allow for greater amplitudes and therefore higher water levels. Additionally, river water takes some time to fully move downstream, meaning that water levels are higher in the days following floods, adding to the effects of tidal inflows.

Comparing the two floods, the authors noted that channel deepening caused by sediment depletion from the Three Gorges Dam helped create higher water levels in 2020 than in 1954. Additionally, higher sea levels in 2020 helped water move upstream, also contributing to peak water levels.

Looking to other tidal rivers around the world, the authors say that cumulatively, more than 3,380 kilometers of tidal rivers are potentially exposed to floods caused by similar mechanisms. Other rivers, such as the Mekong and the Amazon, also see similar tidal subharmonics, meaning the same forces could conspire to create extra-large floods as swollen rivers and incoming ocean water combine. (AGU Advances, https://doi.org/10.1029/2025AV002247, 2026)

—Nathaniel Scharping (@nathanielscharp), Science Writer

Citation: Scharping, N. (2026), How tides and river water combine to amplify floods, Eos, 107, https://doi.org/10.1029/2026EO260230. Published on 14 July 2026. Text © 2026. 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.

Changes in Funding Could Tank Quality of Ocean Heat Content Data

Mon, 07/13/2026 - 12:04
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In the United States and elsewhere, ocean research infrastructure is facing a funding crisis. The U.S. National Science Foundation recently proposed dismantling hundreds of deep-ocean observation instruments, though it reversed the decision after public outcry. Still, a lagging NOAA budget and cuts to federal research funding have slowed the deployment of U.S.-owned instruments that measure ocean metrics and left the future of Argo, a global fleet of robotic instruments drifting in the ocean, in question. In addition, the number of observational floats deployed by Europe, as well as the number of active European floats, has dropped steadily since about 2020.

A study published in Nature Climate Change quantifies the impact that changes in funding could have on ocean data. Through a series of experiments, the research team showed that even small changes to the availability of data within the Global Ocean Observing System (GOOS), a United Nations–supported network of ocean observations, would significantly decrease the quality of ocean heat information available to researchers, making global climate and weather predictions more difficult.

Without U.S. contributions to the network, for example, “we lose the capability to monitor ocean warming,” said Lijing Cheng, an oceanographer at the Chinese Academy of Sciences and coauthor of the new study. Cheng is a member of the World Meteorological Organization’s Ocean Observations Physics and Climate Panel, which evaluates the status of global ocean observation systems and recommends strategies to keep such systems sustainable.

“It’s a really important paper because it is addressing the precarity of our current global ocean observing system,” said Hilary Palevsky, a marine biogeochemist at Boston College who was not involved in the study.

Data Degradation

GOOS is a network of observing platforms, ship observations, buoys, and Argo floats that measure various essential ocean variables such as temperature, salinity, nutrients, biodiversity, and more. In particular, the network provides high-quality data on ocean heat content, a measurement of the amount of energy stored in Earth’s oceans. Scientists use ocean heat content to project global sea level rise, tropical cyclones and hurricanes, marine heat waves and their impacts on ecosystems and fisheries, and more.

“If we want to know how much the climate is impacting ocean ecosystems, we have to monitor ocean temperature and ocean heat content changes,” Cheng said.

According to Cheng, much of the information gathered about the health of ocean observation systems like GOOS is simply inventories—counts of how many observations exist. Rarely does anyone evaluate how the number of observations available affects the quality of the data, he said. And with various global threats to data stewardship and funding, making that assessment could be more important than ever.

To see how a hypothetical loss of GOOS observations could affect ocean heat content data, Cheng and the research team ran two experiments. First, they randomly removed 20%, 40%, 60%, and 80% of the available GOOS ocean heat content observations to mimic possible changes to the system. Losing these data degraded measurements of the global annual ocean heating rate in all cases, increasing the relative error of the measurement by about 33%, 57%, 79%, and 97%, respectively.

“That’s a really risky place for us as the global ocean sciences community to have any country play such a pivotal role.”

Next, they removed the datasets by country, creating hypothetical scenarios where a country’s entire contribution was deleted from the network. Removing data from the five countries with the highest contributions (the United States, Australia, Japan, France, and Germany) degraded ocean heating rate measurements significantly in each case. Removing data contributed by the United States, for example, increased the relative error of the global annual ocean heating rate measurement by 163%, making the measurement difficult to distinguish from noise.

Cheng was surprised by the extent to which losing data maintained by the United States affected ocean heat content observations. The United States contributes more than 50% of the ocean observation data in GOOS and provides crucial observational coverage of the Arctic Ocean and the tropics. “We knew it was important, but it’s even more important than we thought,” Cheng said.

“Historically, I had been proud of how much the U.S. has contributed to the ocean observing enterprise globally,” Palevsky said. But, she added, “that’s a really risky place for us as the global ocean sciences community to have any country play such a pivotal role.”

The authors write that their results may be underestimates of how data loss will affect measurement quality because in many cases, observational equipment and data infrastructure are shared between countries, meaning a change to one country’s ability to collect observations could “propagate through the system.”

The team also tested only how a loss of observations would affect ocean heat content data. Other essential variables could fare even worse because they are already limited by having fewer observations than ocean heat content, Palevsky said.

Coordination and Collaboration

Cheng said the results indicate a need for countries to collaborate more closely to ensure long-term global coverage of ocean observations. “This should be done in a much more coordinated way,” he said. The World Meteorological Organization’s Global Telecommunication System (GTS) offers a possible model, he said. To access data from GTS, a country must also contribute data.

“Some of the U.S. contributions don’t have funding to take us all the way to having those conversations [in 2029].”

Scientists, too, could coordinate better by teaming up with each other when heading out on scientific cruises, Cheng said. He imagines a global platform scientists can use to communicate to see whether their research goals and cruise routes match up with those of scientists elsewhere in the world. The ocean observation community meets every 10 years; the next meeting will occur in Qingdao, China, in 2029. Cheng said the gathering will be a good opportunity for “everyone to sit together and create a high-level agreement about how to move forward” toward better coordination. “I think we can achieve this,” he said.

However, 2029 may come too late to address some of the uncertainty facing U.S. ocean research, Palevsky said. “Some of the U.S. contributions don’t have funding to take us all the way to having those conversations [in 2029].”

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

Citation: van Deelen, G. (2026), Changes in funding could tank quality of ocean heat content data, Eos, 107, https://doi.org/10.1029/2026EO260226. Published on 13 July 2026. Text © 2026. 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.

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