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Comparative Analysis of TEC Anomalies Preceding the 2022 Cyprus and Alaska Earthquakes

Publication date: Available online 5 September 2025

Source: Advances in Space Research

Author(s): Emre Eroglu, Huseyin Bilgin, Kemal Edip, Altin Bidaj, Marsed Leti, Mario Hysenllliu

Electric Sail Guidance and Trajectory Control under Model and Environmental Uncertainties

Publication date: Available online 5 September 2025

Source: Advances in Space Research

Author(s): Lorenzo Niccolai, Marco Bassetto, Giovanni Mengali

Mass composition of cosmic rays with energy (4 – 12.5) EeV according to muon detectors of the Yakutsk EAS Array

Publication date: Available online 5 September 2025

Source: Advances in Space Research

Author(s): A.V. Glushkov, L.T. Ksenofontov, K.G. Lebedev, A.V. Saburov

Investigating Lifetime Characteristics of Low-Latitude Ionospheric F-Region Irregularities Using Single-Station GNSS Data

Publication date: Available online 5 September 2025

Source: Advances in Space Research

Author(s): YunZe Lu, Tao Yu, Yu Liang, Shuo Liu, ZuKang Dai, YiFan Qi, Yan Yu

Progress Status of the NUSES Space Mission

Publication date: Available online 4 September 2025

Source: Advances in Space Research

Author(s): M. Abdullahi, R. Aloisio, S. Ashurov, U. Atalay, F.C.T. Barbato, R. Battiston, M.E. Bertaina, E. Bissaldi, D. Boncioli, L. Burmistrov, I. Cagnoli, E. Casilli, F. Cadoux, D. Cortis, A.L. Cummings, M. D’Arco, S. Davarpanah, I. De Mitri, G. De Robertis, A. Di Giovanni

Paleoclimate patterns offer hints about future warming

Phys.org: Earth science - Mon, 09/15/2025 - 16:40
Rising carbon dioxide (CO2) levels are known to raise temperatures in Earth's atmosphere. But slow feedback processes, including heat storage in the ocean and changes in the carbon cycle, mean that sometimes, such temperature changes don't manifest right away; it can take decades, or even millennia, for Earth to reach equilibrium.

In marine forests in Northern Portugal, kelp emerges as powerful carbon storage solution

Phys.org: Earth science - Mon, 09/15/2025 - 15:18
A pioneering study led by researchers from the Interdisciplinary Center of Marine and Environmental Research (CIIMAR) and the Marine and Environmental Sciences Center (MARE) identifies seaweed forests on the northern coast of Portugal as strategic allies in carbon capture and storage.

Underwater glacier-guarding walls could have unintended consequences

Phys.org: Earth science - Mon, 09/15/2025 - 14:40
Warm water flowing into fjords and beneath ice shelves will continue to be a prime cause of glacial melting as global temperatures rise. This melting will, in turn, contribute to sea level rise and increasing inundation of coastal areas.

When does melting ice capsize? New research unearths several mechanisms

Phys.org: Earth science - Mon, 09/15/2025 - 13:50
Rising temperatures of the world's oceans threaten to accelerate the melting and splintering of glaciers—thereby potentially increasing the number of icebergs and, with it, the need to better understand more about their movement and impact. Through a series of experiments, a team of scientists has pinpointed some of the factors that cause icebergs to capsize, offering insights into how climate change may affect Earth's waters.

Paleoclimate Patterns Offer Hints About Future Warming

EOS - Mon, 09/15/2025 - 12:34
Source: AGU Advances

Rising carbon dioxide (CO2) levels are known to raise temperatures in Earth’s atmosphere. But slow feedback processes, including heat storage in the ocean and changes in the carbon cycle, mean that sometimes, such temperature changes don’t manifest right away; it can take decades, or even millennia, for Earth to reach equilibrium.

However, different climate models generate vastly different estimates of when such an equilibrium will be reached. One reason for these differences is the “pattern effect,” or the way uneven sea surface temperature changes can create distinct ocean warming patterns that affect atmospheric circulation and thus cloud cover, precipitation, and heat transfer. This complex interplay of factors can increase or decrease warming and shape the climate’s sensitivity to greenhouse gases.

One way to help predict what long-term warming patterns might look like is to turn to the past. Unearthing patterns in paleoclimate data, especially from times when Earth experienced a warmer climate, can provide insight into future warming patterns. Zhang et al. analyzed 10 million years of sea surface temperature records to determine the relative warming of different ocean regions under rising CO2 levels.

The study used the Western Pacific Warm Pool, the planet’s largest and warmest surface water body, as a reference point, comparing its sea surface temperature data with those of 17 other ocean sites to establish a global warming pattern.

