Scientists detect a sudden acceleration in global warming

 Global warming has been increasing at a faster pace since about 2015, according to a new study from the Potsdam Institute for Climate Impact Research (PIK). By adjusting global temperature records to remove known natural influences, researchers were able to identify a statistically significant rise in the rate of warming for the first time.

During the past decade, global temperatures have climbed at an estimated rate of about 0.35°C per decade, depending on the dataset analyzed. From 1970 through 2015, the average increase was just under 0.2°C per decade. The more recent trend represents the fastest warming observed in any decade since instrumental temperature records began in 1880.

"We can now demonstrate a strong and statistically significant acceleration of global warming since around 2015," says Grant Foster, a US statistics expert and co-author of the study, which was published today in the scientific journal Geophysical Research Letters.

"We filter out known natural influences in the observational data, so that the 'noise' is reduced, making the underlying long-term warming signal more clearly visible," Foster added.

Removing Natural Climate Variability From Temperature Data

Short term natural events can temporarily raise or lower global temperatures and make it harder to detect changes in long term climate trends. These influences include El Niño events, volcanic eruptions, and variations in solar activity.

To address this challenge, the researchers analyzed measurement data from five widely used global temperature datasets (NASA, NOAA, HadCRUT, Berkeley Earth, ERA5). By adjusting the data to account for these natural factors, the team was able to isolate the underlying warming trend more clearly.

"The adjusted data show an acceleration of global warming since 2015 with a statistical certainty of over 98 percent, consistent across all data sets examined and independent of the analysis method chosen," explains Stefan Rahmstorf, PIK researcher and lead author of the study.

Statistical Analysis Reveals a Shift in Warming Trends

The study focused on determining whether the pace of warming has changed, rather than identifying the causes behind that shift.

After accounting for the influence of El Niño and the recent solar maximum, the extremely warm years of 2023 and 2024 appear slightly cooler in the adjusted analysis. Even with these corrections, they still rank as the two warmest years recorded since instrumental measurements began. Across all datasets, the faster warming trend becomes visible around 2013 or 2014.

To evaluate whether the warming rate has changed since the 1970s, the researchers applied two statistical techniques: a quadratic trend analysis and a piecewise linear model that identifies when shifts in warming rates occur.

Implications for the Paris Agreement Climate Target

The study does not attempt to determine the specific reasons behind the acceleration in warming. However, the authors note that climate models already allow for the possibility that the rate of warming could increase over time.

"If the warming rate of the past 10 years continues, it would lead to a long-term exceedance of the 1.5°C limit of the Paris Agreement before 2030," says Stefan Rahmstorf. "How quickly the Earth continues to warm ultimately depends on how rapidly we reduce global CO2 emissions from fossil fuels to zero."

Source: ScienceDaily

Parents’ stress may be quietly driving childhood obesity, Yale study finds

 Childhood obesity has been increasing in recent years. According to the U.S. Centers for Disease Control, about one in five children and teenagers in the United States met the clinical definition of obesity in 2024.

Preventing obesity in children is not simple. For many years, the main approaches have focused on encouraging healthy eating and regular physical activity. Researchers at Yale now suggest that another important factor should be added to that list: reducing stress in parents.A research team led by Yale psychologist Rajita Sinha found evidence that lowering parental stress may help reduce the risk of obesity in young children.

"It's the third leg of the stool," said Sinha. "We already knew that stress can be a big contributor in the development of childhood obesity. The surprise was that when parents handled stress better, their parenting improved, and their young child's obesity risk went down."

The findings were published in the journal Pediatrics.

Parent Stress May Influence Children's Eating and Health

Earlier studies have shown that children are more likely to develop obesity if their parents are obese. Researchers have also suspected that parental stress may be another hidden contributor to obesity in early childhood.

Previous work has shown that stressed parents are more likely to depend on fast food and less healthy eating habits. These choices can influence children's behavior and food preferences. When parents feel overwhelmed, family routines can break down, unhealthy food choices may become more common, and positive parenting behaviors can decline.

Still, most current childhood obesity prevention programs focus mainly on nutrition education and physical activity. According to Sinha, these efforts often fail to create lasting improvements.

Sinha is the Foundations Fund Professor in Psychiatry and a professor in neuroscience and child study at Yale School of Medicine.

