Melting Ice Shelves Accelerate Critical Antarctic Glacier Retreat

A Giant Iceberg Threatening Pine Island’s Ice Shelf

NASA/Brooke Medley

West Antarctica’s colossal glaciers are experiencing a rapid acceleration in melting, particularly since 2017. This alarming trend signals a decline in the ice shelf’s effectiveness in stabilizing the glacier.

Pine Island Glacier, the fastest-flowing glacier in Antarctica, significantly contributes to global sea level rise. This glacier plays a crucial role in the West Antarctic Ice Sheet, which has the potential to raise global sea levels by 5.3 meters if it fully melts.

The Pine Island Ice Shelf, extending into the ocean, is essential for holding back inland ice and shielding it from warm waters, potentially preventing 51 centimeters of sea level rise.

The instability of Pine Island Glacier, along with the nearby Thwaites Glacier, poses a significant risk to the longevity of the West Antarctic Ice Sheet.

Sarah Wells-Moran from the University of Chicago has been tracking the Pine Island Glacier using images from the Copernicus Sentinel 1 satellite, with data extending back to the 1970s.

The glacier’s velocity surged from 2.2 kilometers per year in 1974 to 4 kilometers per year by 2008 and reached nearly 5 kilometers per year from 2017 to 2023. This represents a 20 percent increase in just six years and a 113 percent increase since 1973.

Between 1973 and 2013, the ice flow from Pine Island Glacier accelerated by over 75%.

These changes have resulted in the glacier’s grounding line—the point at which the ice shelf begins to float—receding dramatically by more than 30 kilometers.

The researchers connected their findings to computer models, concluding that the ice shelf’s thinning and fractures allow warmer waters to penetrate further. This has led to the edge of the shelf “opening up,” as noted by Wells-Moran and her team.

They concluded that ice loss from West Antarctica is worsening due to the Pine Island ice shelf’s diminishing support for the upstream ice.

Sue Cook from the University of Tasmania stated that calving events alone cannot solely explain the acceleration of the glacier. She emphasized, “The damage to the glacier’s shear margin is likely the primary cause. This study corroborates that mechanism.”

Ted Scambos from the University of Colorado noted that warm ocean water is likely reaching the edge of the ice shelf in Pine Island Bay. “The loss of ice shelves may accelerate ocean circulation within the fjord, heightening circulation intensity where the glacier meets bedrock,” Scambos explained.

Nellie Abram from the Australian Antarctic Division remarked that this research will help determine the extent and rate at which the Pine Island ice shelf is collapsing. “It’s evident that the ice loss from this area will continue to affect coastlines worldwide for decades to come,” Abram stated.

Explore Norway’s Svalbard and Tromsø: Fjords, Glaciers, and Northern Lights

Embark on an exhilarating Arctic adventure in Norway. Discover the science behind the Northern Lights, the unique Arctic ecosystem, and how humans adapt to the Northern environment.

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Source: www.newscientist.com

Melting of Northern Greenland’s Ice Dome: Past Events and Future Risks

Greenland drill cargo awaiting transport by ski plane at Prudhoe Dome

Researchers Working at Prudhoe Dome in Greenland

Caleb K. Wolcott-George

The ice dome located in northern Greenland has previously melted completely under temperatures expected to return this century. This significant discovery offers valuable insights into the speed at which melting ice sheets can influence global sea levels.

In a groundbreaking study, researchers drilled 500 meters into Prudhoe Dome, an extensive ice formation the size of Luxembourg situated in northwestern Greenland, gathering seven meters of sediment and rock core. Infrared dating indicated that the core’s surface sand was sun-bleached approximately 7,000 years ago—corroborating that the dome fully melted as the planet emerged from its last glacial maximum due to cyclical changes in Earth’s orbital dynamics.

During that era, summer temperatures were 3°C to 5°C warmer than today’s averages. Alarmingly, human-induced climate change could bring back similar temperatures by 2100.

“This provides direct evidence that the ice sheet is highly sensitive to even the modest warming seen during the Holocene,” stated Yarrow Axford, a Northwestern University researcher not involved in the study.

With the ongoing melting of Greenland’s ice sheet, projections indicate a potential sea level rise of tens of centimeters to a meter within this century. To refine these predictions, scientists must enhance their understanding of how quickly various sections of the ice sheet are dissipating.

The Prudhoe Dome core is the first of multiple cores analyzed by the GreenDrill project, funded by the National Science Foundation and featuring researchers from various U.S. universities. Their goal is to extract crucial climate data from beneath the ice sheets, one of Earth’s least-explored areas.

Notably, deposits excavated in 1966 from beneath the ice at Camp Century—a U.S. nuclear military facility operational for eight years during the Cold War—revealed that Greenland lacked ice around 400,000 years ago. Further, a rock core taken in 1993 from underneath Summit Station illustrated that the entire ice sheet has melted as recently as 1.1 million years ago.

However, the GreenDrill project extends its research deeper beneath the ice, collecting samples from multiple locations near Greenland’s northern coast.

“The crucial question is when did the edge of Greenland experience melting in the past?” posed Caleb Walcott-George, part of a new research team at the University of Kentucky. “This is where the initial sea level rise will transpire.”

Current ice sheet models indicate uncertainty regarding whether northern or southern Greenland will melt at a faster rate in the future. This study bolsters the evidence that warming post-last glacial maximum manifested earlier and with greater intensity in northern Greenland, according to Axford.

Potential explanations may involve feedback mechanisms, such as the loss of Arctic sea ice, which could have allowed more ocean heat to penetrate the atmosphere in the far north.

By confirming that Prudhoe Dome melted under a warming of 3°C to 5°C, this study adds credibility to ice sheet models that predict similar outcomes, asserted Edward Gasson, who was not part of the research at the University of Exeter, UK.

“This research is vital for recalibrating surface melting models: When will we really begin to lose this ice?” Gasson emphasized.

Source: www.newscientist.com

Accelerated Melting in Antarctica May Support Key Ocean Currents

Impact of Melting Antarctic Ice on Ocean Currents

Juan Barretto/AFP via Getty Images

The melting of Greenland’s ice sheet is predicted to hinder or disrupt the Atlantic current that helps keep Europe warm; however, meltwater from West Antarctica might help maintain this essential flow.

That said, it won’t be sufficient to prevent significant climate changes. The Atlantic Meridional Overturning Circulation (AMOC) is already down by 60% and could take up to 3,000 years to recover fully.

“I suggest caution in predicting an AMOC collapse,” states Sasha Sinnett from Utrecht University in the Netherlands. “However, my findings don’t alter what is forecasted for the next century. We may never see if West Antarctica successfully stabilizes the AMOC.”