The researchers then compared the warming shown in these paleoclimate data with the results of several models that simulate warming on the basis of an abrupt quadrupling of CO2 compared to preindustrial levels. They found the paleoclimate data and modeled results showed similar millennia-scale warming patterns, especially at higher latitudes. When both were compared to the past 160 years of sea surface temperature measurements, however, there were some differences in warming patterns. Modern warming is still in a transient state, influenced by ocean heat uptake, whereas the paleopattern represents the full equilibrium response.

It will take thousands of years to reach a new equilibrium, the researchers note. The study suggests that compared to the current transient warming, future warming patterns will be stronger at middle and high latitudes, including the North Pacific, North Atlantic, and Southern oceans. This high-latitude warming will likely be stronger than previous estimates suggested, and it is more pronounced in millennial-level than in century-level projections. (AGU Advances, https://doi.org/10.1029/2025AV001719, 2025)

—Rebecca Owen (@beccapox.bsky.social), Science Writer

Citation: Owen, R. (2025), Paleoclimate patterns offer hints about future warming, Eos, 106, https://doi.org/10.1029/2025EO250336. Published on 15 September 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.

El Niño May Be Driving Insect Decline in the Tropics

EOS - Mon, 09/15/2025 - 12:33

Over the course of millennia, insects, spiders, and other arthropods in tropical forests have evolved in response to natural weather cycles like the El Niño–Southern Oscillation (ENSO).

With climate change, however, these global-scale phenomena are strengthening and becoming more frequent, and arthropods are unable to adapt. In a new study published in Nature, researchers found evidence that El Niño events influenced by global warming are chipping away at the diversity and functions of arthropods in tropical forests around the world.

To understand the effect of ENSO on arthropods, researchers led by University of Hong Kong entomologist Adam Sharp extracted data from studies conducted in tropical forests that have not been commercially altered by human activity, such as Barro Colorado Island in Panama, Mount Wilhelm in Papua New Guinea, and Kibale National Park in Uganda. These datasets included samples on arthropod diversity collected for 48 different species from 35 sites.

Using that information, the researchers created a model that allowed them to identify long-term trends in the diversity of different arthropod families through El Niño events from the 1990s until 2020.

They found a general decline among all the orders they analyzed, which included spiders, beetles, butterflies, cockroaches, termites, and other bugs. The only exception was Diptera, an insect order that includes flies and mosquitoes. Diptera was the only order whose species demonstrated increasing population trends during ENSO events.

Using this model, researchers were able to predict future declines as well as document current trends. They found that the most significant losses of biodiversity would most likely be among spiders, bugs, and butterflies.

The scientists also created a separate model to identify the effects of El Niño on the ecological services provided by arthropods, such as pollination, soil health, and pest control. To do so, they gathered data from studies that measured the amount of tree litter in tropical forests and the amount of damage to plant leaves caused by herbivore arthropods.

“In the models of leaf herbivory, we saw a big decline in the amount of leaves consumed by arthropods after around the year 2000. And this correlated strongly with what we predicted for the diversity of arthropods which would probably inflict that damage,” said Sharp. The model coincided with a decline in beetles in particular, he noted.

Mismatched Life Cycles

“Every time there’s a strong El Niño event, some of that biodiversity is chipped away and it doesn’t have time to recover before the next El Niño event.”

Sharp said that both models, although designed independently, support the same conclusion: “It looks as if every time there’s a strong El Niño event, some of that biodiversity is chipped away and it doesn’t have time to recover before the next El Niño event.”

Oliverio Delgado-Carrillo, an entomologist at the Universidad Nacional Autónoma de México who did not participate in the new study, said Sharp’s findings make sense in light of his own research, which focuses on a pollinator bee species associated with Mexican pumpkin flowers.

Delgado-Carrillo contributed to a paper published earlier this year in Global Change Biology that addressed the effects of climate change on the relationship between plants and pollinators.

Delgado-Carrillo and other researchers found that in general, flowers are beginning to bloom earlier, causing a mismatch between the life cycles of pollinators and their food supply. The pumpkin flowers studied by Delgado-Carrillo, for instance, bloomed before bees emerged from the soil, limiting the time available for pollination.

Sharp agreed with Delgado-Carrillo that more severe ENSO events will most likely cause more of these temporal mismatches between arthropods and plants.

Both researchers said the consequences of the decline in arthropod diversity are hard to predict but will likely be severe and far-reaching. In addition to effects on crops that rely on pollinators, for example, scientists point out that soil health would plummet without cockroaches processing leaf litter and other organic materials that provide nutrients to tropical soils.

In addition, Delgado-Carrillo expressed concern that without insects to control their populations, some opportunistic plants benefiting from climate change might outcompete less resilient species. “Herbivores are functioning as a kind of control mechanism for all those plants that could become dominant and interfere with these ecosystem processes,” he explained.

