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Marine Heat Waves Slow the Ocean’s Carbon Flow

EOS - Mon, 11/03/2025 - 14:23

Marine heat waves describe instances of extraordinarily warm waters that can linger at the surface of the ocean for months. Much like the heat waves we experience on land, marine heat waves can alter environmental chemistry and disrupt biological processes. While catastrophic losses of megafauna are hard-to-miss indicators of a system in distress, researchers are now starting to amass enough data to understand how microbial organisms at the base of the ocean’s food webs are also responding to heat waves.

A new study published in Nature Communications presents a decade of measurements documenting two successive heat waves in the northeastern Pacific Ocean. The paper’s interdisciplinary team of authors used a combination of an autonomous robotic float, a research cruise, and satellite data to understand how microbial communities in the region reorganized in response to the extreme events.

The researchers discovered that production of organic matter increased at the ocean surface during the heat waves, but the carbon-rich particles didn’t sink or swim—rather, they just stayed in place.

The Biological Carbon Pump

Phytoplankton—tiny photosynthesizing microbes—prime the biological carbon pump. By using sunlight and carbon dioxide (CO2) to grow, they draw carbon out of the atmosphere and into the ocean’s carbon cycle. Zooplankton graze on the vast fields of these plantlike organisms, transporting carbon deeper into the water column in the form of fecal pellets and chunks of half-eaten plankton. Eventually, some of these particles sink deep enough to feed ecosystems of the deep ocean.

“The capacity for the ocean to sequester carbon relies on microbes at the base of the food web.”

This carbon pump represents a globally relevant buffer against the impacts of climate change, as the ocean absorbs approximately a quarter of CO2 emitted by human activity. Some estimates suggest that our current atmospheric concentration of CO2 could increase by as much as 50% if the biological carbon pump stopped shuttling carbon to the depths of the ocean.

“The capacity for the ocean to sequester carbon relies on microbes at the base of the food web, so it’s very important that we start understanding what these impacts from marine heat waves are on the microbial communities,” explained Mariana Bif, lead author of the new study. Bif is an assistant professor at the University of Miami and was previously a researcher with the Monterey Bay Aquarium Research Institute (MBARI).

When the Food Web Gets Tangled

In both of the marine heat waves tracked in the study, researchers found that the biological carbon pump showed signs of overheating. Carbon-rich particles loitered at approximately 200 meters (660 feet) below the surface, but during the two heat waves, different mechanisms caused the pileup.

The first heat wave included in the study began in 2013, when unusually weak winds over the Pacific failed to blow the warm air of summer back to the mainland of the United States. The heat wave, dubbed “the Blob,” made headlines as warm, stagnant, oxygen-deficient waters resulted in massive die-offs of fauna from all corners of the Pacific before dissipating in 2015.

In 2019, patchy cloud cover over the ocean and a shallower mixed layer at the sea surface set the stage for another heat wave to sweep the northeastern Pacific. This second heat wave brought temperatures right back up and became known as “the Blob 2.0.”

Bif and her coauthors found that during both heat waves, the marine microbial community went through a change in its “middle managers.”

Within the initial Blob years, physical and chemical conditions favored smaller phytoplankton species, which in turn favored a new herd of zooplankton grazers. This discrete food web eventually created an ocean layer full of organic particles that were too light to sink into the denser waters of the deep.

During the Blob 2.0, concentrations of particulate organic matter were even higher, but the increase wasn’t all from primary production. This time, conditions favored thrifty species. Organisms that could opportunistically feast on detritus and lower-quality organic matter became more prevalent, showing that the system was cycling and recycling carbon to keep it at the top of the water column. Within this community, parasites thrived, and organisms (including a group of radiolarians) that had never previously been seen in the northeastern Pacific started becoming regulars.

Measuring in the Middle of Nowhere

The array of technology used in the study distinguishes it from previous efforts to catalog the effects of marine heat waves.

“We’re now moving into an era of ‘big data’ in ocean biogeochemistry, whereas before we were just restricted to what we could collect from ships.”

“We’re now moving into an era of ‘big data’ in ocean biogeochemistry, whereas before we were just restricted to what we could collect from ships,” said Stephanie Henson, a principal scientist at the National Oceanography Centre in Southampton, U.K. Henson was not involved in the study.

Henson explained that autonomous floats and other advanced monitoring systems are allowing researchers to work with datasets that span beyond the length of a research cruise.

“People have been studying marine heat wave responses in systems like coral reefs and so on,” Henson said, explaining that researchers have observed that not every biological response is the same from one marine heat wave to the next. However, she noted that this study was the first she’s seen that demonstrates that ocean carbon fluxes are also having complex responses to marine heat waves.

To check the vital signs of the Pacific before, during, and after each of the heat waves, the researchers tapped into the Global Ocean Biogeochemistry Array (GO-BGC). GO-BGC instruments are a subset of the Argo array, a global network of thousands of autonomous robotic floats. Each float drifts freely in ocean currents, keeping tabs on pH, salinity, temperature, and more.

