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Impact of spatial and temporal resolution of satellite sea surface salinity measurements on ocean state prediction in the Tropical Indian Ocean; an OSSE framework using SMOS

Publication date: Available online 4 November 2025

Source: Advances in Space Research

Author(s): M. Jishad, Smitha Ratheesh, Neeraj Agarwal, Neerja Sharma, Rashmi Sharma

Performance Evaluation of NTCM Ionospheric Model Variants (NTCM-GL, NTCM-BC, NTCM-Klobpar and NTCM-GlAzpar) during the 25th Solar Cycle

Publication date: Available online 1 November 2025

Source: Advances in Space Research

Author(s): Wenyao Zhang, Yunbin Yuan, Ting Zhang, Chunchun Sheng, Min Li

A novel automated technique based on ensemble learning for prediction of soil moisture using satellite images

Publication date: Available online 1 November 2025

Source: Advances in Space Research

Author(s): Aryan Singh, Rohit Kumar Tiwari, Manish Pratap Singh, Sunil Jha

DCP-CNN-based non-cooperative spacecraft non-contact attitude estimation

Publication date: Available online 1 November 2025

Source: Advances in Space Research

Author(s): Kairui Zhong, Xiaoyu Lang, Kewei Zhu, Zhen Chen, Xiangdong Liu

Ionospheric topside sounding revival

Publication date: Available online 31 October 2025

Source: Advances in Space Research

Author(s): Sergey Pulinets, Konstantin Tsybulya, Victor Depuev, Igor Danilov, Maria Pulinets

Corrigendum to “Unravelling the detection of Carrington storm of 1859 from the historical magnetic declination observations of Trivandrum observatory”. [Adv. Space Res. 76/6 (2025) 3670–3680]

Publication date: Available online 31 October 2025

Source: Advances in Space Research

Author(s): R. Jayakrishnan, C.K. Fazil, L.Rahul Dev, A. Ajesh

Multi-objective early warning mission planning by multiple satellites using a critical task aggregation-based NSGA-II algorithm

Publication date: Available online 30 October 2025

Source: Advances in Space Research

Author(s): Yi Gu, Zihao Li, Hanqing Liu, Qizhang Luo, Huan Liu, Guohua Wu

Study on the influence of ignition voltage on the evaporation and combustion characteristics of metal nanofluid propellants

Publication date: Available online 30 October 2025

Source: Advances in Space Research

Author(s): JinZe Wu, HongMeng Li, GuoXiu Li, Shuo Zhang, Tao Zhang, ZhaoPu Yao

Main driver of Sargassum blooms in the Atlantic Ocean revealed

Phys.org: Earth science - Wed, 11/05/2025 - 19:08
By the beginning of June this year, approximately 38 million tons of Sargassum drifted towards the coasts of the Caribbean islands, the Gulf of Mexico, and northern South America, marking a negative record. Especially during the summer months, the brown algae accumulate on beaches, decomposing and emitting a foul odor. This not only repels tourists but also threatens coastal ecosystems. In the open ocean, Sargassum seaweed floating on the surface serves as nourishment and habitat for numerous marine species.

Southern Ocean's winter CO₂ outgassing underestimated by 40%, study reveals

Phys.org: Earth science - Wed, 11/05/2025 - 19:00
A collaborative research team has discovered that the Southern Ocean releases substantially more carbon dioxide (CO2) during the dark austral winter than previously thought. Their new study reveals that this winter outgassing has been underestimated by up to 40%.

Solar radiation could cool Earth, not replace emissions

Phys.org: Earth science - Wed, 11/05/2025 - 18:08
Techniques to reflect an additional small portion of sunlight back into space could help cool the planet if deployed globally, but they cannot address the full range of climate impacts or replace emission cuts, according to a Royal Society briefing.

Coastal groundwater rivals rivers and volcanoes in shaping ocean chemistry, study finds

Phys.org: Earth science - Wed, 11/05/2025 - 17:02
We've gone to the bottom of the ocean to study how its chemistry shapes our planet's climate, even chasing lava-spewing underwater volcanoes to do it. But it turns out we may have missed something far closer to home: the water beneath our feet.