Testing a Stress Reduction Program for Parents

To explore the role of parental stress, researchers conducted a 12 week randomized prevention trial involving 114 parents from diverse ethnic and socioeconomic backgrounds. All participants had children between two and five years old who were overweight or obese.

Parents were assigned to one of two groups. One group participated in a stress focused program called Parenting Mindfully for Health (PMH). This program taught mindfulness techniques and behavioral self regulation skills while also providing guidance on healthy nutrition and physical activity.

Source: ScienceDaily

Scientists capture a magnetic flip in 140 trillionths of a second

 A team led by Ryo Shimano at the University of Tokyo has directly observed how electron spins flip inside an antiferromagnet, a material in which opposing spins cancel each other out. By capturing this process in action, the researchers identified two separate switching mechanisms. One of them outlines a practical path toward ultrafast, non-volatile magnetic memory and logic devices that could outperform today's technologies. The results were published in Nature Materials.

From punched paper cards and metal rods to vacuum tubes and transistors, modern computing has always relied on physical systems to represent 0s and 1s. As demand for processing power continues to rise, researchers are searching for faster and more efficient alternatives. Antiferromagnets offer a promising option. Although they appear magnetically neutral because their spins balance out, their internal magnetic structure can still be harnessed to store digital information in new ways."For many years," says Shimano, "scientists believed that antiferromagnets like Mn3Sn (manganese three tin) could switch their magnetization extremely quickly. However, it was unclear whether this non-volatile switching could complete within a few to several tens of picoseconds or how the magnetization really changed during the switching process."

Heat or Current? Solving the Switching Mystery

A central question was what actually drives the spin reversal. Does the electric current flip the spins directly, or does heat generated by the current cause the change?

To find out, the team designed an experiment to watch the process unfold in real time. They fabricated a thin film of Mn3Sn and sent brief electrical pulses through it. At the same time, they illuminated the sample with precisely timed ultrafast flashes of light, adjusting the delay between the current pulse and the light pulse. This approach allowed them to assemble a time resolved sequence showing how the magnetization evolved moment by moment.

"The most challenging part of the project," Shimano remembers, "was measuring the infinitesimal changes in the magneto-optical signal. However, we were surprised how clearly we could finally observe the switching process once we established the right method."

Two Distinct Spin Switching Mechanisms Revealed

The experiment produced something unprecedented: a frame by frame view of magnetic pattern changes during switching. The images showed that the behavior depends on the strength of the applied current.

When the current was strong, switching was driven by heating effects. Under weaker current conditions, however, the spins flipped with little to no heating involved. This second pathway is especially significant because it suggests a way to control magnetic states quickly and efficiently without wasting energy as heat.

That heat free switching mechanism could serve as the foundation for next generation spintronic devices used in computing, communications, and advanced electronics. For Shimano, the findings point to new scientific territory still waiting to be explored.

Pushing the Limits of Picosecond Switching

"Our present fastest time-resolved observation of electrical switching in Mn₃Sn is 140 picoseconds, mainly limited by how short the current pulses can be generated in our device setup. However, our findings suggest that the material itself could switch even faster under appropriate conditions. In the future, we aim to explore these ultimate limits by creating even shorter current pulses and by optimizing the device structure."

Although the current measurements are capped at 140 picoseconds, the material's true speed limit may be even shorter. By refining their experimental tools and device design, the researchers hope to uncover just how fast antiferromagnetic spin switching can ultimately go.

Source: ScienceDaily

Scientists reveal how exercise protects the brain from Alzheimer’s

 Researchers at UC San Francisco have identified a biological process that may explain why exercise sharpens thinking and memory. Their findings suggest that physical activity strengthens the brain's built in defense system, helping protect it from age related damage.

As people grow older, the blood-brain barrier becomes more fragile. This tightly packed network of blood vessels normally shields the brain from harmful substances circulating in the bloodstream. Over time, however, it can become leaky, allowing damaging compounds to enter brain tissue. The result is inflammation, which is linked to cognitive decline and is commonly seen in disorders such as Alzheimer's disease

Several years ago, the research team discovered that exercising mice produced higher levels of an enzyme called GPLD1 in their livers. GPLD1 appeared to rejuvenate the brain, but there was a mystery. The enzyme itself cannot cross into the brain, leaving scientists unsure how it delivered its cognitive benefits.