Mariana Bif gets ready to deploy a GO-BGC float in the Bay of Bengal. The float will drift freely in ocean currents at approximately 1,000 to 2,000 meters deep, returning to the surface every 10 days to send data about ocean temperature, salinity, and chemistry via satellite to researchers back on shore. (The Indian Ocean was not part of the new study, but Bif used GO-BGC floats in the Pacific to conduct the research.) Credit: Sudheesh Keloth, July 2025

Despite all that they can do, the floats are not able to collect microbial samples. For this, instead of Bif seeking the data, the data came to Bif.

Steven Hallam, a microbiologist at the University of British Columbia and a coauthor on the new study, reached out to Bif after reading an interview with her about her work on marine heat waves. He had a hunch that the planktonic DNA samples stored in his lab’s freezer might be helpful for Bif’s investigation into the ocean’s carbon cycle. Scientists in Hallam’s lab group had previously published research about bacterial communities in the same region, using samples collected during research cruises along the Line P transect off the coast of British Columbia.

After some back-and-forth via email, Hallam’s lab group reran the samples, expanding the analysis from bacteria to the entire community composition, resulting in a significant contribution to Bif’s study.

While the story of how the planktonic DNA came to Bif is a testament to the power of science communication and collaboration, Henson noted that the Line P transects “don’t necessarily overlap spatially with the regions of greatest impact of the marine heat waves” and combining datasets of different scales (such as shipboard data and the autonomous float datasets) should be done cautiously.

Still, Henson added, “it’s the best we can do, at the moment.”

Lingering Uncertainties

As for future research, Bif is involved in a few new projects exploring marine deoxygenated regions but said, “My focus is always the BGC-Argo floats.”

Bif noted that it will be interesting to look at BGC-Argo data from the floats that are in the middle of the marine heat wave currently affecting the North Pacific. That heat wave is already showing signs of slowing down, though scientists say it will likely hang around through the winter.

“I’m not sure if this one is going to have the legs that some of these previous marine heat waves in the region had,” said Nick Bond, who was not involved in this research but studied marine heat waves as part of his previous role as the Washington state climatologist. He is now a senior research scientist at the University of Washington.

“What we don’t measure, we can’t understand. We need more investments into monitoring the ocean.”

Bond added that while there’s “tentative evidence” that climate warming may be increasing the frequency of marine heat waves in the Pacific, there’s still much more to learn before scientists can accurately forecast how they will behave in the future.

Meanwhile, another looming unknown for this field of research is developing back onshore.

“There is a bit of a concern in the community because at the moment, for the global Argo program, the U.S. contributes about half of the floats that are deployed,” said Henson, her concern alluding to recent budget cuts to nearly all areas of federally funded research in the United States. However, she explained that other countries are stepping up with contributions to keep the Argo program afloat.

“What we don’t measure, we can’t understand. We need more investments into monitoring the ocean,” said Bif.

—Mack Baysinger (@mack-baysinger.bsky.social), Science Writer

Citation: Baysinger, M. (2025), Marine heat waves slow the ocean’s carbon flow, Eos, 106, https://doi.org/10.1029/2025EO250410. Published on 3 November 2025. Text © 2025. The authors. CC BY-NC-ND 3.0
Except where otherwise noted, images are subject to copyright. Any reuse without express permission from the copyright owner is prohibited.

Atmospheric Rivers Shaped Greenland’s Ancient Ice

EOS - Mon, 11/03/2025 - 14:00
Editors’ Highlights are summaries of recent papers by AGU’s journal editors. Source: AGU Advances

In a new study, Schnaubelt et al. [2025] examine how ‘atmospheric rivers’—bands of storms that carry large amounts of moisture through the atmosphere—impacted the Greenland Ice Sheet during a past warm period called the Last Interglacial, about 130,000 to 115,000 years ago. Using detailed computer models of Earth’s climate, the researchers find that changes in Earth’s orbit and atmospheric moisture controlled the timing and intensity of these storm systems reaching Greenland.

Early in the Last Interglacial, more atmospheric rivers occurred during summer months, causing significant melting around the ice sheet’s edges. Later in the period, atmospheric rivers became more frequent in winter, bringing increased snowfall instead.

The authors also find that conditions during that ancient warm period were similar to what scientists expect in future climate scenarios. This suggests that increased atmospheric moisture in the Arctic and more summertime atmospheric rivers will accelerate Greenland’s ice sheet melting in the coming centuries. By comparing past and future climates, this research shows how large-scale storm patterns and moisture transport influence ice sheet stability in a warming world.

Citation: Schnaubelt, J. C., Tabor, C. R., Otto-Bliesner, B. L., & Lora, J. M. (2025). Atmospheric river impacts on the Greenland ice sheet through the Last Interglacial. AGU Advances, 6, e2025AV001653. https://doi.org/10.1029/2025AV001653

—Francois Primeau, Editor, AGU Advances

Text © 2025. The authors. CC BY-NC-ND 3.0
Except where otherwise noted, images are subject to copyright. Any reuse without express permission from the copyright owner is prohibited.

