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Sea ice melting intensifies warming and humidification of high Arctic land, study finds

Phys.org: Earth science - Mon, 11/17/2025 - 15:42
A research team has found that summer rainfall in the Arctic would increase by about 17% under 2°C global warming, approximately 16% of which is attributed to sea ice retreat. Their findings were published in Geophysical Research Letters.

Lab setup mimics Arctic erosion to find out why shorelines are crumbling

Phys.org: Earth science - Mon, 11/17/2025 - 15:18
Arctic coastlines are falling into the sea. Wave action, rising sea levels, and thawing permafrost are all contributing to the massive erosion that has forced whole towns to move farther from the water's edge.

Understanding Relative Atmospheric Roles of Anvil and In-situ Cirrus Clouds

EOS - Mon, 11/17/2025 - 14:53
Editors’ Highlights are summaries of recent papers by AGU’s journal editors. Source: AGU Advances

Cirrus clouds—the wispy, high-altitude ice clouds—are critical players in Earth’s climate. They form in two main ways: anvil cirrus spread out from large storm systems, while in-situ cirrus form on their own, high in the quiet atmosphere. Telling these two types apart on a global scale has been a long-standing challenge.

Using an innovative method that applies computer vision to satellite data, Mu et al. [2025] create the first global maps that cleanly separate these cloud types. The analysis reveals a surprising connection across the planet: powerful storm systems in one half of the world generate massive atmospheric waves that travel across the equator, significantly influencing the formation of in-situ cirrus in the opposite hemisphere.

This discovery highlights how interconnected our climate is and confirms that the two cirrus types are governed by different rules. Anvil cloud amount is driven by storm activity in its own hemisphere. In contrast, in-situ cloud formation, while dependent on local conditions, is also clearly controlled by major storms thousands of miles away. This newfound coupling is vital for climate models to accurately predict how shifting storm patterns under global warming will reshape our future climate.

Citation: Mu, Q., Ge, J., Huang, J., Hu, X., Peng, N., Li, Y., et al. (2025). A new classification of in situ and anvil cirrus clouds uncovers their properties and interhemispheric connections. AGU Advances, 6, e2025AV001919. https://doi.org/10.1029/2025AV001919

—Donald Wuebbles, 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.

Pamir Glacier Expedition Returns with High-Elevation Ice Cores

EOS - Mon, 11/17/2025 - 14:17

Central Asia’s Pamir Mountain Range contains some of the most well-preserved glaciers in the world.

Obtaining cores from a Pamir region glacier has been “almost like a holy grail for ice core scientists,” said Stanislav Kutuzov, a glaciologist at Ohio State University. But logistical challenges thwarted past attempts.

“The scientific community has been trying to take an ice core from this region for a long time.”

Last month, scientists finally did it: Between 27 September and 1 October, 13 researchers successfully drilled three ice cores from Tajikistan’s Kon Chukurbashi ice cap, a glacier 5,800 meters (19,029 feet) above sea level. Researchers expect the cores to contain ice more than 10,000 years old. The cores preserve important climate information that will help scientists better understand glacier evolution and past climate and weather patterns in central Asia.

“I’m still in disbelief that the expedition happened,” said Evan Miles, the expedition’s leader and a glaciologist at the Universität Zürich and the Universität Freiburg. “The scientific community has been trying to take an ice core from this region for a long time.”

The Tajik government formally donated the cores to the international scientific community in a 13 October ceremony. The cores are the first deep, high-elevation, uninterrupted ice archive to be collected in the Pamir region in Asia’s highlands—dubbed Earth’s “Third Pole” for its ice-, snow-, and glacier-covered landscape. 

“In the whole region of high-mountain Asia, there is not very much climate information available for longer periods into the past,” said Christoph Mayer, a glaciologist at the Ludwig-Maximilians-Universität München who was not involved in the expedition. With the core, “we can fill a really big research gap in this region,” he said. 

A Pamir Core at Last

Scientists have wanted additional glacial cores from this region both because of the region’s long-term, somewhat anomalous stability and because such cores could help them better describe the region’s weather patterns, such as the winter westerly winds that bring moisture to the Pamir range and influence the hydrology of a basin supplying water to millions of people.