Filling the Data Gaps

Finally, Sharp and Delgado-Carrillo agreed that more research about ENSO and arthropods in tropical forests is needed. Sharp emphasized the knowledge gap surrounding tropical Africa and Southeast Asia in particular.

Yves Basset, an entomologist from the Smithsonian Tropical Research Institute in Panama, works on what’s most likely the only long-term continuous monitoring program of arthropods in tropical Latin America. His team’s work was one of the main sources of information for Sharp’s study, although he did not directly participate in the research himself.

For Basset, financing more projects like his in all tropical forests around the world is vital for understanding the effects of human-induced climate change on arthropods, especially for cyclic events like ENSO.

—Roberto González (@perrobertogg.bsky.social), Science Writer

Citation: González, R. (2025), El Niño may be driving insect decline in the tropics, Eos, 106, https://doi.org/10.1029/2025EO250339. Published on 15 September 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.

Gravity with an “Edge”: What Lies Beneath Aristarchus Crater

EOS - Mon, 09/15/2025 - 12:00
Editors’ Highlights are summaries of recent papers by AGU’s journal editors. Source: Earth and Space Science

The surface of the Moon hides a complex and varied geology underneath. To unravel the Moon’s rich geological history, we rely on geophysical data acquired over decades of lunar missions. However, processing and interpretation of the remotely acquired data is not straightforward. Hence, new and sophisticated methods of processing and analyzing data are needed to extract the information necessary to detect and define lunar subsurface structures.

Ai et al. [2025] apply a new method combining an edge-detection algorithm, noise reduction techniques, and 3D inversion with high resolution gravity data from the Gravity Recovery and Interior Laboratory (GRAIL). The new approach allows them to sharply define the location and shape of a negative gravity anomaly beneath the Aristarchus Crater (the brightest feature on the Moon, located in Oceanus Procellarum, or “Ocean of Storms”). It confirms a complex geological setting involving crustal relief, fracturing caused by the impactor that formed the crater, dilation, and uplift of a volcanic unit. This study is important because it demonstrates a new method that will be useful to other researchers working on the Moon, and it advances our knowledge of lunar geology.  

Density contrast between subsurface masses in the subsurface of Aristarchus Crater. The distinction between negative anomaly (blue) and positive anomaly areas emerges very clearly, representing different geological processes.  The panels on the right indicate the performance of the models. Credit: Ai et al. [2025], Figure 21

Citation: Ai, H., Huang, Q., Ekinci, Y. L., Alvandi, A., & Narayan, S. (2025). Robust edge detection for structural mapping beneath the Aristarchus Plateau on the Moon using gravity data. Earth and Space Science, 12, e2025EA004379. https://doi.org/10.1029/2025EA004379

—Graziella Caprarelli, Editor-in-Chief, Earth and Space 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.

Generation of a 100-PW near-circularly-polarized attosecond x-ray pulse in the QED regime

Physical Review E (Plasma physics) - Mon, 09/15/2025 - 10:00

Author(s): Meiqi Sun, Ze Chen, Lipan Qin, Zhongyi Chen, Yan Tian, Jin Yan, Yan Wang, Xunjie Ma, Xueqing Yan, and Yunliang Wang

An ultraintense, isolated circularly polarized (CP) attosecond x-ray pulse is often required for many application of pump-probe techniques. A quantum electrodynamics (QED) effect dominated coherent synchrotron emission (CSE) regime is proposed for the generation of an ultraintense isolated, nearly C…


[Phys. Rev. E 112, 035207] Published Mon Sep 15, 2025

How the death of the dinosaurs reengineered Earth

Phys.org: Earth science - Mon, 09/15/2025 - 09:00
Dinosaurs had such an immense impact on Earth that their sudden extinction led to wide-scale changes in landscapes—including the shape of rivers—and these changes are reflected in the geologic record, according to a University of Michigan study.

A physical interpretation of Cole-Cole equations and their ambiguous time constants for Induced Polarization models