Non-Maxwellianity of ion velocity distributions in the Earth's magnetosheath

Physical Review E (Plasma physics) - Mon, 11/03/2025 - 10:00

Author(s): Louis Richard, Sergio Servidio, Ida Svenningsson, Anton V. Artemyev, Kristopher G. Klein, Emiliya Yordanova, Alexandros Chasapis, Oreste Pezzi, and Yuri V. Khotyaintsev

We analyze the deviations from local thermodynamic equilibrium (LTE) of the ion velocity distribution function (iVDF) in collisionless plasma turbulence. Using data from the magnetospheric multiscale (MMS) mission, we examine the non-Maxwellianity of 439 685 iVDFs in the Earth's magnetosheath. We fi…


[Phys. Rev. E 112, L053201] Published Mon Nov 03, 2025

Landslides from the 3 November 2025 Afghanistan earthquake

EOS - Mon, 11/03/2025 - 07:37

Some videos have emerged from Afghanistan this morning, reportedly showing landslides and rockfalls triggered by the M=6.3 earthquake.

At 12:59 am on 3 November 2025 (local time, which is 20:29 UT on 2 November 2025), an M=6.3 earthquake struck near to Mazar-E Sharif in Afghanistan. Initial reports suggest at least 20 fatalities have occurred, but the USGS PAGER estimate is a 40% probability of fatalities in the range of 100 – 1,000, and a 37% probability of fatalities of >1,000. That this earthquake has struck as winter approaches is likely to increase the impact over the coming months.

There are some initial reports and images of landslides. Of course, at this stage these are unconfirmed. But on social media there are two reports of particular interest. The first purportedly shows a large failure in in Marmal district of Balkh province. I have stopped using Twitter, but Jahanzeb Khan, who is an independent journalist for women and human rights violations in Afghanistan, has posted this video there:-

#URGENT: The situation in Marmal district of Balkh province after the earthquake is extremely concerning. Local residents are in difficult conditions and in urgent need of medical and humanitarian assistance.

The situation is worsening in many other districts and provinces. pic.twitter.com/Xo7o2eyKPw

— Jahanzeb Khan (@Jahanzeb_Khan20) November 3, 2025

This appears to show a large, complex landslide, possibly rotational in nature:-

A landslide reportedly triggered by the 3 November 2025 earthquake in Afghanistan. Image from a video posted to Twitter by Jahanzeb Khan.

Meanwhile, another journalist, Abdulhaq Omeri, has posted a video that appears to show a road severely damaged by rockfalls. There appears to be some injured people from these events:-

په افغانستان کې وروستۍ زلزلې زیانونه اړولي دي. #earthquake #Afghanistan pic.twitter.com/dhHhigSLQh

— Abdulhaq Omeri (@AbdulhaqOmeri) November 3, 2025

There are reports that the road between Kabul and Mazar is blocked by landslides. The USGS initial map of intensity and landslides looks like this:-

USGS MMI and landslide forecast map for the 3 November 2025 earthquake in Afghanistan. Map as of 07:20 UTC on 3 November 2025.

The east-west orientated ridge just to the north of the earthquake epicentre appears to have high landslide potential, and the Kabul-Mazar highway, which cuts through this area, is reported to be blocked. This could impede the delivery of assistance, worsening the impact of building collapses.

Return to The Landslide Blog homepage Text © 2023. The authors. CC BY-NC-ND 3.0
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Teleseismic waves hybrid simulation method considering the free surface boundary condition in a 3D receiver-side model

Geophysical Journal International - Mon, 11/03/2025 - 00:00
SummaryWith the deployment of dense linear seismic arrays, teleseismic waves are playing an increasingly important role in studying deep structures beneath seismic stations. However, despite significant advancements in high-performance computing, simulating high-frequency teleseismic waves (above 1 Hz) in a 3D model on a global scale remains challenging. To address this issue, previous studies have developed hybrid methods that utilize the displacement representation theorem to equivalently transform stresses and velocities simulated in a 1D or 3D global reference earth model into body force and moment rate density tensor sources for input into a 3D region model. Although previous hybrid methods have incorporated the free surface, the treatment of two types of equivalent sources at this boundary, particularly the equivalent moment rate density sources, has not been fully addressed. Neglecting the influence of the free surface condition and directly adding the equivalent sources at the free surface may lead to spurious waves. To resolve this, we develop a hybrid simulation method considering the effects of the free surface condition. By setting the relevant components of the equivalent sources on the free surface to zero, the method effectively reduces artifacts caused by coupling effects. We then propose the QSSP-CGFD3D hybrid method, which includes this free surface boundary correction, for simulating teleseismic waves in a 3D receiver-side model. We validate the accuracy and effectiveness of the hybrid method for calculating P-waves, S-waves, and surface waves in the AK135 model. We also apply the method to the fault zone region, where the results show that the fault zone causes arrival time delays and amplitude amplifications of teleseismic P-waves. These effects can be used to infer structural parameters of fault zones. Furthermore, we employ the QSSP-CGFD3D hybrid method to simulate the influence of undulated interface within the crustal structure on telesesimic waveforms, demonstrating its potential for receiver function analysis. The proposed hybrid method demonstrates significant potential for studying structures beneath seismic arrays, and holds promise for advancing our understanding of such features.

