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Defunct Pennsylvania oil and gas wells may leak methane and metals into water

Phys.org: Earth science - Fri, 11/07/2025 - 23:20
In the dense forests of northwestern Pennsylvania, hundreds of thousands of retired oil and gas wells—some dating back to the mid-1800s, long before modern construction standards—dot the landscape, according to geochemists in Penn State's College of Earth and Mineral Sciences who recently led a study in the region. Left uncapped and exposed to air and erosion, they break down, leaching harmful chemicals into the atmosphere and, the researchers reported, into the groundwater.

Flagged data of the Langmuir probes onboard Swarm satellites related extremely low plasma density environment

Publication date: Available online 5 November 2025

Source: Advances in Space Research

Author(s): Yuhao Zheng, Chao Xiong, Gaofang Mi, Yuanqiang Zhao, Ziyuan Zhu, Artem Smirnov, Rui Yan

Why measuring land-use carbon emissions is so challenging—and how to fix it

Phys.org: Earth science - Fri, 11/07/2025 - 18:00
A team led by LMU researchers shows why CO₂ fluxes from land use are so difficult to quantify—and how they can be estimated more accurately in the future.

Enhancing ocean wind observation accuracy: New rain correction approach for FY-3E WindRAD

Phys.org: Earth science - Fri, 11/07/2025 - 17:58
Satellite scatterometers play a crucial role in monitoring ocean surface winds, with their accuracy directly impacting weather forecasting and climate research. However, rainfall has consistently challenged precise wind measurements, as Ku-band radar signals are much affected by rain clouds.

Cracks in Antarctic 'Doomsday Glacier' ice shelf trigger accelerated destabilization

Phys.org: Earth science - Fri, 11/07/2025 - 14:42
Thwaites Glacier in West Antarctica—often called the "Doomsday Glacier"—is one of the fastest-changing ice–ocean systems on Earth, and its future remains a major uncertainty in global sea-level rise projections. One of its floating extensions, the Thwaites Eastern Ice Shelf (TEIS), is partially confined and anchored by a pinning point at its northern terminus.

Safety Device Supplies Life-Saving Air in an Avalanche

EOS - Fri, 11/07/2025 - 14:21

A new medical study simulated an avalanche in the Italian Alps, demonstrating the life-saving power of a new portable fan system.

The Safeback SBX device weighs 18 ounces, fits into a backpack or vest, and draws oxygen from snowpack’s natural porosity to extend survival. While other safety tools—like emergency beacons and airbags—can make it easier to find someone in an avalanche, the Safeback SBX extends the time a person can survive while waiting for rescue.

“This is the biggest innovation in avalanche safety devices in 25 years.”

In a recent study in the Journal of the American Medical Association (JAMA), the Safeback SBX helped buried victims breathe under the snow for at least 35 minutes. That’s a critically important window. Roughly two thirds of people asphyxiate within 30 minutes of avalanche burial.

“This is the biggest innovation in avalanche safety devices in 25 years,” said Giacomo Strapazzon, an adjunct professor of emergency medicine at the Università degli Studi di Padova and lead author of the study.

Simulating an Avalanche

Strapazzon led the study for the Institute of Mountain Emergency Medicine at the private research center Eurac Research. While the makers of Safeback SBX proposed the study, the research team maintained independence.

To study the efficacy of the device, researchers first needed to bury willing victims. They put out a call for volunteers, screening potential participants for claustrophobia before bringing them to the mountains. They recruited 36 participants, ultimately using 12 men and 12 women, a gender balance celebrated in a separate JAMA editorial for addressing the “severe underrepresentation of females” in high-altitude physiology tests.

The test took place in a mountain pass, 2,000 meters above sea level in the Dolomite range in northeastern Italy. Participants were buried face down under 50 centimeters of high-density snow (500 kilograms per cubic meter) while wearing a Safeback SBX.

In an avalanche, the main cause of death is asphyxiation from lack of oxygen. But snow is naturally porous, up to 67% air even at a density of 300 kilograms per cubic meter. The Safeback SBX uses a large fan to suck oxygen-rich air from the snow behind a victim. It delivers up to 150 liters of air per minute toward the user’s face via shoulder strap tubes. The device works with the company’s backpacks and vests and can be activated before entering avalanche terrains. The equipment is cold weather tested, with a battery lasting at least 60 minutes even at −30°C.