Most efforts to obtain Pamir region cores targeted Vanch-Yakh Glacier (formerly Fedchenko Glacier) in Tajikistan. At about 75 kilometers (47 miles) long and more than 1,000 meters (3,281 feet) deep, Vanch-Yakh Glacier was a very desirable object of study. 

But the complex terrain surrounding Vanch-Yakh Glacier means it is extremely hard to reach. Since the 1980s, problems with helicopters, difficult-to-obtain permits, and geopolitical tensions have repeatedly thwarted scientists attempting to drill cores there.

Kon Chukurbashi provided an alternate opportunity. This glacier is accessible by road and foot, no helicopter needed.

The international expedition to Kon Chukurbashi was led by the Swiss Polar Institute’s PAMIR Project in partnership with the Ice Memory Foundation and included researchers from the Academy of Science of Tajikistan, Hokkaido University, Nagoya University, and Ohio State University; local porters; drivers; and a media team. The team left to retrieve the ice cores on 14 September.

The expedition began with a 4-day drive on the bumpy Pamir Highway, one of the world’s highest-elevation roads. Researchers required multiple days of acclimatization, first in the Tajik village of Karakul, then at a 5,100-meter-high (16,732-foot-high) base camp, to safely function at the high altitudes. The team carried roughly 1.5 tons of equipment up to the glacier.

“It’s a risky operation every time. We were fortunate.”

The expedition faced additional challenges, Miles said: There were moments when it looked as though permits might not be issued, cars broke down in the middle of nowhere, and a couple members of the team suffered from acute mountain sickness.

In the final year of funding for their project, the expedition was “make or break,” Miles said. But the team succeeded and carried three ice cores—two about 105 meters (345 feet) long and one shallow 22-meter (72-foot) core—in freezer boxes down from the glacier. They also successfully installed instrumentation to monitor the glacier’s future mass changes and completed a radar survey to determine its internal structure.

After extraction, data from the Kon Chukurbashi ice cores were logged, and researchers took notes on structural changes, dust or rock inclusions, and core quality. Credit: © Jason Klimatsas

“It’s a risky operation every time,” said Kutuzov, who was also the team’s lead driller. “We were fortunate.”

Miles and Kutuzov both said they were impressed with the way the international group was able to work together. “It is only due to the resolve and collaborative nature of our team that we managed to find ways forward and continue,” Miles said. Kutuzov found the international collaboration especially encouraging amid the current dearth of federal support for science in the United States. 

Probing the Pamir’s Climate History

The three ice cores will eventually travel to three continents for safe storage and study.

One is in the custody of the Ice Memory Foundation, an international organization aiming to collect, save, and manage ice cores from glaciers in danger of degradation or disappearance. The foundation runs a heritage collection of ice cores that it plans to store in Antarctica at Concordia Station, a French- and Italian-run research station, starting in December. (The core is currently in Japan, awaiting travel to Antarctica.) The Ice Memory Foundation provided funding that allowed the expedition team to drill multiple cores rather than one.

The Ice Memory core will be preserved for future generations of scientists who may develop techniques to gather information from the ice that today’s methods aren’t able to access. “It’s a brilliant initiative,” Mayer said.

The second deep core, also currently in Japan, is headed to Hokkaido University, where scientists will investigate long-held questions about weather and climate in central Asia.

“We have huge questions on the paleotimescale, the multiple thousands of years timescale about glaciation fluctuations across this region,” Miles said.

Evan Miles inspects a short ice core segment for rock and dust inclusions before it is packed for transport. Credit: © Jason Klimatsas

For one, the drivers behind the unique stability of the region’s glaciers compared to the rest of Asia, a phenomenon dubbed the Karakoram Anomaly, have long been a mystery to scientists. It’s clear from satellite data that the anomaly has persisted since about 1970, but scientists don’t know whether it existed before then. Glaciers in the region also have begun to show signs of melting in the past few years, also raising questions about whether the pattern is truly anomalous or simply a result of natural climate variability.

“We really lack the in situ data to understand even the mechanisms by which this anomaly has happened. We are relying almost solely on remote sensing data,” Miles said.