The AMOC is a system of ocean currents that transports warm surface water from the tropics to northern Europe. Here, the water cools and sinks, then flows back south to Antarctica. This current carries an enormous amount of heat—1.2 petawatts—equivalent to the output of one million power plants, keeping Europe notably warmer than regions like Labrador or Siberia at similar latitudes. Lighter, fresher meltwater from Greenland is expected to obstruct the sinking of the denser, saltier AMOC water, thereby slowing its flow.

If the AMOC were to collapse, winter temperatures in Northern Europe could drop to almost -50℃ (-58°F). Recently, Iceland declared the closure of the AMOC as an “existing” security threat. Additionally, rising sea levels are threatening the U.S. East Coast, while Africa may face even more severe drought conditions.

A recent study indicates that even if we achieve net zero emissions by 2075 and begin reducing CO2 from the atmosphere, there is still a 25% risk of AMOC collapse. One study forecasts its closure in the coming decades, while another suggests that it will remain weakened due to Antarctic winds.

Currently, the melting of the West Antarctic ice sheet has accelerated, with some research indicating a probable complete collapse. However, the impact on AMOC remains uncertain.

The timing of the melting is crucial, according to simulations by Sinet and his team. If pulses of ancient Antarctic meltwater coincide with substantial meltwater from Greenland, the AMOC’s closure will be expedited.

Conversely, if the Antarctic water arrives about 1,000 years prior to the peak melting of Greenland, the AMOC may weaken for a few centuries but then recover over the next 3,000 years. While AMOC shows eventual recovery in all scenarios, early Antarctic melting prevents total collapse and accelerates its resurgence.

This phenomenon could be due to the relocation of the sinking, salty AMOC water moving south as lighter, fresher meltwater accumulates around Greenland, with the flow regaining strength as Antarctic melting decreases.

Though it’s improbable that West Antarctica melts at such a rapid pace while Greenland melts more slowly, these results illuminate a significant connection between AMOC and Antarctic ice melt, notes Louise Sim from the British Antarctic Survey.

“Prior to this study, the extent to which Antarctic changes could significantly influence the effects of Greenland’s ice sheet melting on the AMOC was largely unknown,” she remarks.

However, the study does not address potential feedback effects, such as shifts in wind patterns that might increase Antarctic sea ice, so this relationship needs to be explored in more complex models moving forward, she adds.

Even if rapid melting in West Antarctica prevents the AMOC from collapsing, it could still lead to sea-level rises of up to 3 meters, inundating coastal cities.

“Unfortunately, while one potential disaster may lessen the danger of another, this is little consolation,” concludes Stefan Rahmstorf from the University of Potsdam, Germany.

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Source: www.newscientist.com

Scientists Risk Losing Crucial Tools for Studying Melting Antarctic Ice Sheets Amid Rising Climate Threats

The decommissioning of Palmer has played a significant role in contributing to sea level rise, particularly as certain regions of Antarctica face limited access, raising concerns among scientists regarding potential ice sheet collapses.

In a statement to NBC News, the National Science Foundation (NSF) announced plans to streamline resources by consolidating McMurdo, Amunsense Cott South Paul, and Palmer Station, with the goal of maintaining three research stations operating throughout the year in Antarctica.

A spokesperson for the U.S. Antarctic Program (USAP) mentioned that they aim to “maintain an active and influential presence in Antarctica while facilitating cutting-edge research in biology and glaciology.”

The NSF was the first to propose the termination of the lease this spring, following the Trump administration’s proposed budget cuts of 55%. Scientists expressed their disappointment that Congress initiated the process of abolishing the ship before finalizing its budget.

“Oceanologist Karos Moffat, an associate professor at the University of Delaware, discussed the budgets that have made advancements in both Senate and House appropriations committees.

The NSF is exploring alternative vessels to take on some of Palmer’s responsibilities and plans to return the vessel to its owner, Edison Chowest, a marine transport company based in Louisiana.

In 2024, the NSF finalized the charter of another Antarctic vessel, RV Laurence M. Gould, which has been upgraded to operate in sea ice, rather than utilizing icebreakers. This reduces the options available for enhancing research in polar oceanography and supporting Palmer Station, an annual base on the Antarctic Peninsula that previously depended on two ships.

The NSF mentioned on Friday that there are “alternatives” available to support and resupply Palmer Station, including commercial options.

Measuring 308 feet, the Palmer, named after a 19th-century seal captain, commenced its service in 1992, exploring various regions of Antarctica. The vessel accommodates approximately 22 crew members and can host around 45 scientists.

No other U.S. research vessels can fulfill all the missions that this polar icebreaker is designed for. The vessel is crucial for studying Antarctic ecology, the Southern Ocean carbon cycle, and monitoring the rate at which ice shelves recede and melt, ultimately influencing sea level rise.

Julia S. Werner of the University of Houston, second from the right, friend of Nathaniel B. Palmer.Courtesy Julia S. Werner

While satellites offer valuable data on the dynamics of ice sheet growth and reduction, the primary research on these changes relies on subsurface measurements.

Without such data, U.S. scientists will lack critical insights into the major ice sheets of the Southern Ocean, which are key to predicting future flooding risks in U.S. coastal cities. For instance, researchers highlight that other U.S. vessels are not suitable for safely accessing the notorious Swaitonga glacier, often referred to as the “end of the Apocalyptic Glacier.”

Researchers frequently describe the West Ku as a cork for a bottle that could rapidly drain the West Antarctic ice sheet, serving as a protective barrier against its collapse into the Amundsen Sea. This could result in a sea level rise exceeding 10 feet over a span of hundreds of thousands of years.

By the year 2100, the likelihood of such a collapse could elevate sea levels significantly beyond the 1-3 feet previously anticipated, as indicated in recent reports by the Intergovernmental Panel.

This disintegration could also alter ocean circulation patterns, affecting how quickly the ocean absorbs carbon, which remains an active area of research. Several studies suggest that current Earth temperatures may have surpassed the threshold for collapse, although further investigation is necessary.

Current shifts in mass and stability are influenced by factors occurring hundreds or thousands of feet beneath the water’s surface, necessitating optimal access through robotic instruments.

“To grasp the drastic changes occurring, it’s essential to be at the edge of the ice where it interacts with the ocean,” Werner explained. “And that’s precisely what this boat allows us to do.”

Scientists typically travel to Palmer every two years, using the data collected over the course of a month or more to advance their laboratory research.

The information gathered aboard the vessel is invaluable, enabling scientists to study ice comprehensively for over a decade, adding vital icebreakers to the U.S. science fleet and alleviating the longstanding backlog of researchers seeking fieldwork opportunities at Palmer.

Source: www.nbcnews.com

Signs of Climate Threats Are Evident in Europe’s Melting Glaciers

As she crossed into Austria, Andrea Fisher, the assistant director of the multidisciplinary mountain research institute at the Austrian Academy of Sciences, remarked that such popular movements are growing increasingly vigorous and frequent.