The new research provides an answer.

How GPLD1 Reduces Brain Inflammation

The scientists found that GPLD1 influences another protein known as TNAP. As mice age, TNAP builds up in the cells that form the blood-brain barrier. This buildup weakens the barrier and increases leakiness. When mice exercise, their livers release GPLD1 into the bloodstream. The enzyme travels to the blood vessels surrounding the brain and removes TNAP from the surface of those cells, helping restore the barrier's integrity.

"This discovery shows just how relevant the body is for understanding how the brain declines with age," said Saul Villeda, PhD, associate director of the UCSF Bakar Aging Research Institute.

Villeda is the senior author of the paper, which was published in the journal Cell on Feb. 18.

Pinpointing TNAP's Role in Cognitive Decline

To determine how GPLD1 exerts its effects, the team focused on what the enzyme does best. GPLD1 cuts specific proteins from the surface of cells. Researchers searched for tissues containing proteins that could serve as targets and suspected that some of these proteins might accumulate with age.

Cells in the blood-brain barrier stood out because they carried several possible GPLD1 targets. When the scientists tested these proteins in the lab, only one was trimmed by GPLD1: TNAP.

Further experiments confirmed TNAP's importance. Young mice genetically modified to produce excess TNAP in the blood-brain barrier showed memory and cognitive problems similar to those seen in older animals.

When researchers reduced TNAP levels in 2-year-old mice -- which are the equivalent of 70 human years -- the blood-brain barrier became less permeable, inflammation decreased, and the animals performed better on memory tests.

"We were able to tap into this mechanism late in life, for the mice, and it still worked," said Gregor Bieri, PhD, a postdoctoral scholar in Villeda's lab and co-first author of the study.

Source: ScienceDaily

“Celtic curse” hotspots found in Scotland and Ireland with 1 in 54 at risk

 People with roots in the Outer Hebrides and northwest Ireland face the highest known risk of developing hemochromatosis, a genetic disorder that causes the body to absorb and store too much iron. Over time, that excess iron can build up to dangerous levels.

This is the first time researchers have mapped genetic risk for hemochromatosis, sometimes called the 'Celtic curse', across the UK and Ireland. The condition has long been known to affect Scottish and Irish populations at higher rates, but until now its geographic distribution had not been clearly char Experts say the findings could help health officials focus genetic screening in the areas most affected, allowing people at risk to be identified earlier and treated before serious complications develop.

Iron Overload Can Damage Organs Over Decades

Hemochromatosis often develops slowly. Excess iron can accumulate in organs for years or even decades before symptoms appear. If left untreated, it can lead to liver damage, liver cancer, arthritis, and other serious health problems. Early diagnosis makes a major difference. Regular blood donation to lower iron levels is a simple and effective treatment that can prevent much of the harm.

The disease is caused by inherited changes in DNA known as genetic variants. In the UK and Ireland, the main risk factor is a variant called C282Y.

Researchers at the University of Edinburgh analyzed genetic information from more than 400,000 people who took part in the UK BioBank and Viking Genes studies. They examined how common the C282Y variant was in 29 regions across the British Isles and Ireland.

Where the C282Y Gene Variant Is Most Common

The highest rates were found among people with ancestry from northwest Ireland, where about one in 54 people are estimated to carry the variant. The Outer Hebrides followed closely at one in 62, and Northern Ireland at one in 71.

Mainland Scotland also showed elevated risk, particularly in Glasgow and southwest Scotland. In those areas, about one in 117 people carry the variant, reinforcing the long standing 'Celtic Curse' nickname.

Because the combined genetic risk is so high in these regions, researchers say targeted screening there would likely identify the greatest number of people with the condition.

Diagnosis Patterns and Possible Under Detection

The team also reviewed NHS England records and found more than 70,000 diagnosed cases of hemochromatosis. White Irish individuals were nearly four times more likely to be diagnosed than white British individuals.ted.

Source: ScienceDaily

Can solar storms trigger earthquakes? Scientists propose surprising link

 Scientists at Kyoto University have developed a theoretical model examining whether disturbances in the ionosphere could apply electrostatic forces deep within the Earth's crust. Under certain conditions, these forces might contribute to the start of large earthquakes.