“We have modeling, we have reanalysis, but no actual data,” Kutuzov added. 

The new Pamir cores may be able to determine whether the anomaly has occurred in the past, as well as its possible source—one untested hypothesis posits that perhaps an increase in irrigation in the valleys below contributed to an increase in the region’s precipitation and stabilizing the glaciers, for example. “There’s a scientific puzzle,” Kutuzov said.

“Maybe [the anomaly] is a frequent thing that happens every so many decades or centuries,” Mayer said. “That would be something very interesting to understand.”

The cores will also give insight into the past climate and weather patterns governing the region, which will provide context to understand the current weather and climate dynamics that affect the region’s hundreds of millions of people.

“Society is going to have to grapple in the coming decades with rather dramatic changes to the hydrosphere, including the cryosphere. And this is, I think, where we can provide really useful information,” Miles said.

The third, shallow core also traveled to Japan after the expedition but will eventually head to Ohio State University, where it will be used to test new research methodologies.

The expedition and the research it allows honor the United Nations Decade of Action for Cryospheric Sciences and International Year of Glaciers’ Preservation.

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

17 November, 2025: This article was updated to reflect the correct date of the beginning of the expedition.

Citation: van Deelen, G. (2025), Pamir glacier expedition returns with high-elevation ice cores, Eos, 106, https://doi.org/10.1029/2025EO250427. Published on [DAY MONTH] 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.

Grandes Sequias Coincidieron con el Colapso Maya Clásico

EOS - Mon, 11/17/2025 - 14:17

This is an authorized translation of an Eos article. Esta es una traducción al español autorizada de un artículo de Eos.

Una estalagmita en una cueva de Yucatán ha proporcionado una nueva percepción del rol que la sequía puede haber jugado en los cambios sociopolíticos Mayas hace más de 1,000 años. Un análisis reciente de un proxy de precipitación en las tierras bajas Mayas reveló que varios episodios de sequía severa y prolongada durante el Período Clásico Terminal Maya (aproximadamente 800-1000 CE), un período en el que los grandes centros urbanos experimentaron cambios sociopolíticos importantes.

Los investigadores sugieren que, así como el cambio climático actúa como un multiplicador de amenazas hoy en día, la sequía puede haber amplificado los problemas existentes en los centros políticos Mayas como Chichén Itzá y Uxmal, añadiendo estrés climático a las sociedades que ya estaban bajo presión.

“Estos eventos climáticos habrían afectado a cada sitio individual de una manera muy específica dependiendo de la resiliencia de ese sitio en ese momento”, afirmó el investigador principal Daniel James, quien estudia la reconstrucción paleoambiental en la Universidad London College. “Esperamos que la precisión de este registro permita que [el análisis] se realice en sitios individuales … entonces podremos realmente comenzar a construir una imagen de lo que estoy seguro será una amplia variedad de respuestas sociales al cambio climático a lo largo del tiempo y a lo largo de la región”.

Sequías Extendidas Durante las Temporadas Húmedas

Durante el Período Clásico Terminal Maya, varias ciudades-estado Mayas en las tierras bajas del sur (en la actual México, Belice y Guatemala) experimentaron agitación sociopolítica, abandono de sitios y despoblación. Los centros políticos y culturales cambiaron hacia el norte. Aunque los cambios sociales están claros en el registro arqueológico, aún existe un debate generalizado sobre los posibles impulsores de estos cambios, así como por qué algunas ciudades-estado sobrevivieron, mientras otras no.

Este mapa de las tierras bajas Mayas en Yucatán marca sitios de estudios paleoclimáticos previos con cuadrados blancos, con el sitio de este estudio, Grutas Tzabnah, marcado con una X. Mientras que los círculos blancos denotan sitios de las Tierras Bajas del Norte Maya, y las estrellas denotan sitios de interés para este estudio. La tierra está sombreada con base en su elevación en metros sobre el nivel del mar (msnm). Los contornos azules delinean las precipitaciones totales anuales medias modeladas de 1979 a 2022, en milímetros por año. Crédito: James et al., 2025, https://doi.org/10.1126/sciadv.adw7661, CC BY 4.0

La sequía surge a menudo en estos debates como un potencial desestabilizador: las lluvias insuficientes o impredecibles pueden dar lugar a inestabilidades alimentarias, interrupciones comerciales, enfermedades e incluso conflictos militares. Sin embargo, estudios paleoclimáticos previos fallaron en precisar los momentos y la duración de las sequías en las tierras bajas Mayas durante el Período Clásico Terminal, dijo James.