“Within the next five years, a third of Austria’s glaciers will vanish,” Fischer announced, standing at the remnants of the Stub Glacier, located approximately 72 miles northeast of Mortersch. Stub, one of Austria’s most frequented ski destinations, is projected to completely disappear by 2033.

“The demise of the alpine glaciers is drawing near. We are witnessing it firsthand. This isn’t a model on a computer; it’s a stark reality,” Fisher stated as she maneuvered the muddy truck to the precipice of the ice.

Andrea Fisher.
Sean Keene / NBC News

As global efforts to reduce greenhouse gas emissions falter, temperatures worldwide continue to increase. According to NASA, last year marked the hottest on record. The United States’ exit from the Paris Climate Agreement has critically weakened global climate initiatives, complicating the already challenging objective of limiting warming to 1.5 degrees Celsius (approximately 3 degrees Fahrenheit).

Europe exhibits the fastest temperature growth on the planet, with Austrian temperatures rising by 3.1 degrees Celsius since 1900—more than double the global average. Fisher emphasized the importance of glacier studies to forecast future climate trends.

“Glaciers serve as archives of climate history,” she explained. They contain records of precipitation and atmospheric patterns spanning centuries. “I’m diligently searching for all the cold ice that preserves this crucial information before it disappears,” she concluded.

Source: www.nbcnews.com

Gold can raise its temperature 14 times its melting point without actually melting.

Researchers deployed lasers to overheat gold samples, measuring temperatures with ultra-bright X-ray pulses

Greg Stewart/SLAC National Accelerator Research Institute

A thin layer of wafers that fire laser shots can heat to 14 times the melting point, pushing solids well beyond predicted limits, with some solids potentially lacking any defined melting point.

Overheating is a well-known phenomenon where a solid can exceed its melting point or even its boiling point without altering its state. For instance, water heated in a microwave can reach temperatures above 100°C (212°F) if the container is smooth and undisturbed, but will boil vigorously as soon as disturbed.

Many physicists have suggested an upper overheating limit of approximately three times the standard melting point in Kelvin, termed the entropy catastrophe. This occurs because the entropy, often viewed as the degree of disorder in a system, is greater when the material transitions to a liquid state. Remaining solid at temperatures above this point contradicts the second law of thermodynamics.

Recently, Thomas White from the University of Nevada, Reno, and his team found that gold can heat up to 14 times its melting point, exceeding even the entropy catastrophe.

White and his colleagues directed a powerful laser at a 50-nanometer-thick gold sheet for 45 seconds, then measured the temperature using reflective X-rays through a novel approach. By analyzing shifts in the frequency of the reflected X-rays, they determined the excess energy transferred to the gold, allowing them to calculate the heating effect on the sheet.

“The temperatures we measured were astonishingly high,” White remarked.

After ensuring no errors in their measurements, White and his team revisited existing theories, realizing that the rapid heating of gold likely reduced the solid’s entropy compared to its potential liquid state, surpassing predicted temperature limits. “It’s crucial to state that we haven’t violated the second law of thermodynamics,” White clarified.

The actual limitations of overheating are still open questions, he noted. “I may have thought the overheating limit was resolved in the 1980s, but now I believe it’s a question worthy of further exploration. Can we heat materials beyond their melting point?”

Utilizing this X-ray technology for measuring solid heating may also help simulate the effects of extreme heat and pressure from planetary interiors on materials within very short timescales, according to Sam Vinco at Oxford University. “Currently, there isn’t an effective thermometer for solids that operates on such brief timescales,” he noted.

It will also be fascinating to ascertain if this phenomenon applies to other solids beyond gold, Vinco stated, particularly regarding whether there’s a limit to heating before melting occurs. “What’s captivating is considering whether rapid heating could essentially circumvent traditional thermodynamic principles,” he added.

Source: www.newscientist.com

Melting moon dust to create solar panels on the moon

Boot print on the dusty surface of the moon

Public domain sources from CBW/Alamy/Access rights

The base of future moons could be powered by solar cells made on-site from the melted moon dust.

Building items on the moon using materials already there is more practical than shipping them from the Earth. when Felix Lang He heard about this idea at the University of Potsdam in Germany and knew what to do right away. “We have to make solar cells like this, we have to make them right away,” he says.

Two years later, Lang’s team built and tested several solar cells that featured lunar dust as an ingredient. Another important component is a crystal called halide perovskite, which contains elements such as lead, bromine, and iodine, as well as long molecules of carbon, hydrogen and nitrogen.

The team melted a synthetic version of the lunar regolith, a layer of loose rock and dust that covers the moon, into “Moonglass.” Because they did not refine the regolith, the mungrass was less transparent than traditional solar cells. However, Lang says the team’s best prototype still reached around 12% efficiency. More traditional perovskite solar cells typically reach an efficiency close to 26%. Lang said the computer simulation suggests that his team could reach that number in the future.

In general, researchers agree that perovskite solar cells are superior to more traditional silicon-based devices in both space and Earth. From a lunar perspective, the use of perovskite materials is also attractive. This is because it can be kept very thin and reduces the weight of the material transported on the moon. Team estimates that a solar cell with an area of ​​400 square meters requires only about a kilogram of perovskite. This is an impressive claim, I say Ian Crawford at Birkbeck, University of London.

It is equally important that the regolith does not need to be purified. This means that no special reactor is needed. In fact, Lang says that the large curved mirror and sunlight can create a beam of light that is warm enough to make the mungrass. One of his colleagues has already tested the technology on their university roofs and saw signs of legolith melting, he says.

Nicholas Bennett At the University of Technology, Sydney says that while past research has tried to process the lunar regolith into clear glass, this is the first time that solar cells have been shown to work with fine moonglass instead. The challenge now, he says, is to make a lot of mungrass outside the lab. If successful, such melting techniques could help create other items that the moon base needs, such as tiles, Crawford says.

Michael Duke The Lunar and Planetary Institute states that manufacturing moongrass-based solar cells will require many technological advances, from excavating the legend to connecting individual cells. Still, if a solar plant is established on the moon, there could be a positive knock-on effect. In this future, space-based systems like satellites will need less energy to fire payloads from the moon, allowing solar cells covered in the moon rather than what was created on Earth.

Lang and his colleagues are currently working on increasing the efficiency of solar cells. For example, we know whether choosing iron before using magnets to melt Regolith can improve the quality of mungrass.

Ultimately, they want to expand the process to other dusty residents. “We’re already thinking, ‘Can we make this work on Mars Regolith?”,” says Lang.