Synthetic Tests of Reliability of Back-Projection Images of Earthquake Ruptures

Geophysical Journal International - Mon, 11/03/2025 - 00:00
SummaryBack-projection inversions of teleseismic waveforms for the images of rupture progression in great earthquakes have become a popular tool in earthquake studies. However, verifying the trustworthiness of the obtained images in synthetic tests, in which forward-problem data from known propagating ruptures on finite faults are inverted and compared with the true images, have been disproportionally lacking. Such validations for known rupture geometries in a homogeneous medium provide the best-scenario probe into the theoretical ability of the method to resolve the true faulting kinematics. Unambiguous identification of the true source of radiation is possible if alternative trial subfaults, not representing the real emitter, shift the wave-arrival time by different amounts at different stations, resulting in no significant stack achieved for them. This condition is quantitatively expressed in the value of the dimensionless uniqueness coefficient q, which must exceed unity for the inversion to become unique. The criterion is not satisfied for the faults of finite dimensions, precluding reliable determination of rupture progression and speed for them, no matter how wide the coverage of the azimuths from the fault to the stations and how many stations in the network. Unambiguous determination of the exact location is possible for point-source radiators with widening of the azimuthal coverage: the reduction in ambiguity is seen in the progressive improvement in the correctness of the images as the uniqueness coefficient increases to the values greater than one. Fictitious moving, linearly aligned sources appear, increasing in number, as the value of the coefficient gradually drops.

Seismic characteristics and implications of ultramafic rocks from the Red Hills Massif, northern South Island, New Zealand

Geophysical Journal International - Mon, 11/03/2025 - 00:00
SummaryOlivine, orthopyroxene and clinopyroxene are the most common minerals in ultramafic rocks, their modal contents and crystallographic preferred orientations (CPOs) are main factors determine the total seismic properties (e.g. seismic velocity and anisotropy). Red Hills Massif is the main part of Dun Mountain Ophiolite Belt, and includes all six most typical olivine CPO types (A-E & AG-type) and various ultramafic rock types. In this case study, 6 paired harzburgite and dunite (Series 1 samples) and olivine/clinopyroxene-related ultramafic rocks (3 dunites, 2 wehrlites, 2 olivine clinopyroxenites and 1 clinopyroxenite) are selected to proceed detailed seismic characteristics analysis. Seismic distributions of Series 1 and 2 peridotites are based on their olivine CPO characteristics while the distributions of Series 2 (olivine) clinopyroxenites are based on their clinopyroxene CPO characteristics. Due to the addition of orthopyroxene, almost all harzburgites have slower P-wave velocity and less P/S-wave anisotropy than dunites in the same pair. On the other hand, both olivine & clinopyroxene CPO combinations and modal contents of Series 2 ultramafic rocks are various. With increasing modal proportions of orthopyroxene or clinopyroxene, seismic properties are not necessarily decreasing. When the [001]OL crystallographic axis in harzburgite develops a girdle fabric, or when the [100]OL and [001]CPX orientations exhibit misalignment with respect to the lineation direction, a significant reduction in seismic wave velocities is observed. Concurrently, seismic anisotropy magnitudes demonstrate marked enhancement under orthopyroxene- or clinopyroxene-dominant conditions (>60 per cent modal abundance). The intricate olivine and ortho-/clinopyroxene CPO patterns and related seismic characteristics preserved beneath the Red Hills Massif are thought to pre-date initiation of the Alpine Fault (∼25 Ma). This interpretation is supported by the similarity in olivine grain size between the Red Hills peridotites and the lithospheric mantle beneath West Otago, implying a shared pre-25 Ma mantle domain. Prior to Alpine Fault offset, these two regions were adjacent, and their lithospheric high-velocity seismic signatures remain correspondingly alike. Once the initiation of Alpine Fault kinematics started, the observed anomalous SKS azimuth proximal to the study area may reflect either: (1) the development of protomylonitic textures analogous to those documented in the West Otago lithospheric mantle, or (2) the preservation of pre-existing deformation fabrics. Conversely, lithospheric fast shear wave splitting directions, when combined with gravity data and rock density constraints, can potentially resolve the dominant olivine CPO type(s), the relative proportions of olivine and ortho-/clinopyroxene, and their combined CPO patterns.

Covariance-Based Estimation Performance for In-Flight Calibration of NASA’s ACS3 Solar Sail

Publication date: Available online 28 October 2025

Source: Advances in Space Research

Author(s): Andrea Minervino Amodio, Livio Carzana, Dominic Dirkx, Jeannette Heiligers

Ground Validation of Dust Multi-properties Analyzer Onboard Tianwen-2

Publication date: Available online 27 October 2025

Source: Advances in Space Research

Author(s): Xu Tan, Cunhui Li, Jiajie Wang, Zhongcheng Mu, Zecheng Cui, Meng Chen, Xin Ren, Xiaodong Liu, Yan Su, Wei Wang, Renhao Tian, Jiawei Li

Generation of oppositely propagating Alfvén waves by a substorm-injected proton cloud

Publication date: Available online 27 October 2025

Source: Advances in Space Research

Author(s): Ekaterina E. Smotrova, Olga S. Mikhailova, Pavel. N. Mager, Aleksandr V. Rubtsov

Seismic study sheds light on factors that led to 2025 Myanmar supershear rupture

Phys.org: Earth science - Sat, 11/01/2025 - 12:30
Recently, Science put out an article detailing new research on the Myanmar earthquake that occurred on March 28, 2025. In one of these studies, Shengji Wei and colleagues analyze data on the event and provide insight on multiple factors that lead to these rare and devastating supershear ruptures. Their research was published this week.