Polar ocean turbulence projected to intensify as sea ice declines

Phys.org: Earth science - Wed, 11/05/2025 - 16:02
A study published in Nature Climate Change by an international team of scientists from the IBS Center for Climate Physics (ICCP) at Pusan National University in South Korea, presents new evidence that ocean turbulence and a process known as "horizontal stirring" will increase dramatically in the Arctic and Southern Oceans due to human-induced global warming and decreasing sea ice coverage.

New underwater device tracks real-time nutrient exchanges between sediments and water

Phys.org: Earth science - Wed, 11/05/2025 - 14:45
Beneath the surface of lakes and coastal waters lies a hidden world of sediment that plays a crucial role in the health of aquatic ecosystems. "Benthic fluxes" of nitrogen and phosphorus, such as releases of these dissolved nutrients from sediments to their overlying waters, can fuel algae growth and toxic harmful algal blooms (HABs), which degrade water quality, disrupt wildlife and recreation, and reduce property values.

As CO2 Levels Rise, Old Amazon Trees Are Getting Bigger

EOS - Wed, 11/05/2025 - 14:27

When we look at the towering trees of old-growth forest patches in the Amazon, we might think these ancient beings have reached their maximum size and width.

It turns out they have not, a new study suggests. It shows that even the largest and oldest Amazonian trees still capture carbon dioxide (CO2)—and keep getting bigger, albeit at a slow pace.

Led by Adriane Esquivel-Muelbert, an ecologist at the University of Cambridge, the researchers analyzed 3 decades of tree measurements from 188 primary forest plots spread across nine Amazonian countries. Each plot was around 1 hectare, about the size of a city block, and was measured by teams using tapes and notebooks, often under harsh conditions.

The plots were selected from the Amazon Forest Inventory Network (RAINFOR), which has become one of the most important monitoring efforts in tropical ecology, according to Esquivel-Muelbert. The monitoring period varied between 1971 and 2015.

“We already knew the Amazon works as a carbon sink,” she said. “But we wanted to understand what’s happening inside the forest—what kinds of trees are changing, and how.”

The study, published in Nature Plants, found that the average tree size had increased by 3.3% per decade over the past 30 years. Large-canopy trees—those with trunks wider than 40 centimeters—grew even faster in diameter. Smaller trees shaded by larger ones also grew, while the size of medium-sized trees remained relatively stable.

The consistency across the Amazon basin suggests the increasing amount of CO2 in the atmosphere is the ingredient fattening up the trees. “Carbon is an extra resource,” Esquivel-Muelbert explained. “With the same amount of light, a plant can photosynthesize more efficiently when there’s more CO2 available.”

In other words, as humans release more carbon into the atmosphere, Amazonian trees seem to be using some of it to grow. The researchers interpreted the pattern as a mix of two effects: a winner-takes-all response, in which the tallest trees gain even more advantage, and a carbon-limited benefit response, in which smaller, shaded trees find it easier to survive in low light. Both effects can occur at the same time, leading to more biomass for both groups at the extremes of the size scale.

The study also found no sign that large trees are dying faster, contradicting earlier hypotheses that canopy giants would be the first casualties of heat and drought. The resilience of these ancient trees—some of them centuries old—is important because they sequester a disproportionate share of the forest’s carbon.

“The largest 1% of trees account for about half of all the carbon stored and absorbed by the forest,” Esquivel-Muelbert said. Losing them would mean losing much of the Amazon’s buffering power against climate change.

Not Exactly Good News

“It doesn’t mean carbon dioxide is good for the forest. What we’re seeing is resilience, not relief.”

The findings might sound like good news, but “it doesn’t mean carbon dioxide is good for the forest,” Esquivel-Muelbert said. “What we’re seeing is resilience, not relief.”

Carbon dioxide might be fattening up old trees, but its consequences for the global climate totally offset what might look like an advantage or a good thing at first sight, she emphasized.

To Tomás Domingues, a forest ecologist at the Universidade de São Paulo in Ribeirão Preto, the new results offer valuable real-world confirmation of what experimental models have long proposed. “The study shows that the community as a whole is gaining biomass, presumably due to higher CO2,” he said. “That aligns perfectly with what we’re testing at AmazonFACE.”