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Source: www.newscientist.com

Researchers find that melting ice sheets are causing a reduction in the speed of the world’s strongest ocean currents

Antarctic Circulating Current (ACC), which is more than four times as strong as the Gulf Stream, is the world’s strongest ocean current and plays an unbalanced role in the climate system due to its role as a major basin conduit. Scientists at the University of Melbourne and the Research Centre in Nordic Norway have shown that ACC will slow by about 20% by 2050 in high carbon emission scenarios. This influx of freshwater into the southern ocean is expected to alter the properties such as the density (salinity) of the ocean and its circulation patterns.



Sohail et al. High-resolution ocean and sea ice simulations of ocean currents, heat transport, and other factors were analyzed to diagnose the effects of temperature changes, saltiness, and wind conditions. Image credit: Sohail et al. , doi: 10.1088/1748-9326/adb31c.

“The oceans are extremely complex, finely balanced,” says Dr. Bishakhdatta Gayen, liquid mechanic at the University of Melbourne.

“If this current ‘engine’ collapses, serious consequences, including more climate change, including extreme extreme climate variability in certain regions, will accelerate global warming due to a decline in the ability of the ocean to function as a carbon sink. “

The ACC acts as a barrier to invasive species, like the southern burkelp and marine vectors such as shrimp and mollusks, which travel in the current from other continents reaching Antarctica.

If this current slows and weakens, it is more likely that such species will head towards the fragile Antarctica, potentially serious effects on food webs, which could change the available diet of Antarctic penguins, for example.

The ACC is an important part of the marine conveyor belt around the world, moving water around the world and linking the Atlantic, Pacific and Indian seas. These are the main mechanisms of exchange of heat, carbon dioxide, chemicals and biology throughout these basins.

In their study, the authors used Gadi, the fastest supercomputer in Australia located on the Access National Research Infrastructure.

They discovered that transport of seawater from the surface to the deepest could also be slower in the future.

“If ice melting accelerates as predicted by other studies, slowdowns are predicted to be similar in low emission scenarios,” Dr. Sohail said.

“The 2015 Paris Agreement aims to limit global warming to 1.5 degrees Celsius above pre-industrial levels.”

“Many scientists agree that we have already reached this 1.5 degree target, which could have an impact on the melting of Antarctic ice, making it even hotter.”

“Cooperative efforts to limit global warming (by reducing carbon emissions) will limit the melting of Antarctic ice and avoid the expected slowdown in ACC.”

This study reveals that the effects of ice melting and ocean warming on ACC are more complicated than previously thought.

“The melted ice sheets throw a large amount of fresh water from salt water into the salty sea.”

“This sudden change in ocean salinity has a series of results, including weakening of subsidence to the depths of surface seawater (called Antarctic bottom water), and based on this study, it includes weakening of the powerful marine jets surrounding Antarctica,” Dr. Gayen said.

study Published in the journal Environmental Survey Letter.

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Taimoor Sohail et al. 2025. Decreasing the polar current in the Antarctic due to polarization. environment. res. Rent 20, 034046; doi:10.1088/1748-9326/adb31c

Source: www.sci.news

Dark Algae Accelerates Greenland Ice Sheet Melting

Greenland ice sheet algae absorb light and accelerate melting

Laura Halbach

Dark algae growing on the surface of the Arctic ice sheet are likely to expand future coverage, and tend to exacerbate melting, sea level rise and warming.

“These algae are not a new phenomenon.” James Bradley At the Institute of Oceanography in Marseille, France. “But if they bloom more intensely or the flowers bloom more widely, this is an important thing to consider in future projections of sea level rise.”

Greenland's ice sheets, which cover most of the island, are rapidly melting due to rising temperatures, making them the biggest contributor to sea level rise worldwide.

ancylonema Algae under a microscope

Natural Communication

ancylonema Algae species bloom in patches of ice called ablation zones, which are exposed as snow lines recede to the ice sheet every summer. Flowers darken the ice, reduce its reflectivity, absorbing more heat, thereby increasing melting in these regions by an estimated 10-13%.

To better understand this feedback loop, Bradley and his colleagues gathered ancylonema Samples from the southwest tip of the ice sheet were examined for cells using advanced imaging techniques.

The results reveal that algae are highly adapted to malnutritional conditions and suggest that they can invade ice at high elevations with low nutrients.

Global warming already causes snow lines to increase altitude over time, exposing more ice. Ice algae should add yet another layer to these interactions and explain it in future climate forecasts.

“We have been studying glacial algae flowers for several years, and one of the biggest questions that remains is that we can grow to such high numbers in such undernourished ice.” I say that. Christopher Williamson At the University of Bristol, UK, where he was not involved in the project. “A big part of understanding this puzzle is the amount of nutrients needed for glacial algae cells and whether it can efficiently take and store rare nutrients available in the system. This research is cutting edge. They do an amazing job of demonstrating these things using the methodology of

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Source: www.newscientist.com

Arctic Faces High Temperatures, Melting Ice, and Fires in 2024 According to NOAA Report

overview

  • This year was the second hottest year on record in the Arctic, according to a new report from NOAA.
  • The authors said the tundra has become a carbon source rather than a carbon sink.
  • The North Pole is heating much faster than lower altitude locations because melting ice reflects less radiation back into space.

The Arctic just experienced its second warmest year on record. And worryingly, the region's tundra is transitioning from a carbon sink to a carbon emitter as permafrost thaws and methane is released.

This would only increase the amount of heat-trapping gas entering the atmosphere, paving the way for further global warming.

The findings, shared Tuesday in the National Oceanic and Atmospheric Administration's Arctic Report Card, show how climate change is disrupting ecosystems and altering the landscape in regions where global warming is most intense.

The Arctic, considered a leading region for the effects of climate change, is heating much faster than lower-altitude locations, depending on the baseline scientists use for comparisons and which geographies they include in their assessments. But that speed is 2-4 times faster. Each of the last nine years in the Arctic has been the hottest on record since 1900.

This dynamic is the result of a phenomenon called arctic amplification. As snow cover and sea ice are lost in the Arctic, more dark-colored water and rocks are revealed. Their dark surfaces reflect less radiation back into space, instead absorbing heat. In addition, ocean and atmospheric circulation patterns increasingly transport heat toward the Earth's poles.

Taken together, that means the Arctic is a fundamentally different place than it was just a decade ago. Twila Moon said.

“The Arctic is in a kind of new regime, not a new normal, of course, but it's definitely different than it was just a few decades ago,” she says.

Overall, the Arctic is becoming a greener landscape with more extreme precipitation, less snow and ice, the report said. As fires in the Arctic send smoke into populated areas, ice melts and sea levels rise, the effects of those changes are becoming increasingly apparent closer to American homes, scientists said.

“These problems aren't just limited to the Arctic; they affect all of us,” says Brendan Rogers, an associate scientist at the Woodwell Climate Research Center in Woods Hole, Massachusetts. .

This year's report includes a detailed explanation of how the carbon cycle in the Arctic is changing. Scientists have been closely watching what happens when permafrost thaws, releasing powerful greenhouse gases as it thaws and decomposes.