Humanity is on path toward 'climate chaos,' scientists warn

Phys.org: Earth science - Sat, 11/01/2025 - 12:20
Industries and individuals around the world burned record amounts of oil, gas and coal last year, releasing more greenhouse gases than ever before, a group of leading scientists said in a new report, warning that humanity is hurtling toward "climate chaos."

Abandoned coal mine drainage identified as a significant source of carbon emissions

Phys.org: Earth science - Sat, 11/01/2025 - 11:13
For the past 250 years, people have mined coal industrially in Pennsylvania, U.S.. By 1830, the city of Pittsburgh was using more than 400 tons of the fossil fuel every day. Burning all that coal has contributed to climate change. Additionally, unremediated mines—especially those that operated before Congress passed regulations in 1977—have leaked environmentally harmful mine drainage. But that might not be the end of their legacy.

Explorers seek ancient Antarctica ice in climate change study

Phys.org: Earth science - Sat, 11/01/2025 - 11:05
An explorer and a glaciologist have embarked on a three-month mission to cross part of Antarctica on kite skis in search of ice that is 130,000 years old.

Voicing Farmers’ Concerns on the Future of Agriculture

EOS - Fri, 10/31/2025 - 18:03
Editors’ Highlights are summaries of recent papers by AGU’s journal editors. Source: Community Science

A new study by Hopkins et al. [2025], which was recently published in Community Science’s special collection on “Transdisciplinary Collaboration for Sustainable Agriculture,” looks at how small- and mid-scale farmers and ranchers see the future of agriculture. It also examines how uncertainty about that future affects their mental health, decision-making, and ability to keep their farms running.

The authors interviewed 31 farmers in Georgia, asking about the challenges they face. These included money problems, a shrinking farm workforce, more complex regulations, and difficulties in passing farms on to the next generation. Many of these personal concerns were tied to bigger worries about agriculture overall, such as the growing gap between farmers and non-farmers, the rise of corporate-owned farms, changing weather patterns, and possible risks to the country’s food supply. These challenges often left farmers feeling alone, undervalued, and discouraged.

The study gives a rare long-term view of how farming communities can remain sustainable and resilient. It calls for strategies and policies that truly reflect farmers’ experiences and concerns—both for today’s problems and for future challenges—and that address not just immediate issues but also the deeper, systemic causes of stress in agriculture.

Citation: Hopkins, N., Weatherly, C., Reece, C., & Proctor, C. (2025). “At some point, you just run out of road”: Farmers’ concerns about the future of agriculture. Community Science, 4, e2025CSJ000140. https://doi.org/10.1029/2025CSJ000140

—Claire Beveridge, Editor, Community Science

Text © 2025. The authors. CC BY-NC-ND 3.0
Except where otherwise noted, images are subject to copyright. Any reuse without express permission from the copyright owner is prohibited.

Contrasting optical properties of fine particulate matter in Seoul and Mexico City highlight climate impacts

Phys.org: Earth science - Fri, 10/31/2025 - 15:10
Severe fine dust pollution over Seoul and Mexico City, being composed of the same type of fine particulate matter (PM2.5), exhibits markedly different characteristics. Seoul's air tends to reflect sunlight, contributing to a cooling effect on Earth, whereas Mexico City's particles are more inclined to absorb sunlight, potentially accelerating global warming.

Serendipity in Space: NASA’s Eye in the Sky

EOS - Fri, 10/31/2025 - 15:05
Editors’ Highlights are summaries of recent papers by AGU’s journal editors. Source: AGU Advances

NASA’s Orbiting Carbon Observatory-2 (OCO-2) was the first space-based sensor designed to study the Earth’s global carbon cycle and retrieves precise and accurate measurements of column CO2 from which fluxes of carbon over land and ocean may be inferred. The spectroscopic measurements, calibrated against an in-situ network, sample the atmosphere so that regional-to-continental fluxes can be quantified.

Svoboda et al. [2025] point out the enormous societal value of the OCO-2 observations from these satellites that in the normal course of events could continue providing gold-standard data for another decade.

Over its decade-plus in operation, OCO-2 has unraveled long-standing mysteries (Liu et al., 2017) and quantified massive events like the Australian fires in 2019-2020 (Byrne et al., 2021). Its most unexpected result was not from the CO2 retrieval, but rather from a serendipitous by-product! By virtue of its spectral resolution, OCO-2 ‘sees’ the faint glow, invisible to the naked eye, plants produce as chlorophyl molecules absorb photons. This glow, quantified, has turned about to be an extraordinary tool for studying plants and has proved to be amongst the most sensitive early warning signs of plant stress. It is well on its way to being a crucial way of measuring growth and anticipating stress in forest and agricultural landscapes, yet the mission is proposed for early termination.