James y sus colegas caminaron a una cueva llamada Grutas Tzabnah, en el estado de Yucatán, México, ubicada cerca de varios grandes sitios Mayas Clásicos, incluidos Chichén Itzá y Uxmal. Esta cueva ha sido buscada previamente para estudios de paleoclima de la región debido a su accesibilidad y las formaciones de cuevas bien conservadas. Además, Grutas Tzabnah es también una cueva relativamente poco profunda, lo que significa que el agua no tarda mucho en gotear en la cueva desde el nivel del suelo.

Los investigadores eligieron una estalagmita que ha estado creciendo por miles de años y muestra distintas capas de crecimiento anual. Esta estalagmita en particular creció rápido en las capas que datan del Período Clásico Terminal Maya, dijo James, entonces el equipo fue capaz de colectar 10-20 puntos de datos dentro de cada capa anual para determinar la precipitación subanual y estacional.

Los investigadores Daniel James (izquierda), Ola Kwiecien (centro) y David Hodell (derecha) instalan un automuestreador de agua por goteo en las Grutas Tzabnah para analizar los cambios estacionales en la química del goteo. Crédito: Sebastian Breitenbach, 2022

“Tú puedes ver temporadas húmedas y temporadas secas en nuestro registro, mientras que los registros previos de la misma cueva están viendo la precipitación media anual”, dijo James. “La precipitación de la temporada húmeda es la que determina el éxito o el fracaso de la agricultura, a diferencia del promedio anual”.

Ellos midieron la edad de las capas empleando datación radiométrica de uranio-torio y la cantidad de precipitación usando una relación isotópica estable de oxígeno, O dentro de la calcita. Las muestras de estalagmita que registraron un bajo O indican más precipitación, mientras que las O más altas indican menos precipitaciones. El equipo calibró sus cálculos paleoclimáticos con mediciones modernas de agua de lluvia y goteo de cuevas en unos pocos años para asegurarse de que podían convertir las mediciones de O de la estalagmita a precipitaciones.

De 871 a 1021, la estalagmita registró ocho sequías extremas durante las temporadas húmedas, cada una con una duración de al menos 3 años. Una sequía de 4 años que inició en 894 fue interrumpida por un solo año húmedo y fue seguida por otros 5 años de sequía de temporada húmeda. Unas décadas más tarde, la región había experimentado 13 años consecutivos de sequía en la temporada húmeda (929–942), más larga que cualquier sequía multianual de los registros históricos locales. Esta investigación fue publicada en Science Advances en agosto.

“La cronología hace de este uno de los registros de paleoclima más detallados disponibles para comprender las interacciones entre humanos-clima durante el período de colapso Maya.”

“Este nuevo estudio representa un avance significativo en nuestra comprensión de los patrones de sequía del Clásico Terminal, principalmente debido a su excepcional resolución temporal y robusto control de la edad con incertidumbres de solo unos pocos años”, dijo Sophie Warken, quien estudia los espeleotemas y variabilidad climática en la Universidad Heidelberg en Alemania y no participó en esta investigación.

“Este enfoque de alta resolución permite a los autores examinar el momento y la duración de los episodios de sequía individuales con mucha precisión, los cuales estudios previos solo pudieron identificar como amplios períodos de desecación”, agregó Warken. “La cronología hace de este uno de los registros paleoclimáticos más detallados disponibles para comprender las interacciones entre humanos-clima durante el período del colapso Maya.”

Una pieza del Rompecabezas

Mientras que este registro de precipitaciones es un gran avance, Warken dijo que le gustaría verlo verificado usando proxies adicionales como elementos traza, así como un período de calibración moderno más largo. También, a ella le gustaría ver este registro extendido antes y después del Período Clásico Terminal para evaluar si esas sequías fueron realmente excepcionales para la región.