“Permafrost regions contain about twice as much carbon as is currently present in the atmosphere, and about three times as much carbon as is contained in the above-ground biomass of forests around the world. There's a lot of carbon out there,” Rogers said.

He added that permafrost areas “have been carbon sinks for thousands of years on average, primarily due to low temperatures and frozen soil.” Carbon sinks, by definition, absorb and capture more carbon dioxide than they emit. But now such areas are instead sources of greenhouse gas emissions, as they dissolve carbon and methane and release it into the atmosphere, Rogers said.

Wildfires also contribute to Arctic emissions. Last year's wildfires burned more than twice as much area in the region as the year before, and produced more emissions than Canada's economic activity.

Rogers said Canada's total wildfire emissions are “roughly three times the emissions from all other sectors in Canada.” “This is more than the annual emissions of any other country except China, the United States, India and Russia.”

Last year's wildfires forced the evacuation of Yellowknife, the capital of Canada's Northwest Territories. About 19,000 people had to evacuate the cityin Areas with discontinuous permafrost.

Temperature records are organized by Arctic water year, so the most recent records are from October 2023 to September 2024. Every September, scientists measure the extent of Arctic sea ice at its seasonal minimum.

This year's sea ice was the sixth lowest in the 45 years since satellite measurements began. Sea ice extent has decreased by about 50% since the 1980s. Meanwhile, the Arctic tundra is the second greenest since records began in 2000, indicating more shrubs have taken root and spread into new terrain.

Measurements of Arctic permafrost taken from boreholes drilled beneath the earth's surface show that average temperatures were warmer than in all but one year.

“There are many indicators that consistently show extreme or near-extreme conditions,” Moon said.

Source: www.nbcnews.com

Hikers and melting snow reveal ancient ecosystem in the Alps before dinosaurs

Deep beneath the snow-covered slopes lie prehistoric wonders waiting to be discovered. Recently, hikers in the Italian Alps stumbled upon an ancient ecosystem that predates even the dinosaurs, thanks to melting snow.

The groundbreaking discovery was announced on Wednesday, revealing well-preserved reptile and amphibian footprints dating back 280 million years to the Permian period, according to scientists.

Cristiano Dal Sasso, a paleontologist at the Natural History Museum of Milan, described the impressive footprints left by animals at that time, with some measuring 2 to 3 inches long. These fascinating finds are now on display at the museum.

The fossil was unearthed in the mountains of Lombardy, Italy, where the melting snow and ice exposed these ancient treasures due to the ongoing climate crisis.

Researchers move rocks containing fossil footprints in the Italian Alps.
Elio della Ferrera / Milan Museum of Natural History

In the summer of 2023, Claudia Steffensen stumbled upon one of these fossils while hiking in the Valtellina Orobie mountains. This discovery led to a series of investigations by experts like Orsonio Ronchi and Lorenzo Marchetti, unraveling the mysteries of this ancient ecosystem.

Researchers were amazed by the abundance and preservation of the fossils, which provide valuable insights into the Permian period just before the dinosaurs roamed the Earth.

Computer-generated images show what prehistoric reptiles looked like.
Fabio Manucci / Milan Natural History Museum

The rapidly changing climate has played a significant role in revealing these fossils, as rising temperatures have caused snow and ice to melt, exposing the long-hidden remains.

As more footprints and fossils emerge from the mountains in the coming years, researchers warn that studying the past can shed light on the environmental challenges we face today. It serves as a stark reminder of the impact our actions can have on the world.

Source: www.nbcnews.com

The impact of the melting Greenland Ice Sheet on ocean currents

Climate change affects our planet and our lives in many ways. Dry the atmosphere To Increase in home runs Climate change accelerates glacial melt with each Major League Baseball season. Greenland Ice Sheet The land ice mass that covers about 80% of Greenland. When glaciers melt, icebergs form, a process called “iceberg formation.” Glacier collapse Recent climate change has increased the rate at which icebergs are flowing from the Greenland Ice Sheet into the North Atlantic.

Scientists have found that in the past, large increases in the rate of glacial collapse have disrupted important ocean current systems in the Atlantic Ocean. Atlantic Meridional Gyre Or as the AMOC, it carries warm water north and cold water south, affecting global temperatures and moving nutrients across the Atlantic Ocean, meaning that disrupting the AMOC could change the climate and destabilize marine ecosystems. Recently, scientists conducted a study to determine whether the current increase in glacier collapse could disrupt the AMOC.

For this study, the researchers developed a method to quantify glacial runoff during past periods of increased glacial collapse in the North Atlantic that disrupted the AMOC. Heinrich Event They began by looking at present-day glaciers in the North Atlantic and the Arctic. As icebergs break up, they deposit sediment. This sediment includes sand and rocks from the land below the ice sheet, as well as the remains of organisms that lived on the ice sheet. When the icebergs melt at sea, the sediment is released and sinks to the ocean floor.

Scientists observed modern glaciers melting and measured the average amount of sediment, by volume, that they released. Using this average, the researchers estimated how much ice was released during past Heinrich events, based on the amount of sediment that was deposited on the floor of the North Atlantic Ocean.

Scientists used this method to estimate the total amount of ice lost during 10 Heinrich events (the last of which) that occurred over the past 140,000 years. Glacial Cycle Previous scientists had determined the duration of Heinrich events, which allowed the researchers to estimate the ice runoff rate during each event. The researchers compared their estimated runoff rates to current ice runoff rates and found that current ice runoff rates are similar to those of previous mid-sized Heinrich events that disrupted the AMOC. However, the scientists who conducted the study also noted that the AMOC is currently stable.

The researchers suggested two factors that could help explain why the current increase in glacial collapse is not disrupting the AMOC as much as it has in the past. First, the researchers think that the AMOC was stronger when the current glacial runoff rate began to increase than it was at the start of past Heinrich events, which may make the current AMOC more resistant to disruptions. Second, each of the 10 Heinrich events the scientists used in their study lasted about 250 years, while the faster glacial collapse seen today may have been due to a slowdown in the early Heinrich events. It began in recent decades They suggested that AMOC collapse could only occur after a longer period of increased glacier calving than has happened previously.

If the rate of glacial calving continues to increase by the time the AMOC collapses, the size of the Greenland Ice Sheet may limit its influence on the AMOC. The researchers noted that if the Greenland Ice Sheet continues to melt at its current rate, the rate of calving will slow before 250 years have passed. The icebergs that caused the Heinrich events in the last glacial cycle broke off from a much larger ice sheet. Laurentide Ice Sheet It no longer exists.

The scientists who conducted the study said that freshwater runoff from the melting Greenland Ice Sheet could also disrupt the AMOC, but its impact would be less severe than ice runoff. However, they noted that freshwater runoff is likely to increase as glacial collapse slows in the coming decades, which could have unpredictable consequences. The researchers suggested that the scientific community should continue their work to model the impacts of a melting Greenland Ice Sheet as accurately as possible, because, in their words, “the fate of the AMOC remains uncertain.”