During the test, half the participants received a functioning device that switched off after 35 minutes. The other half received a sham device. Participants were buried one at a time, while a gang of puffy-coat-clad medical professionals monitored their vital statistics from the surface.

The Safeback SBX successfully extended survival time. Of the 12 participants buried with a sham device, only one lasted 35 minutes. Seven had to be rescued after their pulse oximetry, or the level of oxygen in the blood, dipped below the study threshold of 80%. The other four requested an early rescue by radio. Average burial time was 6.4 minutes under the snow.

Of the 12 people buried with a functioning device, 11 lasted the full 35 minutes. Only one requested an early rescue. When the functioning devices were switched off after 35 minutes, participants lasted an average of 7.2 minutes. Five requested rescue, and six required it after their pulse oximetry dropped below 80%.

Winter Work

The device could be valuable for anyone who works and recreates in avalanche terrain, including Earth scientists.

Peter Veals is an atmospheric scientist at the University of Utah. His lab group deploys atmospheric gauges in the Wasatch Mountains each year before the snow falls. But winters are long, and equipment needs maintenance. His team may ski 30 minutes over 4.5 meters (15 feet) of snow to knock icicles off a heated radar dish before a storm starts.

His lab group uses a detailed safety plan, but it’s difficult to avoid avalanche terrain completely, he said. By extending the rescue time, the Safeback SBX has clear value in the mountains.

“Those are some brave volunteers.”

“There’s probably a lot of people that get there a minute too late,” Veals said of avalanche rescues. “Extending [survival time] by 20 minutes plus is a huge deal.”

Other factors affect survivability. People in an avalanche may strike a tree or boulder. Deeper, denser snow would delay a rescue. Preventive measures like avalanche training and education are still essential.

“All those factors mean this isn’t a silver bullet, but I think it is still a huge step forward,” Veals said of the device.

The study did a great job mimicking the conditions of an avalanche, he noted.

“I thought it was as applicable as you could get to the actual situation,” Veals said. “Those are some brave volunteers.”

—J. Besl (@jbesl.bsky.social), Science Writer

Citation: Besl, J. (2025), Safety device supplies life-saving air in an avalanche, Eos, 106, https://doi.org/10.1029/2025EO250418. Published on 7 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.

As global climate action threatens to stall, can Australia step up at COP30 in Brazil?

Phys.org: Earth science - Fri, 11/07/2025 - 11:37
Ten years on from the landmark Paris Agreement, countries have taken big strides in limiting emissions and the clean energy transition is accelerating rapidly. But geopolitical headwinds are growing and the damage bill for climate pollution is rising. Climate action hangs in the balance.

Antarctic ice melt triggers further melting: Evidence for cascading feedbacks 9,000 years ago

Phys.org: Earth science - Fri, 11/07/2025 - 10:00
A study has revealed that the substantial retreat of the East Antarctic Ice Sheet (EAIS) approximately 9,000 years ago was driven by a self-reinforcing feedback loop between ice melt and ocean circulation.

The 4 November 2025 landslide at Mae Moh Mine in Thailand

EOS - Fri, 11/07/2025 - 08:39

A landslide in coal waste covering about a square kilometre was triggered by heavy rainfall.

At about 4 am on 4 November 2025, a very large landslide occurred in a coal waste pile at the Mae Moh Mine in Thailand. This is an extremely large coal mining site that is co-located with electricity generating plants.

The landslide itself is very large. EGAT, the owner of the powerplant at the site, has released this image of the aftermath of the failure:-

The 4 November 2025 landslide at Mae Moh Mine in Thailand. Image released by EGAT.

It appears that the landslide occurred in Mae Moh 8 Project area, and that it damaged the offices of Sahakol Equipment Co. Ltd. Google Maps places both of these elements in the area of [18.34735, 99.70067], but the precise location of the landslide is unclear. We will need to wait for a cloud-free day to pin this down more precisely.

News reports indicate that movement was first detected on about 31 October 2025, and that heavy rainfall over the following days led to the failure. The main body of the landslide appears to be mainly translational, although there may be a rotational component in the head scarp area. Displacement near to the crown appears to be several tens of metres at least.