“Estas redes paleoclimáticas ampliadas también podrían proporcionar importantes líneas de base para evaluar los cambios climáticos recientes y futuros en esta región vulnerable”, agregó ella.

A pesar de que las sequías prolongadas coinciden con los principales cambios sociales, James advirtió que esto no significa que la sequía causara estos cambios o que fuera incluso el factor más importante.

“Otras dificultades como la hambruna, la enfermedad y la violencia interna podrían haber sido causadas por la sequía o, de hecho, podrían haber existido previamente y haber hecho que la sociedad fuera más susceptible y menos preparada para las dificultades climáticas”, dijo James.

“Me encantaría que estos datos se utilicen para separar historias individuales de sitios individuales de resiliencia y supervivencia, así como también las historias de desintegración de sistemas y abandono y pérdida de población.”

Es importante destacar que la evidencia arqueológica sugiere que dos ciudades Mayas cercanas a esta cueva, Chichén Itzá y la capital regional de Uxmal, no declinaron al mismo ritmo (Uxmal declinó mucho más rápido). Comprender las presiones que experimentaron las dos ciudades, incluida la sequía, será clave para crear una imagen holística de cómo funcionaron las ciudades durante el Período Clásico Terminal.

“Mientras que el estrés climático probablemente jugó un papel importante en las transformaciones del Clásico Terminal”, dijo Warken, “la respuesta de los Mayas a la sequía fue probablemente mediada por las vulnerabilidades sociales, políticas y económicas existentes que variaron entre diferentes centros y regiones”.

“Esto podría deberse a lo bien gobernados que estuvieron, cuán rígido o flexible era su sistema político o qué tan buena era su gestión del agua en ese momento”, dijo James.

“Me encantaría que estos datos se utilicen para separar historias individuales de sitios individuales de resiliencia y supervivencia, así como también las historias de desintegración de sistemas y abandono y pérdida de población”, añadió.

—Kimberly M. S. Cartier (@astrokimcartier.bsky.social), Escritora Asociada

This translation by Solange Fiallos Ayala (@sol_fiallos_ec) was made possible by a partnership with Planeteando. Esta traducción fue posible gracias a una asociación con Planeteando.

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.

Can we tap the ocean's power to capture carbon?

Phys.org: Earth science - Mon, 11/17/2025 - 13:50
The oceans have to play a role in helping humanity remove carbon dioxide from the atmosphere to curb dangerous climate warming. But are we ready to scale up the technologies that will do the job?

Satellite imagery of the 11 November 2025 landslide at Hongqi Bridge in China

EOS - Mon, 11/17/2025 - 07:37

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

Satellite company Blacksky has released a high resolution satellite image, captured on 12 November 2025, showing the aftermath of the 11 November 2025 landslide at Hongqi Bridge in China. The image was captured by their Gen-3 instrument, and distributed via Twitter:-

The aftermath of the 11 November 2025 landslide at Hongqi Bridge in Sichuan Province, China. Image captured by Blacksky and released via Twitter.

On Reddit, there is a good short video of the site too, which includes this still:-

The aftermath of the 11 November 2025 landslide at Hongqi Bridge in Sichuan Province, China. Still from a video posted to Reddit.

This is a rock slope landslide with several metres of movement on the back scarp. Essentially the rock spur has failed. On one side (the left on the photograph above) the slope has collapsed down to the level of the lake (and probably below), whilst the main mass has a lower level of displacement (although I suspect that the failure is still through the mass to below the lake). It appears that the tunnels remain largely intact. The main part of the cantilever bridge has performed well, with the largest piers and their bridge decks remaining intact. However, the missing section is going to be very challenging to replace.

It appears that filling of the lake might have been suspended (satellite imagery shows no change in the level since the landslide occurred). One hopes that this is to allow a reappraisal of the stability of the slopes along the reservoir banks. I would be particularly concerned about those slopes that have had excavations close to the current level of the lake. There will also be some concern about the stability of this landslide. Is it possible that further filling of the lake could induce a further collapse, endangering the main bridge pillars?

Acknowledgement

Many thanks to loyal reader Alasdair for finding the image and the video.