Citation: Svoboda, M., Kira, O., Sun, Y., Smith, W. K., Magney, T., Wood, J. D., & Parazoo, N. C. (2025). Monitoring the pulse of America’s natural resources from the Orbiting Carbon Observatory missions. AGU Advances, 6, e2025AV002063. https://doi.org/10.1029/2025AV002063

—David Schimel, Editor, AGU Advances

Text © 2025. The authors. CC BY-NC-ND 3.0
Except where otherwise noted, images are subject to copyright. Any reuse without express permission from the copyright owner is prohibited.

How ship's logs have shaped our understanding of the sea

Phys.org: Earth science - Fri, 10/31/2025 - 13:11
What drives a wealthy Danish-Norwegian general to delve into ship's logs and become almost obsessed with understanding ocean currents in the 1800s? And why has this amateur researcher remained unknown until now?

The Role of a Ditch in the Matrix

EOS - Fri, 10/31/2025 - 11:45

This is an audio story from Eos, your trusted source for Earth and space science news. Do you like this feature? Let us know in the comments or at eos@agu.org.

TRANSCRIPT

Emily Gardner: Before Chelsea Clifford was an environmental scientist, she was a college student, working at White Mountain Research Center at UCLA, studying bugs.

Chelsea Clifford: While everyone else was doing really glamorous fieldwork in Yosemite, Kings Canyon, places like that, I was borrowing my aunt’s ex-husband’s ’91 manual transmission Honda Civic. I didn’t really know how to do manual and was scared of taking it up in the mountains. And so, when I had the opportunity to do independent research, I had gotten kind of fascinated staring out the window all that summer at these weird decorative ditches they had in the desert, diverted from the irrigation ditches into people’s backyards in the fancier suburbs.

Gardner: Clifford set out to study the invertebrate communities in these ditches, to see how they compared to the communities in natural creeks. That work sent her down a rabbit hole, and she’s still going down.

(The sound of running water fades in).

If you’ve never really thought about ditches, you’re not alone. In fact, according to a new paper written by Clifford and dozens of other researchers, most scientists don’t think about them either. Here’s AJ Reisinger, a freshwater ecosystem ecologist and biogeochemist at the University of Florida, who was not an author of the paper.

Reisinger: I do think that ditches are understudied, particularly in terms of their ecological and environmental implications. I think that’s largely driven by the artificial nature of ditches and the fact that ecologists tend to gravitate towards natural settings, natural ecosystems, natural environments. That’s why we get into ecology in the first place, because we’re interested in the environment. And so the artificial nature of ditches kind of precludes a lot of people from being interested or wanting to work in those areas often, I think.

Gardner: And that’s a problem, some scientists say. Because ditches do more than just carry water: They can be sources or sinks of nutrients, transport pollutants, host distinct ecosystems, and even emit greenhouse gases. This is why Clifford and dozens of other scientists came together in 2023 for a workshop to raise the profile of ditch research. The group included biogeochemists, ecologists, biologists, and even archaeologists. They published a perspective paper on their work in Communications Earth and Environment.

Among these self-described “ditchologists” was Michael Peacock, a biogeochemist at the University of Liverpool, where the workshop was held, and the Swedish University of Agricultural Sciences in Uppsala. He and Clifford led this paper together. They started out by—after much discussion—defining a ditch.

Peacock: I think we settled on the definition of a ditch for the paper was a linear constructed waterway that is usually filled with water and is aiming to take that water somewhere else, wherever people want it to go.

Gardner: In addition, ditches are usually narrower than 25 meters across. “Ditch” is also sort of a catchall term. Ditches used for irrigation might be called gripes, catchwaters, or dikes, whereas ditches used for transport might be called canals or waterways, for instance. As the paper points out, people might reach for these words because the word “ditch” has something of a negative connotation. To “ditch” also means “to abandon.” There’s also “dull as ditchwater” and “last-ditch efforts.”

Then the researchers laid out several of the reasons why ditches matter. Clifford gave the example of her hometown, Gloucester, Va., a sea level rise hot spot near the Chesapeake Bay. When saltwater intrusion occurs, it tends to reach ditches first, and is then transported further inland, compromising the freshwater used for crop irrigation or even drinking. Saltwater intrusion can also cause marsh migration, in which salt-tolerant crops move farther inland, and sometimes interfere with agriculture.

Clifford: Basically, what’s happening to the landscape as a whole is often happening to ditches first. Ditches are often headwaters of larger water bodies. So water may, you know, pass through them before going further downstream. So that can be a good spot to monitor and potentially intervene before there are larger issues.

Gardner: The paper points out that ditches can transport materials including microplastics, pharmaceuticals, pesticides, trace metals, pathogens, and PFAS [per- and polyfluoroalkyl substances]. These can affect humans, of course, and also the animal and plant communities in and around ditches.