The lowest portions of the landslide have a flow type of mechanism. There may be some pipes on the slope on the right side of the image – it would be interesting to know if these have fed water into the slope.

Newspaper reports cover a statement to the Stock Exchange of Thailand by Sahakol Equipment Public Company Limited:-

“EGAT has declared a state of emergency in the area and has cordoned off the area for safety reasons, forcing the company to temporarily halt work on the Mae Moh 8 project. From a preliminary investigation, the company’s damaged assets include some office buildings and maintenance facilities, some of the Mae Moh 8 project’s soil conveyor belt structures, and other operating machinery.”

This is not the first such failure at Mae Moh mine. In a paper in the journal Engineering Geology, Hoy et al. (2024) describe a 1.2 km long waste dump failure on 18 March 2018. The landslide looks to have been remarkably similar to the event this week.

Reference

Hoy, M. et al. 2024. Investigation of a large-scale waste dump failure at the Mae Moh mine in Thailand. Engineering Geology, 329, 107400. https://doi.org/10.1016/j.enggeo.2023.107400

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A quasi-2D model of dike propagation with non-equilibrium magma crystallization

Geophysical Journal International - Fri, 11/07/2025 - 00:00
SummaryMagma transport in dikes is usually modelled by means of lubrication theory, assuming that magma properties are uniform across the dike. We explore the influence of cross-dike temperature heterogeneity on the dynamics of dike propagation using a quasi-2D model, derived from a full 2D model with an assumption of small width to length ratio. The model couples elastic fracture mechanics with multiphase magma flow, solving the governing equations using a hybrid numerical approach that combines the Displacement Discontinuity Method for elasticity with finite volume discretization for fluid flow and heat transfer. The model includes heat exchange with wall rocks, shear heating and latent heat release. It accounts for non-equilibrium magma crystallization, implementing temperature-dependent crystallization kinetics using an Arrhenius formulation for the relaxation timescale. As a case study, we simulate the ascent of a volatile-rich dacite from a source at 30 km depth. The distribution of temperature, crystallinity, and, thus, viscosity across the dike leads to a plug-like velocity profile with magma stagnation near the walls, substantially different from the parabolic Poiseuille flow assumed in classical lubrication theory. With temperature-dependent crystallization rate, rapid cooling of magma near the dike walls can generate a glassy chilled margin. The adjacent magma has higher crystallinity due to intermediate cooling rates, while the hotter core remains depleted in crystals throughout dike propagation. The dike propagates further and is thinner than predicted by (1D) lubrication theory because the low-viscosity core continues to facilitate vertical transport while the wall zones become progressively more viscous due to cooling and crystallization. The latent heat of crystallization can have a substantial impact in slowing down cooling and prolonging propagation. Other important factors include the characteristic crystal growth time, initial magma temperature and water content. Our quasi-2D approach bridges the gap between oversimplified 1D models and computationally expensive 3D simulations, providing a practical framework for investigating magma transport in silicic dikes.

Enigmatic Seismic Excitation of the 1957 Andreanof, Aleutian Is., Earthquake

Geophysical Journal International - Fri, 11/07/2025 - 00:00
SummaryThe 1957 Andreanof, Aleutian Is., earthquake (1957 March 9, 51.53°N, 175.63°W, d=25 km) is among the most enigmatic great earthquakes instrumentally recorded. The length of the aftershock area is very long (about 1,200 km), and tsunami excitation has been recently confirmed to be very extensive, yet its instrumental seismic magnitude Ms is only about 8.1 to 8.3. Detailed analyses of long-period surface waves in the past gave an Mw=8.4, and the seismic-tsunami disparity remains unresolved. The main difficulty in seismic studies is the absence of high-quality seismic data. Here we investigate the cause of this disparity by carefully analyzing some historical seismograms with modern digitization methods. We also take advantage of the 1996 Aleutian Is. earthquake (Mw=7.87) that occurred very close to the 1957 event. For the 1996 event, high-quality modern broad-band seismograms are available which can be effectively used as empirical Green’s functions for the analysis of the 1957 event. Using the Wiechert (Strasbourg, Uppsala), Milne-Shaw (Wellington), and Benioff (Uppsala, Pasadena) seismograms of the 1957 event, we could determine that the 1957 event had significant secondary excitation of long-period (150 s) waves during about 1,000 s following the first event. The Mw of the combined source is approximately 8.4. Because of the limited bandwidth of the old instruments, we cannot detect long-period energy beyond 150 s. However, the unusually long-lasting excitation over nearly 1,000 s suggests that the event had significant excitation at periods longer than 150 s with a much larger Mw for the total event. Although we cannot address this question quantitatively because of our band-limited data, our numerical experiment using a source with a slow component shows that if the time scale of the slow source is longer than 500 s, our data can be made compatible with an Mw =8.8 to 8.9 event, thereby reconciling the results from seismic and tsunami data.