Return to The Landslide Blog homepage Text © 2023. The authors. CC BY-NC-ND 3.0
Except where otherwise noted, images are subject to copyright. Any reuse without express permission from the copyright owner is prohibited.

Spectral induced polarization of artificial sand-clay mixtures – An experimental study supported by microcomputed tomography

Geophysical Journal International - Mon, 11/17/2025 - 00:00
SummaryEvaluating sedimentary texture is crucial for managing of aquifers and assessing groundwater quality. Direct methods of aquifer characterization (like pumping tests) are of limited value because of their invasive character and connection to boreholes, which results in scarce data networks. Non-invasive geophysical methods complement the invasive methods. Among geophysical methods, the spectral induced polarization (SIP) method, which allows measuring frequency dependent complex electrical impedance, is especially promising in this context, because it offers insights into the specific surface area (which is the proxy of the clay content), as well as into textural features of porous media (like pore-size or grain-size distributions).However, SIP data concerning sand-clay mixtures remain scarce. This lack of experimental data, in turn, hinders further development of the IP theory of clayey media. To fill this gap, we carried out a set of experiments to study SIP signatures of artificial sand-clay mixtures with varying clay content, clay types, and pore water salinity. The dataset includes nine mixtures with kaolinite or bentonite in various contents. We equilibrated each mixture with six NaCl solutions ranging in salinity from 0.1 to 30 g l−1. Based on these measurements, we first obtained the formation factor and the surface conductivity values of the samples. Then, we interpreted this dataset in terms of the real and imaginary conductivity, the formation factor, the in-phase surface conductivity, and the normalized total chargeability. Finally, based on the Debye decomposition approach, we converted the IP spectra into relaxation time distributions (RTDs) to analyse dominant relaxation times in comparison with micro-computed tomography (μCT) images.We show that the in-phase conductivity of the sand-bentonite mixtures strongly exceeds that of the sand-kaolinite mixtures with the same clay content. We attributed this difference to the higher surface conductivity of the bentonite clays. The quadrature conductivity exhibits a clear dependence on the clay type, its content, and the conductivity of the pore water. Our observations reveal that both quadrature conductivity and normalized chargeability increase with kaolinite content. However, for the bentonite samples, these parameters show maxima rather than a gradual trend. We explained this behaviour when comparing RTDs with μCT images. This comparison allowed us to identify elements of texture (sand grains coated with a thin film made of clay, clay aggregates of different sizes, clay “bridges” connecting two grains or multiple grains, etc.), which are responsible for IP of various intensities and different time constants. The size and morphology of these elements depend on the clay content, mineralogy, the clay phase topology, and pore water salinity.Ultimately, the combined application of the SIP and μCT methods to a variety of sand-clay mixtures enabled us to differentiate the samples with different clay types, contents, and water salinities. We believe that these petrophysical results can serve as the basis for SIP application to detect remotely different clay types and content, and to monitor the water salinity in clayey rocks, soils, and sediments.

3D Geoelectrical Imaging Beyond 1 km Depth for Mineral Exploration: Framework of Deep Electrical Resistivity Tomography and Induced Polarization with Advanced Strategies

Geophysical Journal International - Mon, 11/17/2025 - 00:00
SummaryDirect Current Electrical Resistivity Tomography (ERT) is a widely used geophysical method for near-surface investigations, offering high-resolution imaging for geological, engineering, and environmental applications. While traditional ERT surveys typically target depths of 0–200 m, technological advancements have enabled deeper investigations, commonly referred to as Deep ERT. In this study, we explore the practical challenges and methodological improvements associated with Deep ERT, particularly when combined with Induced Polarization (IP) measurements. Rather than other electromagnetic methods, ERT offers a more straightforward framework for analyzing IP effects, which can potentially correlate with the volume fraction of ore minerals. Nevertheless, deep IP investigations are often challenged by weak signal strength and various sources of electromagnetic interference. To address these challenges, we evaluated key strategies including survey planning, high-power current injection, unconventional electrode configurations, and advanced signal processing techniques. The adoption of nodal geophysical recording systems eliminates the logistical constraints of cabled multi-electrode setups, improving flexibility and data acquisition efficiency. Additionally, continuous full time-series recording allows for enhanced noise filtering and signal stacking, ultimately increasing the signal-to-noise ratio and extending the effective exploration depth. We demonstrate this methodology through a comprehensive case study conducted at the Koillismaa Linear Intrusion Complex in Finland, where a 3D Deep ERT-IP survey successfully delineated conductive and chargeable anomalies at depths exceeding 1.5 km. These anomalies closely align with independent gravity and borehole logging data, consistent with the mafic-ultramafic intrusion structures. Our results emphasize the importance of balancing data quality, survey efficiency, and spatial resolution in survey design. This work not only provides a robust workflow for the implementation of Deep ERT-IP surveys but also represents the first documented successful acquisition of high-quality IP data at these substantial depths, significantly advancing the state of deep geoelectrical exploration.