Gea van der Lee is an aquatic ecology researcher at Wageningen University [and Research] in the Netherlands—a nation home to more than 300,000 kilometers, or about 186,000 miles, of ditches, or canals. In the Netherlands, she said, ditches are seen as a way to drain the land, but their role as a space for biodiversity is overlooked: They host bugs, plants, amphibians, and other animal life. A few years ago, she led a project that found that recording the sounds made in ditches can improve understanding of metabolism in ditches, because it can capture low-frequency sounds, like these, that may correspond to photosynthesis.

(A few seconds of a low-pitched sound play.)

Here’s van der Lee.

Reading List

Lines in the Landscape
(Communications Earth and Environment paper)

Freshwater ecoacoustics: Listening to the ecological status of multi-stressed lowland waters
(Ecological Indicators paper by Gea van der Lee & colleagues)

van der Lee: I found it really nice to be together with because there’s not so many people working on ditches, and then you come together with [a] whole group of ditch nerds that are really excited about ditches.

Gardner: Of course, outside of countries like the Netherlands, ditches don’t always take up a lot of room in the landscape. But Peacock offered a biogeochemistry perspective on why ditches still shouldn’t be overlooked.

Peacock: Generally, they’re small, and we ignore them, but we know they emit a lot of greenhouse gases, particularly methane, and they can sort of exert overwhelming effects on the ecosystem-scale methane balance.

You might have a field that is drained with ditches and the field is a net sink of methane because it’s dry. But the ditches, because they’re wet, which is where the bugs that make methane like to live, the ditches emit loads of methane. And if you add up the ditches and the fields, sometimes the ditches overwhelm the fields, and the landscape can be a small net source of methane. And you would never know that if you didn’t go and look at the ditches.

Gardner: Jeremy Biggs, a freshwater biologist, CEO of the Freshwater Habitats Trust, and visiting professor at Oxford Brookes University, who was also not involved in the paper, said this effort felt timely.

Biggs: It feels quite familiar to me because it feels like the same, the same kind of approach, the same line that we’ve taken with ponds and small waters more generally, that they’ve been neglected and overlooked.

Gardner: “Small waters” include freshwaters like ponds, headwater streams, springs, seepages, and of course ditches. They’re often ignored by researchers and regulators, Biggs said, simply because they’re small.

Biggs: We just assume small things are unimportant. And everyone just assumes that a big lake is more important than a small one and a big river is more important than a small one, and that’s why they’re not in regulations, in essence. But there’s a lot of them. That’s the thing. You don’t notice them, but there’s a lot of them.

Gardner: In earlier work, Peacock came up with the rough estimate that drainage ditches alone may cover up to 10.7 million hectares, or 26 million acres, globally. All this area means there’s also a lot of life in small waters.

Biggs: Although their individual site richness, or what ecologists call alpha diversity, is less than it is for a bigger water body, just as you’d expect, when you put them together in networks, it quite often turns out that they support more species collectively than do the bigger water bodies.

Gardner: Biggs is talking about standing waters and headwater streams here, but because headwater streams are a close proxy to ditches, he said he wouldn’t be surprised if the same was true for ditches, too. Ditches are home to communities of animals like wading birds, fish, and turtles, sometimes providing the only available refuge for such animals in highly farmed or urbanized landscapes. A ditch is also home to one of the rarest plant species in the U.K., the fen ragwort.

So what’s next for ditches?

Peacock: I suppose the first step in a way is just to notice them, that to realize that they’re there and they’re everywhere and that they shouldn’t be ignored. I think in one paper I called ditches “no-man’s-land,” because all the terrestrial scientists stop at the ditch edge. “That’s a ditch. That’s nothing to do with me.” And all the limnologists, the people who study waters, see a ditch and think, “That’s not an inland water. It’s a ditch.” And they just slip through the net. And I think we need to recognize that they are there. They are important. There’s a lot of them and they’re probably doing lots of different important things, some of them positive, some of them negative.

(“Swamp Walking Blues by Chelsea Clifford fades in.)

Gardner: I’m Emily Gardner, reporting for Eos, the science news publication of AGU. You can find a reading list and a transcript for this story at Eos.org. Thank you to Chelsea Clifford, Michael Peacock, Gea van der Lee, AJ Reisinger, and Jeremy Biggs for speaking with me for this story. And an extra big thank you to Chelsea Clifford for providing the music you’re hearing right now. Thanks for listening!

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

Sound effect by Alexander Jauk from Pixabay

Citation: Gardner, E. (2025), The role of a ditch in the matrix, Eos, 106, https://doi.org/10.1029/2025EO250407. Published on 31 October 2025. Text © 2025. AGU. CC BY-NC-ND 3.0
Except where otherwise noted, images are subject to copyright. Any reuse without express permission from the copyright owner is prohibited.

In Arctic Soils, Methane-Eating Microbes Just Might Win Out over Methane Makers

EOS - Fri, 10/31/2025 - 11:34

In the Arctic, a major variable for future climate change lives in the ground, invisible.

Microbes in the layers of soil just above the frozen permafrost metabolize carbon, turning it into carbon dioxide and methane, a far more potent greenhouse gas. As these soils warm, more carbon is being unlocked, potentially setting in motion a warming feedback loop sometimes nicknamed the “methane bomb.” Now, new research on the microbial denizens of Arctic soils indicates that such a vicious cycle may not be inevitable.