Mapping a new frontier with AI-integrated geographic information systems

Phys.org: Earth science - Thu, 11/06/2025 - 21:06
Over the past 50 years, geographers have embraced each new technological shift in geographic information systems (GIS)—the technology that turns location data into maps and insights about how places and people interact—first the computer boom, then the rise of the internet and data-sharing capabilities with web-based GIS, and later the emergence of smartphone data and cloud-based GIS systems.

What really happened on Easter Island? Ancient sediments rewrite the 'ecocide' story

Phys.org: Earth science - Thu, 11/06/2025 - 19:50
A new study led by researchers at the Lamont-Doherty Earth Observatory offers the clearest evidence yet that a centuries-long drought transformed life on Rapa Nui (Easter Island) beginning around the year 1550.

Asian summer monsoon's unusual role in 2021 Pacific Northwest heat wave revealed

Phys.org: Earth science - Thu, 11/06/2025 - 19:10
In recent years, as extreme weather events have occurred with increasing frequency, scientists have been searching within the chaotic atmospheric system for clues that can enhance forecasting capabilities—factors such as ENSO, sea ice, the stratospheric polar vortex, and tropical convective activity. These factors provide critical basis for weather and climate predictions across different time scales.

Space dust reveals Arctic ice conditions before satellite imaging

Phys.org: Earth science - Thu, 11/06/2025 - 19:00
Arctic sea ice has declined by more than 42% since 1979, when regular satellite monitoring began. As the ice grows thinner and recedes, more water is exposed to sunlight. Ice reflects sunlight but dark water absorbs it, advancing warming and accelerating ice loss. Climate models indicate that the Arctic will see ice-free summers within the coming decades, and scientists still aren't sure what this will mean for life on Earth.

In the US, Western rivers may be allies in the fight against climate change

Phys.org: Earth science - Thu, 11/06/2025 - 19:00
For decades, scientists have generally thought that rivers emit more carbon dioxide, a greenhouse gas, than they take in. But a new analysis of every river network in the contiguous United States—including underrepresented rivers in deserts and shrublands—challenges this assumption, uncovering hints that many Western waterways may be soaking up carbon dioxide from the atmosphere.

Arizona's Willcox basin is sinking fast due to groundwater extraction

Phys.org: Earth science - Thu, 11/06/2025 - 17:40
In Arizona's Willcox Basin, just over an hour east of Tucson, fissures are tearing through the earth, wells are running dry, and strange areas are flooding when it rains. The cause is clear. As large agricultural producers pump more and more groundwater for irrigation, the water table is falling, and the land surface itself is sinking.

Marine Heatwaves Reshape Precipitation Patterns

EOS - Thu, 11/06/2025 - 15:11
Editors’ Highlights are summaries of recent papers by AGU’s journal editors. Source: Journal of Geophysical Research: Atmospheres

Marine heatwaves (MHWs)—prolonged periods of unusually warm ocean temperatures—are intensifying globally, disrupting marine ecosystems and biological processes. While their impacts on marine life are better documented, how MHWs influence precipitation has remained largely unexplored.

Zeng et al. [2025] investigate the relationship between MHWs and precipitation using two decades of high-resolution observational and reanalysis data (2002–2021). On average, MHWs shift global mean precipitation anomalies from −1.69 mm/day before peak intensity to +2.82 mm/day afterward. The study further identifies four distinct MHW types based on precipitation anomalies before and after the peak. The most common type (~46%) features reduced precipitation throughout its lifetime, followed by events (~26%) where precipitation transitions from negative to positive. In these latter cases, warmer early-stage oceans enhance evaporation and moisture convergence, increase moist static energy, and trigger stronger rainfall after the peak, which blocks solar radiation and accelerates MHW decay.