AmazonFACE—a large-scale open-air experiment near Manaus in the Brazilian state of Amazonas—exposes forest patches to elevated concentrations of atmospheric carbon to simulate future conditions. One of its main goals is to see how long the carbon fertilization effect can last before the forest runs into another limitation: the lack of nutrients such as phosphorus, calcium, magnesium, and potassium.

“The CO2 effect has a short life,” Domingues explained. “Trees can only turn extra carbon into growth if they have enough nutrients. In the Amazon, everybody—trees, microbes, fungi, insects—is competing for the same scarce resources.” If nutrients become limited, he added, growth could plateau or even reverse, regardless of the CO2 supply.

Still Holding On

The new findings highlight how complex the Amazon’s responses to human-driven change can be. While extra carbon has acted as a growth stimulus so far, climate stressors, especially heat, drought, and windstorms, are also intensifying.

Previous studies suggested that the Amazon’s overall carbon storage capacity is starting to weaken. Changes in species composition, repeated droughts, and the spread of degradation along the southern and eastern edges of the basin are already weakening parts of the system. “The forest is still resisting,” Esquivel-Muelbert said, “but that doesn’t mean it will resist forever.”

“These forests are resilient, but they’re irreplaceable. If we lose them, they don’t come back in our lifetime.”

Domingues noted that 30 years of observations, though impressive for tropical fieldwork, still capture only a short moment in ecological time. “For the forest, 30 years is nothing,” he said. “These trees live for centuries. We need to keep watching.”

Despite the unknowns, both researchers are clear: Protecting mature, intact forests is crucial if we want to fight climate change. Reforestation won’t replace the carbon storage capacity of old-growth trees. “These forests are resilient, but they’re irreplaceable,” Esquivel-Muelbert said. “If we lose them, they don’t come back in our lifetime.”

The study’s main message, Esquivel-Muelbert added, is not that the Amazon is thriving under climate change. It’s that the forest is still holding on, at least for now.

—Meghie Rodrigues (@meghier.bsky.social), Science Writer

Citation: Rodrigues, M. (2025), As CO2 levels rise, old Amazon trees are getting bigger, Eos, 106, https://doi.org/10.1029/2025EO250413. Published on 5 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.

Are “Day Zero Droughts” Closer Than We Think? Here’s What We Know

EOS - Wed, 11/05/2025 - 14:27

The outlook for our planet’s water future is anything but reassuring. Across much of the world, communities are already confronting prolonged drought, shrinking reservoirs, and the growing struggle to secure reliable access.

“Even without global warming, if water demand continues to rise steadily, scarcity is inevitable.”

Now, a new study in Nature Communications suggests that so-called day zero droughts (DZDs)—moments when water levels in reservoirs fall so low that water may no longer reach homes—could become common as early as this decade and the 2030s.

To find out where and when DZDs are most likely to occur, scientists at the Center for Climate Physics in Busan, South Korea, ran a series of large-scale climate simulations. They considered the imbalance between decreasing natural supply (such as years of below-average rainfall and depleted river flows) and increasing human demand (including surging economic and demographic growth).

“Most studies tend to focus on supply alone, not on the interplay between supply and demand,” explained Christian L. E. Franzke, a climate scientist and coauthor of the study. “But even without global warming, if water demand continues to rise steadily, scarcity is inevitable.”

Cities on the Edge of Thirst

The team found that urban areas face the highest risk of DZDs. As cities expand, their thirst for water often exceeds what local systems can provide, leaving them exposed to shortages and instability.

The near catastrophe in Cape Town in 2018, when water was rationed to avoid a complete shutdown, remains a stark warning for cities worldwide. “I remember the measures that had to be taken,” Franzke said. “There were severe restrictions—people had to limit their use to just a few liters a day.”