A Time-Space and Frequency-Wavenumber Dual-Domain Fusion Network for Coupling Noise Separation

Geophysical Journal International - Mon, 11/17/2025 - 00:00
SummaryDistributed Acoustic Sensing (DAS) technology has gained widespread attention in seismic exploration due to its high spatial resolution and low deployment cost. However, the presence of coupling noise in DAS data significantly affects the accurate extraction and interpretation of seismic signals. Coupling noise typically appears as narrowband stripe-like or zigzag-like interference and shares similar characteristics with seismic signals in the time-space (T-S) domain, making it challenging for traditional denoising methods to achieve effective signal-noise separation without residual noise or signal leakage. To address these challenges, this paper proposes a deep learning-based dual-domain fusion approach that integrates both T-S and frequency-wavenumber (F-K) domain information to enhance the accuracy of coupling noise separation. The method leverages the narrowband characteristics of coupling noise in the F-K domain while incorporating spatiotemporal information from the T-S domain to achieve cross-domain feature fusion, thereby improving the separability between signals and coupling noise. Experimental results demonstrate that the proposed method significantly improves coupling noise suppression performance on both synthetic and field DAS vertical seismic profile (VSP) data while minimizing signal leakage. Furthermore, in corridor stacking experiments, the method effectively reduces the impact of coupling noise on seismic interpretation, improving the reliability of subsurface formation analysis. Compared to conventional F-K filtering, single-domain network and denoising diffusion model, the proposed approach achieves superior performance in terms of coupling noise suppression and signal amplitude preservation.

A theoretical model for electrical conductivity of a weakly transversely isotropic porous medium with two conducting phases

Geophysical Journal International - Mon, 11/17/2025 - 00:00
SummaryElectrical properties of porous media consisting of solid and fluid phases have been continuously investigated in the study of geomaterials given their strong link to pore space characteristics (e.g. pore size and connectivity). Over the past decades, numerous theoretical models have been developed to determine the electrical conductivity of the porous media as a function of conductivities of their constituents and their relative proportions. In this paper, we present a new theoretical model to calculate the electrical conductivity of a weakly transversely isotropic (TI) porous medium with two conducting phases. We first use the well-established series and parallel electrical connections, together with a newly introduced coefficient g, to construct a conductive cell that represents the porous medium’s microscopic structure. We then obtain the macroscopic weakly TI conductivity stacking these cells in one dimension. We innovatively introduce a normal probability distribution to simulate the distribution of porosities across cells. Good agreement between our theoretical predictions and literature data validates the model for weakly TI porous media. We also show that series and parallel connections of the solid and liquid phases provide reliable building blocks for more advanced models, and that using a normal distribution to simulate electrical anisotropy in quasi-isotropic or weakly TI porous media is viable. Finally, we use the model to study the effects of key variables on weakly TI conductivity. We find that increasing the coefficient g reduces electrical conductivity and that the Electrical Anisotropy Coefficient (EAC) attains its maximum at 50 per cent porosity in weakly TI porous media with two conducting phases.