Understanding these dynamical processes is crucial for predicting future climate extremes in a warming world. This is among the first studies to identify precipitation–MHW relationships at different stages based on observations. These findings reveal dynamic air-sea feedbacks, showing that MHWs not only affect marine ecosystems but also modify regional precipitation patterns.

Citation: Zeng, S., Dong, L., Wu, L., Song, F., Zhang, Z., & Jing, Z. (2025). Distinct impacts of different marine heatwaves on precipitation. Journal of Geophysical Research: Atmospheres, 130, e2025JD044381. https://doi.org/10.1029/2025JD044381

—Yun Qian, Editor, JGR: Atmospheres

Text © 2025. The authors. CC BY-NC-ND 3.0
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What Tumbling Asteroids Tell Us About Their Innards

EOS - Thu, 11/06/2025 - 14:18

Asteroids are primordial pieces of our solar system’s history, but they aren’t exactly pristine relics. Their surfaces in particular are eroded by solar radiation and pockmarked with meteorite impacts. Detailed studies of asteroids’ interiors are also lacking, simply because very few probes have been able to study them up close.

However, a promising new study uses data from the Gaia space observatory to understand the links between asteroid tumbling behavior, collision history, and interior structure. The key to the study is the discovery that rotation speeds of asteroids in the main belt, between Mars and Jupiter, don’t follow a random distribution.

When rotation period is plotted against asteroid size, asteroids fall into two distinct populations: slow spinners, which take more than about 24 hours to complete a rotation, and fast spinners, whose rotations take less than 24 hours. Small asteroids are more likely than large ones to be slow spinners.

“People found an excess [of] faster rotating asteroids and also an excess [of] slow rotating asteroids,” with fewer asteroids rotating at a medium speed, said Wen-Han Zhou, a planetary scientist at the University of Tokyo. In his Ph.D. research at the University of Nice, he and his collaborators realized that many of the slow rotators were also tumbling: rotating chaotically, rather than spinning steadily along a clearly defined axis.

“Asteroids are not islands in space; they collide with each other.”

“Asteroids are not islands in space; they collide with each other,” Zhou said. “When an asteroid spins very slowly, a tiny collision can make it tumble. This [also] tumbles the materials inside, which will dissipate the energy.”

This dissipation effect comes from internal friction. In their recent Nature Astronomy article, Zhou and his colleagues linked an asteroid’s rate of rotation, whether it is tumbling or spinning smoothly, its size, and its internal structure into a single theoretical framework. In this theory, fast rotating asteroids are stable spinners because any collision that sends them tumbling also jumbles their innards, causing internal friction that dissipates the chaos and brings the asteroids back to stability. Slow spinners, however, lock into tumbling chaotically because their guts don’t jumble enough to dissipate the energy.

“In my research, I propose slow rotators are all tumbling,” Zhou said. “This is a very strong statement, but so far it is consistent with observation.”

Zhou and collaborators also concluded that these slow tumblers are all rubble-pile asteroids: loose aggregates of small chunks barely held together by mutual gravitation, rather than being monolithic hunks of rock. This has implications for planetary defense.

“Imagine a bunch of pieces of Styrofoam stuck together with cohesive forces. You try to disrupt that, good luck!” said Alessondra Springmann, an asteroid researcher based in Colorado. Springmann has studied near-Earth asteroids using radar at the Arecibo Observatory in Puerto Rico but was not involved in this new research.

Knowing more “about an asteroid’s internal properties can help us if it ever came time to redirect an asteroid away from Earth.”

Scientists have tried. They found that smashing a projectile into a rubble pile, like NASA’s Double Asteroid Redirection Test (DART) mission did to the near-Earth asteroid Dimorphos, might not destroy it. The asteroid might simply re-form itself after being smashed. (Notably, Dimorphos is much smaller than the main belt asteroids in Gaia’s data.) Radar data on its rotation could tell planetary defenders what methods are useful well in advance. But so, too, could learning more about an asteroid’s innards.

Knowing more “about an asteroid’s internal properties can help us if it ever came time to redirect an asteroid away from Earth,” Springmann said.