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Source: sciworthy.com

The melting Antarctic ice may decelerate the rise in sea levels

Weddell Sea ice shelf in Antarctica

Sergio Pitamitz/VW Pics/Universal Images Group via Getty Images

Uplifting the land beneath the Antarctic ice sheet could help slow ice loss and limit sea level rise over the coming centuries, but if emissions continue to rise, it could cause more sea levels to rise than the ice melt alone.

The findings come from models that simulate Earth’s mantle, the layer beneath the crust, in greater detail than ever before. When Antarctica loses its weight as ice melts, the elastic mantle beneath it bounces back, causing the land above it to rise. When ice melts and the continents lose their weight, Earth’s elastic mantle bounces back, causing the land above it to rise. The bounced back land can slow the flow of ice sheets where they meet the ocean. This “sea-level feedback” occurs primarily because the uplifted land changes the shape of the ocean floor, limiting the thickness of the ice sheet’s edges. Thinner ice there reduces the overall inflow of ice into the ocean.

Researchers have long suspected that this effect plays a role in slowing ice loss, but it was unclear when this effect begins or how it varies in different parts of the ice sheet.

Natalia Gomez Gomes and his colleagues at McGill University in Canada modeled the relationship between the melting ice and the rebounding land, and also simulated the mantle, capturing the different viscosities beneath the continents: East Antarctica sits on a more viscous mantle and thicker crust, while West Antarctica’s rapidly melting glaciers sit on a less viscous mantle and thinner crust. This more detailed picture of Earth’s interior is based on precise measurements of ice sheet elevation changes over decades, as well as data about the mantle beneath Antarctica from seismic waves generated by earthquakes. “This is hard-earned,” Gomes says.

The researchers found that under a very low emissions scenario, compared to a model that considered the ground beneath the ice solid, land uplift would reduce Antarctica’s contribution to global mean sea level rise by more than 50 centimeters by 2500. This effect was less pronounced under a moderate emissions scenario, but still led to a large reduction in sea level rise, with effects starting to be felt as early as 2100.

But in a very high emissions scenario, the team found that land uplift in Antarctica would raise sea levels by an additional 0.8 meters by 2500. This happened because the ice sheet retreated faster than land uplift, and the rising sea floor pushed more water into the rest of the ocean.

“From a modeling perspective, this is a huge step forward.” Alexander Bradley The British Antarctic Survey’s Bradley says it’s always been thought that land uplift would limit sea-level rise, but this high-resolution modeling shows that the effect depends on emissions. “The changes that occur in the 21st and 22nd centuries will depend very much on what we do now,” he says.

Alexander Lovell Researchers at the Georgia Institute of Technology in Atlanta call it a “very good simulation,” but the scenario in which land uplift drives sea level rise is based on worst-case assumptions about emissions and the rate at which ice sheets are retreating.

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Source: www.newscientist.com

Melting Ice Causing Earth’s Rotation to Slow and Axis to Shift, Research Finds

A recent study reveals that climate change is fundamentally reshaping the Earth, impacting its core. The melting of polar ice caps and glaciers due to global warming is causing a redistribution of water towards the equator, resulting in a shift in the Earth’s rotation and leading to increased daylight hours. This phenomenon is supported by new evidence suggesting that changes in the Earth’s ice could potentially affect its axis. These alterations create feedback loops within the Earth’s molten core, as highlighted in studies published in Nature Geoscience and the Proceedings of the National Academy of Sciences.

According to Benedict Soja, an assistant professor at ETH Zurich in Switzerland, human activities are significantly influencing the Earth’s rotation. Changes in the planet’s shape and mass distribution, influenced historically by forces like the moon’s gravitational pull and rebounding of crust after ice age glaciers disappeared, are now being accelerated by rapid ice melting caused by climate change. Soja warns that continued carbon emissions could make ice loss a more significant factor in Earth’s rotation than the moon.


In addition to external factors like gravity and ice loss, fluid movements in the Earth’s core also play a role in affecting the planet’s rotation. These movements can speed up or slow down the Earth’s rotation and are currently compensating for the slowdown caused by climate change. The new study suggests that climate change is leading to small variations in polar motion due to changes in mass distribution, estimated to be about one meter per decade.

An iceberg in Antarctica on February 8th.
Şebnem Coşkun / Anadolu via Getty Images File

These changes in rotation are expected to have implications for space missions, navigation, and timekeeping. Understanding how Earth’s rotation and axis are affected by climate change will be crucial for accurate space exploration and maintaining global time standards. The research emphasizes the interconnectedness of surface processes with the Earth’s core, shedding light on the complex relationship between human activities and the planet’s inner workings.

Source: www.nbcnews.com

The melting sea ice in the Canadian Arctic is now a hindrance, not a help, to shipping.

Broken sea ice in Lancaster Sound, part of the Northwest Passage

Allison Cook

Shipping companies had hoped that melting sea ice would open up shorter shipping routes through the Canadian Arctic, but thicker ice moving in from further north may dash those hopes.

“North [of the Northwest Passage] “No new routes are expected to open anytime soon.” Allison Cook At the Scottish Association for Marine Science.

For over a century, sailors have navigated the icy waters of the Canadian Arctic along the Northwest Passage, a dangerous but efficient sea route connecting the Atlantic and Pacific oceans. As climate change melts the sea ice, the southern part of the passage is less dangerous, and since 1990, voyages through the Northwest Passage have quadrupled.

The North Strait is expected to be an even shorter route, but it is ice-bound for longer periods than the South Strait, and so fewer ships use it. But because the entire route was almost ice-free in the summer of 2007, and the climate has continued to warm since then, many believe the North Strait route will soon become regularly navigable. This possibility has spurred ideas of a boom in Northern Sea Routes.

Cook and his colleagues assessed whether this vision was working using ice charts provided by the Canadian government to ship captains between 2007 and 2021. For each leg of the Northwest Passage, they calculated the number of weeks per year when ice was light enough for moderately ice-hardened ships to navigate safely.

Map showing the route of the Northwest Passage through the Canadian Arctic Islands

Allison Cook

The detailed images of the ice reveal that rather than the passage opening, the safe passage window shortened at several “choke points” along the route, particularly along the northern route. For example, the passage window in the eastern Beaufort Sea shortened from 27 weeks to 13 weeks. The passage window in McClure Strait shortened from 6.5 weeks per year to just two weeks. In other areas, passage windows increased by a few weeks or remained unchanged, but the passage window that determines the overall passage window is determined by the shortest passage window, Cook said.