“It could be that these systems for a variety of reasons are not actually producing the methane we believe that they’re capable of producing.”

By cataloging the kinds of microbes found in permafrost soils from around the Arctic, as well as in recently thawed permafrost itself, a group of researchers delivered a clearer picture of microbial diversity in Arctic soils, as well as how those microbial communities change as their environment warms up. One key finding in their paper, recently published in Communications Earth and Environment, is that under certain conditions there could be more methane-eating microbes than methane-making microbes in the Arctic, meaning the soil could actually end up being a carbon sink.

“It could be that these systems for a variety of reasons are not actually producing the methane we believe that they’re capable of producing,” said Jessica Buser-Young, a microbiologist at the University of Alaska Anchorage not affiliated with the research.

The Microbes and the Methane

Since 2010, a consortium of scientists from Europe has been gathering permafrost samples in the Arctic, digging through topsoil and subsoil and into the permanently frozen ground below. Gathering these samples is difficult in the vast, remote, and frozen northern reaches of the world, but the group retrieved samples from across Canada, Greenland, and Siberia.

In the new paper, the researchers conducted genomic analyses of the microbiome of eight pan-Arctic permafrost and soil samples as well as samples of both intact and degraded permafrost near Fairbanks, Alaska. They focused specifically on microbes, comprising both bacteria and archaea, that either release or consume methane, a greenhouse gas that can be 30 times more potent than carbon dioxide.

When the researchers looked at the data, the first surprise came from the lack of diversity among both methane-producing microbes, or methanogens, and methane-consuming microbes, or methanotrophs, said study coauthor Tim Urich, a microbiologist at the University of Greifswald in Germany.

Among methanotrophs, a single genus, Methylobacter, dominated samples at every location. These bacteria are found across the Arctic, often living in soil layers just above their methanogen counterparts, consuming the methane that bubbles up from below. Why this single genus has been so successful isn’t yet known, Urich said.

The analysis “really calls for studying representatives of this specific clade in more detail to understand the ecophysiology and their response to changing conditions in the soil,” Urich said.

Possibly Defusing the Methane Bomb

Urich and his coauthors also looked at sites where permafrost had thawed, comparing wet and dry locations. The site with sodden soils held more methanogenic microbes, which thrived in the oxygen-deprived conditions. At dry sites, by contrast, methanotrophic microbes won out, especially a variety with the unique ability to take methane from the air and turn it into less potent carbon dioxide. While these facultative methanotrophs have the ability to metabolize atmospheric methane, researchers noted, they don’t necessarily do it in practice.

“It really depends on the hydrologic fate of these soils.”

Regardless, Urich said, the upshot is that a warmer, drier Arctic may be a boon for the changing climate.

“It really depends on the hydrologic fate of these soils,” he said.

If the Arctic ends up on the dry end of the spectrum, its soils could become a net sink for methane (though not a large one) as microbes begin sucking gas from the air. The mechanism described by Urich and his colleagues is not the only potential negative methane feedback loop, either. In a recent paper in AGU Advances, Buser-Young and her coauthors found that microbes in Alaska’s Copper River Delta that use iron for their metabolism have begun outcompeting those that produce methane, potentially reducing methane emissions.

“We believe that this could be happening potentially everywhere there’s glaciers in the world,” Buser-Young said.

What studies like Urich’s are making clear is that while thawing Arctic permafrost is an obvious sign of climate change, its contribution to warming is less apparent, said Christian Knoblauch, a biogeochemist at the University of Hamburg who was not involved with the research.

“We had so many papers about this methane bomb,” he said. “I think this was an oversimplification or an overestimation of methane release.”

Future of Methane Still Uncertain

Researchers are still hampered by a paucity of data about the changing Arctic.

High on Urich’s list of potentially valuable datasets are studies on the ecophysiology of the methane-associated microbes he and his colleagues found in Arctic soils. Such studies would provide more data on how microbe metabolism changes in response to warming temperatures and varying levels of oxygen, among other things.

Urich also cautioned that his research did not measure levels of methane release or uptake from Arctic soils, leaving unanswered the question of the microbes’ actual impact on the environment.

Knoblauch reiterated the need for more data, noting that we still cannot say with certainty whether the future Arctic will be more wet or more dry and therefore what methane release will look like.

“We have a lot of models, and there are a lot of simulations, but we do not have so much data on the ground,” he said. “I think the big questions are really how fast is the material decomposed, how much will thaw and in [what] time it is decomposed and then released, and how the system will be affected by changing vegetation.”

—Nathaniel Scharping (@nathanielscharp), Science Writer

Citation: Scharping, N. (2025), In Arctic soils, methane-eating microbes just might win out over methane makers, Eos, 106, https://doi.org/10.1029/2025EO250400. Published on 31 October 2025. Text © 2025. The authors. CC BY-NC-ND 3.0
Except where otherwise noted, images are subject to copyright. Any reuse without express permission from the copyright owner is prohibited.

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