Multifractal Insights into Mid-Latitude Atmospheric and Solar Dynamics Across Different Solar Cycle Phases

Publication date: Available online 9 November 2025

Source: Advances in Space Research

Author(s): Mahdi Momeni, Yenca Migoya-Orué

Computationally Efficient Distributed Model Predictive Control of Satellite Swarms

Publication date: Available online 7 November 2025

Source: Advances in Space Research

Author(s): Junyu Chen, Baolin Wu, Zhaobo Sun

Proposing a Novel Optimized Dynamic Sampling Approach for Enhancing Land Use Classification and Projection Accuracy

Publication date: Available online 7 November 2025

Source: Advances in Space Research

Author(s): Ali Haji Elyasi, Mohsen Nasseri, Peyman Badiei

Enhancing Temperature Data Analysis Through Threshold-Optimized Ensemble Detection(TOED) Approach of Climate Anomalies

Publication date: Available online 7 November 2025

Source: Advances in Space Research

Author(s): K. Kanishkar, J. Rufina Sherin, L. Gowri

Determination, estimation and modeling of satellite-induced code bias for BDS GEO Satellites and its impact on wide-lane UPD estimation and wide-lane ambiguity resolution

Publication date: Available online 7 November 2025

Source: Advances in Space Research

Author(s): Jinwen Zeng, Xiufeng He, Wei Zhan, Haijun Yuan, Jinsheng Tu

Seismo-Ionospheric Anomalies Associated with the 2025 Mw 7.7 Myanmar Earthquake: A Case Study

Publication date: Available online 7 November 2025

Source: Advances in Space Research

Author(s): Siva Sai Kumar Rajana, Sambit Prasanajit Naik, Sampad Kumar Panda, Chiranjeevi G Vivek, Sridevi Jade

Satellites play critical role in tracking climate adaptation, researchers say

Phys.org: Earth science - Fri, 11/14/2025 - 18:29
Satellite-based Earth observation provides a unique and powerful tool in tracking climate adaptation, an international study involving University of Galway researchers has shown.

Offsetting blue carbon benefits: Mangrove tree stems identified as previously underestimated methane source

Phys.org: Earth science - Fri, 11/14/2025 - 16:16
Mangrove ecosystems rank among the most efficient "blue carbon" systems on Earth, capable of absorbing and storing vast quantities of atmospheric carbon dioxide (CO2). However, mangroves also release methane (CH4), a potent greenhouse gas, potentially offsetting a portion of their climate mitigation benefits.

Lab Setup Mimics Arctic Erosion

EOS - Fri, 11/14/2025 - 14:26
Source: Journal of Geophysical Research: Earth Surface

Arctic coastlines are falling into the sea. Wave action, rising sea levels, and thawing permafrost are all contributing to the massive erosion that has forced whole towns to move farther from the water’s edge.

To understand how these forces combine to bring down cliffs, Omonigbehin et al. created a microcosm of an Arctic coastline in a lab. First, the researchers mimicked soil containing permafrost by mixing water and sand in ratios designed to maximize the density of the sand, then compacting the mixture with a hydraulic press and freezing it. The researchers pummeled these blocks of faux permafrost with water in a cooled wave flume, a long and narrow tank in which waves are generated so researchers can observe their effects. In this study, the scientists varied the wave height and frequency to see how the permafrost would respond.

The method reproduced observed patterns of erosion that hollow out the bases of coastal bluffs. Wave height had the strongest influence on the rate of erosion, with the highest-wave conditions causing twice as much erosion as low-wave conditions. Wave frequency, on the other hand, strongly influenced the height of the notch carved out by the waves.

When the researchers increased the ice content in the soil by adding more water prior to freezing, they found that the higher ice content decreased the initial erosion rate (because the ice took longer to thaw). This finding suggests that coastlines with higher ice content that currently appear stable may not see high erosion rates in the immediate term but could erode abruptly if the current global warming rate is sustained—a finding that’s consistent with the theory that climate change will trigger tipping points. However, the researchers caution that more research is needed to confirm this finding. (Journal of Geophysical Research: Earth Surface, https://doi.org/10.1029/2025JF008528, 2025)

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

Citation: Sidik, S. M. (2025), Lab setup mimics Arctic erosion, Eos, 106, https://doi.org/10.1029/2025EO250422. Published on 14 November 2025. Text © 2025. AGU. CC BY-NC-ND 3.0
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