Geophysical Journal International - Mon, 09/15/2025 - 00:00
SummaryThe Cole-Cole (CC) equation was introduced as an empirical formula that in many cases matched laboratory measurements of dispersive frequency-dependent dielectric, conductive or resistive physical properties. The CC formula has four parameters, a high and low frequency limit, one of which is often normalised into a polarizability η or a chargeability m, a time constant τ and a frequency dependence c. The chargeability can be directly related to the volume fraction of polarizable material in a uniform conductive background. In an electrically resistive host, the chargeability is given by the fraction of pores blocked by sulphides or other electronically conductive polarizers in the Pelton conceptual model. Fundamentally, an electrochemical model predicts that uniformly sized, non-reactive polarizers would produce exponential or Debye decays during the return to equilibrium after excitation, while uniformly-sized, chemically-reactive materials such as sulphides should exhibit Warburg decays. Numerically, the frequency dependence c can be matched and predicted from the standard deviation of a log-normal size distribution of polarizable material. Using a simple circuit analogy, excitation by a Voltage or a Current source can produce very different decay time-constants. This analogy and mathematical analysis predict that the time constants from fitting a CC conductivity model (${{\tau }_\sigma }$) can be very different from a CC resistivity model (τρ). A published laboratory sulphide measurement example with ${{\tau }_\rho }$ = 10 days, m = 0.96 and c = 0.2 corresponds to ${{\tau }_\sigma }$ = 88 ms, or 7 orders of magnitude shorter in time. Further, the physical circuit analogy confirms the electrochemical model that while the different time constants are mathematically independent of m and c, ${{\tau }_\sigma }$ is an intrinsic time-constant fundamentally related to the grain size of polarizable material and as such a far better parameter than τρ to use for mineral discrimination studies. Published tabulations of fitted parameters need to specify c as well as the chargeability and CC time-constant to allow for transformation between conductivity and resistivity time-constants. The maximum phase time constant ${{\tau }_\phi } = \sqrt {{{\tau }_\sigma }{{\tau }_\rho }} $ is a fitting rather than experimentally measurable parameter, that is still dependent on m and c, but less dependent than ${{\tau }_\rho }$ as previously discussed in the literature.

Geodetic Observations Revealing Crustal Deformation and Tectonic Transition in the Northeastern Nam Co Region, Southeastern Tibetan Plateau

Geophysical Journal International - Mon, 09/15/2025 - 00:00
SummaryThe northeastern Nam Co region, historically impacted by significant earthquakes such as the 1951 Ms 8.0 Beng Co and 1952 Ms 7.5 Gulu events, exhibits intricate crustal deformation patterns shaped by strike-slip and extensional fault systems. This study integrates multi-source geodetic data to analyze three-dimensional deformation patterns and fault interaction. In this region, we established 16 new GNSS campaign-model observation stations. By aligning these with existing GNSS data within a unified reference frame, we obtained a high-resolution horizontal velocity field. Additionally, ascending and descending InSAR deformation velocity fields were derived utilizing Sentinel-1A data and SBAS-InSAR technology. By fusing the GNSS and InSAR velocity fields, we extracted and analyzed the three-dimensional deformation velocity field. Utilizing an enhanced back-slip dislocation model that accounts for fault dip angles, we inverted the slip behaviors of three major faults and investigated their tectonic transition patterns. The deformation field reveals distinct kinematic behaviors among these faults. Specifically, the Beng Co fault demonstrates dextral strike-slip motion, increasing from 4.8 ± 0.1 mm/yr in west to 5.4 ± 0.1 mm/yr east, accompanied by thrusting at a rate of 3.5 ± 0.1 mm/yr. Notably, the locking depths deepen eastward from 12.6 ± 0.6 km to 17.4 ± 0.8 km. In contrast, the Dong Co and northern Yadong-Gulu faults exhibit sinistral strike-slip rates of 1.0 ± 0.1 mm/yr and 4.2 ± 0.1 mm/yr, respectively, paired with maximum extensional rates of 2.0 ± 0.3 mm/yr and 5.2 ± 0.5 mm/yr. Collectively, these faults form a stable strike-slip to extension coupled system, modulating regional crustal deformation through kinematic interactions. This study quantifies a tectonic transition model, elucidating how strike-slip faulting evolves into extensional structures in central Tibetan Plateau. Our findings contribute to a deeper understanding of strain partitioning and intracontinental deformation mechanisms within the central Tibetan Plateau.

Editorial Board

Publication date: October 2025

Source: Journal of Atmospheric and Solar-Terrestrial Physics, Volume 275

Author(s):

Absorbing and scattering aerosols over semi-arid region in India: Temporal variation and possible sources

Publication date: October 2025

Source: Journal of Atmospheric and Solar-Terrestrial Physics, Volume 275

Author(s): Pawan S. Soyam, Pramod D. Safai, Shivdas Bankar, Kiran Todekar, Neelam Malap, Sunil Kondle, Pradeep Zambare, Mahendra Mane, Sanjay S. Kale, Thara Prabhakaran

Forecasting near-surface air temperature via SARIMA and LSTM: A regional time-series study

Publication date: October 2025

Source: Journal of Atmospheric and Solar-Terrestrial Physics, Volume 275

Author(s): Muhammed M. Aksoy, Md. Najmul Mowla, Mehmet Bilgili, Engin Pinar, Tahir Durhasan, Davood Asadi

Automatic Detection of Sunspots on full-disk continuum images using the MiniMax Optimization and Feature Extraction

Publication date: October 2025

Source: Journal of Atmospheric and Solar-Terrestrial Physics, Volume 275

Author(s): Madhan Veeramani, Sudhakar M.S.

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