Researchers believe the shortened season is primarily due to an increase in thicker sea ice flowing in from an area known as the “last ice field” north of Greenland, which is expected to become the last remaining bastion of sea ice in the Arctic Ocean as the climate warms. “Climate change is making the sea ice a little less intense and a little more mobile,” Cook says.

The findings are consistent with expectations that ice will remain in the Canadian Arctic the longest, he said. Amanda Lynch The bigger geopolitical and economic question now is how the melting ice will affect shipping on the Russian side of the Arctic, said Robert G. Schneider, a researcher at Brown University in Rhode Island who was not involved in the study.

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Source: www.newscientist.com

Hot water leaking beneath Antarctic ice sheet may quicken melting

Aerial photo of the Antarctic ice sheet

David Vaughn/BAS

Antarctica’s melting ice sheet could retreat faster as warmer ocean water invades underneath it, and rising ocean temperatures could trigger a “runaway” feedback effect that pushes warm water further inland, melting even more ice and accelerating sea-level rise.

As the climate warms, the future of Antarctica’s vast ice sheet remains uncertain, and predictions vary widely about how quickly it will melt and therefore how much it will contribute to sea-level rise. One dynamic that researchers have only recently begun to recognize as a key factor is the intrusion of warmer ocean water beneath the ice.

“The mechanisms of invasion are much more powerful than we previously understood.” Alexander Bradley At the British Antarctic Survey.

Such intrusions are driven by density differences between the freshwater flowing out from beneath the ice sheet and the warmer waters where the ice meets the sea floor, known as the grounding line. They are difficult to observe directly because they occur hundreds of meters beneath the ice, but simulations suggest that in some places the warm waters could extend several kilometers inland.

One model by Alexander Lovell Researchers from the Georgia Institute of Technology in Atlanta found that widespread ice-sheet intrusion could add heat from below, lubricating ice flow along bedrock and more than doubling ice loss from the ice sheet.

Bradley and his colleagues Ian Hewitt Using their model, Oxford researchers explained how the shape of cavities in the ice changes as the ice melts, altering how ocean water flows in.

The researchers found that once ocean water reaches a certain temperature threshold, ice from the ice sheet melts faster than it can be replaced by outflowing ice. If this cavity grows larger, more water could flow under the ice sheet and penetrate further inland, creating a so-called “runaway” positive feedback effect.

“Small changes in ocean temperature lead to dramatic changes in how far warm water can intrude,” Bradley said. The ocean warming needed to cause this effect is within the range expected this century, he said, but models cannot yet predict it for specific ice sheets, and not all ice sheets are equally susceptible to such intrusions.

“This positive feedback could lead to much more intrusion than we thought,” Lovell says. “Whether that’s a tipping point that leads to unrestrained intrusion of ocean water beneath the ice sheet is probably a stretch.”

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Source: www.newscientist.com

The “doomsday glacier” is melting at an alarming rate, putting Earth’s largest city in danger of flooding

Considered one of West Antarctica’s most infamous glaciers, the “doomsday glacier” has earned its nickname due to the potentially significant rise in sea levels it could cause, ultimately reshaping coastlines. This glacier, known as Thwaites Glacier, is massive, the size of England and spanning 120km wide. It extends from the peak of the West Antarctic Ice Sheet to the Amundsen Sea, where it reaches out onto an ice shelf.


Unfortunately, Thwaites Glacier is experiencing troubling changes, with a notable increase in ice loss over recent years as a consequence of climate change. The rate of ice loss has doubled in the past 30 years due to rising ocean temperatures, which lead to the melting of the ocean floor beneath the glacier. Warm water is being transported towards Thwaites, particularly deep below the ocean surface, contributing to this rapid ice loss. The land beneath West Antarctic glaciers is below sea level, and the sloping ocean floor means warmer waters can intrude underneath, eroding the glaciers and making them less stable.

A recent study revealed that Thwaites Glacier may be more susceptible than previously believed, with seawater surging beneath it for kilometers. The melting of glaciers, including Thwaites, could result in a significant rise in sea levels, potentially impacting coastal areas worldwide. Additionally, the collapse of Thwaites could trigger nearby glaciers to follow suit, further elevating global sea levels by more than three meters. This irreversible loss on human timescales would mark a critical “tipping point.”

Scientists are concerned about the potential collapse of Thwaites Glacier, as it could have disastrous consequences for sea levels and climate. Researchers are exploring strategies to adapt to these expected changes and protect coastal regions at risk of submersion. The costs of preparing for rising sea levels are substantial, emphasizing the importance of proactive planning and adaptation. While sea level rise is inevitable, proactive measures can help mitigate its impact and protect vulnerable populations and ecosystems.

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Despite the impending challenges, scientists and experts emphasize the importance of courage and adaptation in the face of climate change. Dr. Caitlen Norton from the British Antarctic Survey stresses the need for resilience and preparedness to address the growing threat of rising sea levels. Adapting defenses, protecting coastal areas, and planning for future changes are crucial steps in mitigating the impact of climate change on coastal regions.

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Source: www.sciencefocus.com

The Melting of Polar Ice Could Alter Earth’s Rotation and Timekeeping.

Global warming is causing the Earth’s rotation to slow slightly, which could affect the way we measure time.

A study published Wednesday found that the melting of polar ice, a trend accelerated primarily by anthropogenic climate change, is causing the Earth to spin more slowly than it would otherwise.

Study author Duncan Agnew, a geophysicist at the Scripps Institution of Oceanography at the University of California, San Diego, said melting polar ice changes where the Earth’s mass is concentrated. This change affects the planet’s angular velocity.

Agnew likened the dynamic to a figure skater spinning around on ice. He said, “If a skater starts spinning and lowers his arms or extends his legs, he will slow down.” However, if the skater’s arms are pulled inward, the skater will rotate faster.

So less solid ice at the poles means more mass around the equator, at the Earth’s waist.

“What melting ice does is take water that has solidified in places like Antarctica or Greenland, and when that frozen water melts, it moves that liquid to other parts of the planet. “Thomas Herring said. He was a professor of geophysics at the Massachusetts Institute of Technology but was not involved in the new research. “Water flows toward the equator.”

In other words, this study shows how human influence can successfully manipulate forces that have puzzled scholars, stargazers, and scientists for millennia: forces long thought to be constants beyond human control. It suggests that it has happened.

“It’s kind of impressive, even to me, that we were able to accomplish something that measurably changed the rotational speed of the Earth,” Agnew said. “Something unprecedented is happening.”

His research, published in the journal Nature, suggests that climate change is playing a significant enough role in the Earth’s rotation to delay the possibility of a “negative leap second.” If the polar ice hadn’t melted, clocks around the world might have needed to subtract one second by 2026 to synchronize universal time with the Earth’s rotation, which is influenced by a variety of factors.

Rather, the impact of climate change has delayed that outlook by an estimated three years. If timekeeping organizations ultimately decide to add negative leap seconds, the adjustment could disrupt computer networks.