The research is not designed to forecast earthquakes. Instead, it outlines a possible physical mechanism showing how shifts in ionospheric charge levels -- triggered by intense solar activity such as solar flares -- might interact with already weakened areas of the crust and influence how fractures develop.

How the Ionosphere Could Affect Fault Zones

In this model, cracked regions of the crust are thought to contain water at extremely high temperatures and pressures, possibly in a supercritical state. Electrically, these fractured zones may act like capacitors. They are coupled both to the Earth's surface and to the lower ionosphere, creating a vast electrostatic system that links the ground to the upper atmosphere.

When solar activity surges, electron density in the ionosphere can rise significantly. This can produce a negatively charged layer in the lower ionosphere. Through capacitive coupling, that charge may generate intense electric fields inside microscopic voids within fractured rock. The resulting electrostatic pressure could approach levels similar to tidal or gravitational stresses that are already known to influence fault stability.

According to the team's calculations, ionospheric disturbances tied to major solar flares -- involving increases in total electron content of several tens of TEC units -- might create electrostatic pressures of several megapascals within these crustal voids.

Ionospheric Anomalies Observed Before Major Quakes

Unusual ionospheric behavior has often been detected before powerful earthquakes. Observations have included spikes in electron density, drops in ionospheric altitude, and slower propagation of medium-scale traveling ionospheric disturbances. Traditionally, scientists have interpreted these changes as effects caused by stress building up inside the crust.

This new framework offers an additional perspective. It suggests a two way interaction in which processes inside the Earth can influence the ionosphere, while ionospheric disturbances may also send feedback forces back down into the crust. The model connects space weather and seismic activity without claiming that solar activity directly causes earthquakes.

Source: ScienceDaily

Lost fossils reveal sea monsters that took over after Earth’s greatest extinction

 About 250 million years ago, a region that is now a harsh desert in remote northwestern Australia lay along the edge of a shallow bay connected to a vast prehistoric ocean. Fossils collected there more than six decades ago and largely overlooked in museum collections are now reshaping scientists' understanding of how land animals first returned to the sea and spread across the globe.

The end-Permian mass extinction, the most devastating die-off in Earth's history, struck about 252 million years ago and was followed by extreme global warming. In its aftermath, modern-style marine ecosystems began to take shape at the start of the Age of Dinosaurs (or Mesozoic era). During this critical window, the earliest sea-going tetrapods (limbed vertebrates), including amphibians and reptiles, emerged and quickly became dominant aquatic apex predators. Most fossils of these early marine hunters have been found in the northern hemisphere. Comparable discoveries from the southern hemisphere have been rare and remain poorly documented.

Now, a fresh analysis of 250 million-year-old fossils from the Kimberly region of northern Western Australia reveals a surprisingly diverse group of marine amphibians with unexpected global connections across ancient oceans.

Lost Fossils Rediscovered After 50 Years

Marine amphibian fossils were first uncovered in Australia during expeditions in the 1960s and 1970s. The specimens were divided between museums in Australia and the U.S.A. Research published in 1972 concluded that the material represented a single species, Erythrobatrachus noonkanbahensis. The species was identified from several skull fragments eroding out of rock at Noonkanbah cattle station, east of the remote Kimberly town of Derby.

Over the following decades, the original Erythrobatrachus fossils were misplaced. Their disappearance triggered an international search through museum collections. In 2024, the long-lost specimens were finally located, allowing researchers to reexamine these puzzling marine amphibians with modern techniques.

Early Marine Amphibians After the Permian Extinction

Erythrobatrachus belonged to a group known as trematosaurid temnospondyls. These animals were 'crocodile-like' relatives of today's salamanders and frogs and could reach lengths of up to 2 m. Trematosaurids are especially significant because their fossils appear in coastal rock deposits formed less than 1 million years after the end-Permian mass extinction. As a result, they represent the oldest clearly recognizable group of Mesozoic marine tetrapods.

A closer look at the rediscovered skull fragments revealed an important surprise. The bones once attributed to a single species actually came from at least two different trematosaurids: Erythrobatrachus and a second form belonging to the genus Aphaneramma.

Source: ScienceDaily