Central spatial maps (a) and (b) show the spatial distribution of the ensemble mean waiting time and duration of day zero drought (DZD) events, respectively, following the time of first emergence (TOFE) at each grid point of DZD-prone regions across the globe. Map (c) represents the spatial distribution of the frequency (%) of extreme DZD events, defined as those where the event duration exceeds the waiting time, indicating prolonged water scarcity impact and short recovery period. The accompanying inset circular diagram illustrates the distribution of these events, with the color scale indicating the proportion (percentages) of grid cells experiencing such conditions. The surrounding paired panels depict the probability density function (PDF) of waiting time and duration for DZD events across seven DZD-prone regions. The vertical dashed lines mark the ensemble mean (black), 90th percentile (blue), and 99th percentile (green) for each region. The red dashed line represents the monthly scale of the compound extreme event, which is 48 months. The period considered for each grid point starts from the month after each decade of their respective TOFEs and continues until 2100. Click image for larger version. Credit: Ravinandrasana and Franzke, 2025, https://doi.org/10.1038/s41467-025-63784-6, CC BY-NC-ND 4.0

The human toll of DZDs goes beyond empty taps. It deepens existing inequalities, hitting low-income communities hardest because they are generally less able to endure rising costs of accessing clean water while also being more reliant on public utilities that are slower to secure alternate water sources. Urban DZDs also threaten public health by disrupting sanitation.

Overall, a DZD weakens economies and undermines social stability—especially in developing regions where physical, economic, and institutional vulnerabilities overlap.

According to the study, regions along the Mediterranean, southern Africa, and parts of North America are likely hot spots for DZDs, places where the zero point could arrive much sooner and last much longer.

“These already dry regions are becoming even drier,” said Alejandro Jaramillo Moreno, a hydroclimatology specialist from the Department of Atmospheric Sciences at Universidad Nacional Autónoma de México. Jaramillo was not involved in the new study. “Global warming is amplifying the contrast between wet and dry areas. Where rainfall is scarce, it will likely become scarcer.”

Avoiding the Tipping Point

For Franzke, solutions must come not only from individuals using water more responsibly but also from policymakers who prioritize smart management and modern infrastructure. “There’s a lot of leakage,” he said. “Pipes are old, and water escapes before it reaches people. Updating this infrastructure is crucial.”

It may seem unthinkable that metropolises like Los Angeles could one day face evacuation because of water shortages, but experts warn that this scenario isn’t far-fetched if systemic solutions aren’t implemented.

In many regions, water rationing caused by severe drought is already a reality. Chile, for instance, has experienced a water crisis for more than a decade, and water is rationed in areas including the nation’s capital and largest city, Santiago. Iraq, Syria, and Turkey are experiencing one of the worst regional droughts in their modern histories.

Jaramillo takes a long view of civilizations’ relationship with water supply. “Throughout history, cities have reached their zero point—not only in water but in other essential resources,” he reflected. “The difference is that now, we still have time (and knowledge) to change course.”

—Mariana Mastache-Maldonado (@deerenoir.bsky.social), Science Writer

Citation: Mastache-Maldonado, M. (2025), Are “day zero droughts” closer than we think? Here’s what we know, Eos, 106, https://doi.org/10.1029/2025EO250409. Published on 5 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.

China commands 47% of remote sensing research, while U.S. produces just 9%

Phys.org: Earth science - Wed, 11/05/2025 - 13:03
The United States is falling far behind China in remote sensing research, according to a comprehensive new study that tracked seven decades of academic publishing and reveals a notable reversal in global technological standing.

Ancient trees' inefficient photorespiration may have helped stabilize Earth's atmosphere during last ice age

Phys.org: Earth science - Wed, 11/05/2025 - 10:00
Ancient trees may have played a key role in regulating Earth's climate during the last ice age—by 'breathing' less efficiently.

Cleaner air may be accelerating warming by making clouds less reflective

Phys.org: Earth science - Wed, 11/05/2025 - 10:00
Earth is reflecting less sunlight, and absorbing more heat, than it did several decades ago. Global warming is advancing faster than climate models predicted, with observed temperatures exceeding projections in 2023 and 2024. These trends have scientists scrambling to understand why the atmosphere is letting more light in.

Global land carbon sink halved in 2024, AI model suggests

Phys.org: Earth science - Tue, 11/04/2025 - 20:51
A Peking University research team led by Wang Heyuan and Wang Kai at the Institute for Carbon Neutrality (ICN) used AI models to determine that the global land carbon sink has drastically shrunk due to an abrupt and extreme jump in global temperature. Their study, "AI-tracked halving of global land carbon sink in 2024," was published in Science Bulletin.

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