A view of the Earth captured by a deep space climate observation satellite.NASA

The leap second adjustment is necessary because even without climate change, the Earth’s daily rotation tends to slow down over time, even though it appears constant.

Studies show that about 70 million years ago, days became even shorter, lasting about 23.5 hours. Implications of paleoceanography and paleoclimatology. This means that Cretaceous dinosaurs experienced 372 planetary days a year.

Several important factors influence a planet’s rotation, but they sometimes act in opposition.

Due in part to the moon’s gravitational pull, tidal friction in the oceans slows the Earth’s rotation. Meanwhile, since the last Ice Age, the Earth’s crust has been uplifting in some areas in response to the removal of ice sheet weight. This effect changes the distribution of mass, causing the planet to spin faster. Both of these processes are approximately constant and have predictable rates.

Yet another factor is the movement of fluids within Earth’s liquid inner core, a wild card that can either speed up or slow down Earth’s rotation, Agnew said.

Here, melted polar ice was added to the mix. As climate change intensifies, researchers expect melting ice to have an even more profound effect on the Earth’s rotation.

“As we predict, as melting accelerates over time, its contribution will become even larger,” Herring said. He added that the new study is a thorough and robust analysis that combines research from multiple scientific fields.

The need for timekeepers to adjust universal time to match the Earth’s rotation is not a new phenomenon. But historically, this involved adding leap seconds to the common standard for clocks. This is because astronomical time lags behind atomic time (measured by the vibrations of atoms in atomic clocks) due to the slowing of the Earth’s rotation.

But in recent decades, changes in the Earth’s core have caused the Earth to rotate faster than expected. This has led timekeepers, for the first time since Coordinated Universal Time was officially adopted in the 1960s, to consider whether it makes sense to subtract leap seconds to synchronize universal time with the Earth’s rotation. Ta.

The melting of polar ice counteracted that trend, avoiding any decision points regarding negative leap seconds. According to Agnew’s estimates, if the current rate of Earth’s rotation is maintained, it will likely be delayed by three years from 2026 to 2029.

Adding or subtracting leap seconds is troublesome because it can disrupt satellite, financial, and energy transmission systems that rely on very precise timing. For that purpose, Timekeepers around the world have voted to abolish leap seconds in 2022. By 2035, addition and subtraction will shift universal time from the pace of the Earth’s rotation.

“Since around 2000, there has been a movement to abolish leap seconds,” Agnew said.

Regardless of whether the clocks ultimately change, the idea that melting polar ice is affecting the Earth’s rotation speaks to how important an issue it has become. Studies have already shown that ice loss has significant impacts on coastal communities.

Scientists predict that sea level rise will accelerate as the climate warms, a process that will continue for hundreds of years. Last year, leading polar researchers warned in a report that parts of the major ice sheets could collapse and coastal regions should brace for several feet of sea level rise. If humans allowed global average temperatures to rise by 2 degrees Celsius, Earth could see sea levels rise by more than 40 feet.

Source: www.nbcnews.com

Greenland’s melting ice could trigger a heat wave in Europe this year

Melting ice in Greenland could worsen extreme weather across Europe

REDA & CO srl/Alamy

Europe's 10 hottest and driest summers in the past 40 years have all come after a particularly large amount of fresh water was released from the Greenland ice sheet, meaning southern Europe will experience an especially hot summer this year. Maybe you are doing it.

They say this link occurs because the excess meltwater triggers a series of amplifying feedbacks that affect the strength and position of the atmospheric jet stream over Europe. Marilena Ortmans At the UK National Marine Centre.

“2018 and 2022 were the most recent examples,” she says. 2022 saw extreme heat and numerous bushfires across Europe, with high temperatures reaching 40°C (104°F) in parts of the UK for the first time.

These feedback effects, on top of the underlying warming trend from fossil fuel emissions, mean Europe will become even hotter and drier in coming decades as the melting of the Greenland ice sheet accelerates. Then Mr. Ortmans says:

“This is on top of the warming that is already happening due to increases in greenhouse gases,” she says.

Hotter heat waves and drier droughts are expected as the planet warms, but in some regions, such as Europe, recent heat waves and droughts have been even more extreme than climate modeling projects. Several studies have linked these extreme events to changes in the strength and position of the Arctic jet stream. The Arctic jet stream is a band of upper-level winds whose location and strength have a significant impact on weather.

But it's not clear what causes these changes, Ortmans says. Now, she and her colleagues are analyzing weather observations from the past 40 years, and the results show that extreme weather is ultimately the result of a period of increased ice melt in Greenland. It is said that there is.

“Observational statistical associations are very powerful,” she says.

The excess meltwater leads to a shallow layer of freshwater that extends south of the North Atlantic Ocean. This layer does not easily mix with the warm, salty ocean water below, causing the ocean surface to be colder than normal in winter.

This makes the gradient between this colder water and warmer water further south even more extreme, strengthening the weather front aloft. As a result, wind patterns strengthen, pushing warm water flowing northward, the North Atlantic Current, further north than usual. This further amplifies the temperature gradient.

“The front that forms between an area of ​​cold fresh water and an area of ​​warm ocean water is the main source of energy for storms,” ​​she says.

In a 2020 study, Ortmans suggested: This process leads to an increase in storms. during one winter.

Now, Oltmans' team suggests that these winter changes have lasting effects into the following summer. “Two years after the freshwater anomaly occurred, we are still seeing significant signs,” she says.

The researchers found that stronger temperature gradients lead to stronger jet streams across Europe, making the weather in southern Europe even hotter and drier. Then, as the unusually cold water recedes, the jet stream moves north, bringing hot, dry weather to northern Europe.

“We have discussed the individual links in this feedback chain before,” Ortmans says. “What we did in this study is bring these links together.”

Computer models miss this chain of feedback because they don't include factors such as large fluctuations in meltwater from year to year, she says.

“The association between Atlantic freshwater anomalies and subsequent European summer weather proposed in this study is interesting and relevant to current scientific research on long-term predictions of summer weather, especially “If that relationship holds true for future summers,” he says. adam scaife He works on long-term forecasts at the UK Met Office.

“I think this study is somewhat convincing,” he says. Fei Luo At the Singapore Climate Research Center. But when it comes to predicting summer weather, looking at the previous year's snowmelt isn't as helpful as looking at winter weather conditions, Luo said.

But Oltmans is confident enough to predict that Europe will experience more heatwaves and droughts in the coming years as Greenland's ice melts further in the summer of 2023. “I think southern Europe will experience strong heat anomalies this summer,” she says.

These are likely to become even more powerful in 2025, after which they will begin to impact Northern Europe. “We expect Northern Europe to experience another strong heatwave and drought, not this year, but in the next few years.”

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Source: www.newscientist.com