You Spin Me Round

The European Space Agency’s Gaia observatory was built primarily to map the Milky Way. Because it provided a sensitive wide-angle view of the whole sky, the observatory also incidentally provided data on other objects, including asteroids in the main belt of our solar system. To determine asteroid spin rates, asteroid researchers turned to Gaia data showing how reflected light varies over time as the objects spin. This is when they found the clear division between fast and slow rotators.

Scientists have a reasonable explanation for the behavior of the fastest spinners: the YORP effect (for Yarkovsky-O’Keefe-Radzievskii-Paddack). In essence, asteroids receive sunlight across their surface facing the Sun, but their uneven surfaces absorb and reemit that light in more or less random directions. Over many millions of years, that accumulated difference in light exposure can cause asteroids to spin until they reach the spin barrier of one rotation every 2.2 hours, at which point they break into pieces if they’re rubble piles.

But slow rotators defied easy explanation.

However, Gaia provided another clue: If the variations in light it measured were regular, then the asteroid was a stable spinner. If they were irregular, then the asteroid was tumbling. Many slow spinners were tumbling, whereas almost every fast rotator was stable.

Zhou and his collaborators realized that if most or all slow spinners are tumblers, it could explain why observed asteroids are split into two distinct populations. Asteroids are too faint for even Gaia to clearly distinguish between rotators and tumblers in every case, but when the researchers simulated main belt asteroids on a computer—including the effects of collisions and YORP—they produced something strikingly similar to the Gaia data.

Along the way, the researchers also realized tumbling behaviors are linked to possible internal structural properties, particularly deformability and internal friction, which are not typically measurable without placing a seismometer on an asteroid’s surface. In other words, these analyses could actually reveal the life history and internal properties of asteroids in new ways.

—Matthew R. Francis (@BowlerHatScience.org), Science Writer

Citation: Francis, M. R. (2025), What tumbling asteroids tell us about their innards, Eos, 106, https://doi.org/10.1029/2025EO250414. Published on 6 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.

古气候模式为未来变暖提供线索

EOS - Thu, 11/06/2025 - 14:18
Source: AGU Advances

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

众所周知,二氧化碳(CO2)浓度上升会导致地球大气温度升高。但缓慢的反馈过程,包括海洋的热量储存和碳循环的变化,意味着这种温度变化有时不会立即显现;地球可能需要数十年甚至数千年才能达到平衡。

然而,不同的气候模型对于何时达到这种平衡的预测却大相径庭。造成这些差异的原因之一是“模态效应”,即海面温度的不均匀变化会形成不同的海洋变暖模式,进而影响大气环流,最终影响云量、降水和热量传递。这些因素之间的复杂相互作用会加剧或减缓变暖,并影响气候对温室气体的敏感性。

帮助预测长期变暖模式的一种方法是回顾过去。挖掘古气候数据中的模式,特别是来自地球气候温暖时期的数据,可以为未来的变暖模式提供线索。刘小庆、张一歌等人分析了过去1000万年的海洋表面温度记录,以确定在二氧化碳浓度上升的情况下,不同海洋区域的相对升温情况。

该研究以地球上最大、最温暖的表层水体——西太平洋暖池为参考点,将其海表温度数据与其他17个海洋站点的海表温度数据进行比较,从而建立全球变暖模式。

随后,研究人员随后将这些古气候数据中显示的升温情况与几个模拟模型的结果进行比较,这些模型模拟了二氧化碳浓度相对于工业化前水平突然增加四倍的情况。他们发现,古气候数据和模型结果显示出相似的千年尺度升温模式,尤其是在高纬度地区。然而,当两者与过去160年的海表温度测量数据进行比较时,升温模式出现了显著的差异。受海洋热吸收的影响,现代升温仍处于过渡状态,而古气候模式则代表了完全的平衡响应。

研究人员指出,要达到新的平衡需要数千年的时间。该研究表明,与目前的瞬时气候变化相比,未来在中高纬度地区,包括北太平洋、北大西洋和南大洋的升温模式将更为显著。这种高纬度地区的升温幅度可能超过之前的估计,并且在千年尺度上的预测比在百年尺度上的预测更为明显。(AGU Advances, https://doi.org/10.1029/2025AV001719, 2025)

—科学撰稿人Rebecca Owen (@beccapox.bsky.social)

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

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