Showing posts sorted by relevance for query melting permafrost. Sort by date Show all posts
Showing posts sorted by relevance for query melting permafrost. Sort by date Show all posts

Monday, January 22, 2024

ICYMI
Ancient zombie viruses in melting permafrost could cause new pandemic, scientists warn

Andy Gregory
Sun, 21 January 2024 

Ancient “zombie viruses” frozen in melting Arctic permafrost could fuel a new pandemic if unleashed by climate change, scientists have warned.

Global heating is enabling increased human activity in the Earth’s northernmost reaches, as melting sea ice opens up shipping and industrial possibilities, including mining deep into the permafrost which covers a fifth of the northern hemisphere, mainly in Canada, Siberia and Alaska.

But scientists have reportedly started to plan an Arctic monitoring network to watch out for any early cases of a disease sparked by ancient viruses, also known as Methusela microbes.

A cemetery sits on melting permafrost tundra at the Yupik Eskimo village of Quinhagak in Alaska (Mark Ralston/AFP via Getty Images)


Ancient viruses have already been found in Siberian permafrost, including one sample which was 48,500 years old. A team led by geneticist Jean-Michel Claverie has revived several such viruses, capable of infecting only single-cell organisms.

But the scientist fear viruses capable of infecting humans likely also lurk in the permafrost. “We see the traces of many, many, many other viruses,” Professor Claverie told CNN in March, adding: “If the amoeba viruses are still alive, there is no reason why the other viruses will not be still alive, and capable of infecting their own hosts.”

As a result, Prof Claverie is among scientists working with the University of the Arctic network on plans to establish quarantine facilities and provide medical expertise that could pinpoint and attempt to treat any early cases without them leaving the region, according to The Observer.

“At the moment, analyses of pandemic threats focus on diseases that might emerge in southern regions and then spread north,” Prof Claverie, of Aix-Marseille University in France, told the paper. “By contrast, little attention has been given to an outbreak that might emerge in the far north and then travel south – and that is an oversight, I believe.

“There are viruses up there that have the potential to infect humans and start a new disease outbreak.” Among the genomic traces of human pathogens identified already by the team in Siberian permafrost are pox viruses and herpes viruses, he said.

According to scientists, Alaska has been warming twice as fast as the global average (Mark Ralston/AFP via Getty Images)

Virologist Marion Koopmans agreed, telling the paper: “We don’t know what viruses are lying out there in the permafrost but I think there is a real risk that there might be one capable of triggering a disease outbreak – say of an ancient form of polio. We have to assume that something like this could happen.”

With forecasts suggesting the Arctic Sea will be ice-free as early as 2040 due to climate breakdown, it is the prospect of increased human activity in the Arctic, as opposed to melting permafrost, which most concerns Prof Claverie.

“Huge mining operations are being planned, and are going to drive vast holes into the deep permafrost to extract oil and ores,” he said. “Those operations will release vast amounts of pathogens that still thrive there. Miners will walk in and breath the viruses. The effects could be calamitous.”

“Our immune systems may have never been in contact with some of those microbes, and that is another worry,” said Prof Claverie. “The scenario of an unknown virus once infecting a Neanderthal coming back at us, although unlikely, has become a real possibility.”

Prof Koopmans added: “If you look at the history of epidemic outbreaks, one of the key drivers has been change in land use. Nipah virus was spread by fruit bats who were driven from their habitats by humans. Similarly, monkeypox has been linked to the spread of urbanisation in Africa.

“And that is what we are about to witness in the Arctic: a complete change in land use, and that could be dangerous, as we have seen elsewhere.”

Tuesday, October 01, 2024

 

NCSA, Google work together in Alaska as part of Permafrost Discovery Gateway




National Center for Supercomputing Applications





Earlier this summer, members of the National Center for Supercomputing Applications traveled to Alaska as part of their continued work with the Permafrost Discovery Gateway, a project led by the Woodwell Climate Research Center using artificial intelligence (AI) and machine learning (ML) in tracking Arctic permafrost thaw.

NCSA’s Associate Director for Software Kenton McHenry and Research Software Engineer Todd Nicholson visited Fairbanks, Alaska along with 12 Google.org fellows to see first hand the melting permafrost and the impacts to those that live there.

“I have seen the artifacts of melting permafrost for years through the satellite images we work with, yet I was shocked to see things firsthand,” said McHenry. “What should be flat terrain was filled with 6-feet-deep ravines, the borders of these ice-wedge polygons. The trees at 45 or greater degree angles. The sinkholes in the University of Fairbanks parking lot.”

Seeing the permafrost research tunnel was a great experience. It shows just how significant permafrost is to the Arctic, how much it affects the land and the environment. Hearing from people about how permafrost thaw affects them in their day-to-day life lets you know how important the topic is.

Todd Nicholson, NCSA Research Software Engineer

Funded by a $5 million grant from Google.org, the Permafrost Discover Gateway, with further Google.org fellowship support, is developing and expanding a new, open-access resource that will use satellite data and AI technology to make it possible to track Arctic permafrost thaw regularly for the first time ever. This potentially game-changing resource for climate science will utilize advances in AI/ML technology to streamline the data analysis process and make it easier to rapidly identify patterns and trends in permafrost thaw datasets that will be essential to informing climate mitigation and adaptation strategies for city planners.

“We are excited to be working with Google.org to improve and extend the tools and data pipelines initially developed for the Permafrost Discovery Gateway to new use cases,” said NCSA Lead Research Software Engineer Luigi Marini after the award was announced. “Closing the time gap between remote sensing data products becoming available and permafrost data products being published, such as the pan-Arctic sub-meter scale ice-wedge polygon dataset developed by Chandi Witharana and team, will hopefully help scientists and stakeholders better understand permafrost thawing at the pan-Arctic scale. We also hope to generalize some of the technologies and tools being developed so that more scientists can leverage this work to develop new permafrost-related data pipelines.”

But NCSA’s trip didn’t just center around software and science. The Arctic adventure included underground tours, an ice hotel, team activities and more.

“On our way to the permafrost cave we stopped by to see a portion of the Trans-Alaska oil pipeline,” McHenry said. “A few of us were amazed that it was actually built on top of permafrost, and to prevent its foundation from melting, it had thousands of passive refrigeration units along it to pump the winter cold into the ground to help prevent the permafrost from thawing in the summer.”

During the same period, the project hosted 12 Google software engineers who assisted in the Arctic research. Through a program partnering with research projects like the Permafrost Discovery Gateway, Google staff apply for opportunities to work on scientific research as a change of pace from their normal work.

“Several of the fellows told us how much they really enjoyed this experience working within science and would like more opportunities to do so,” McHenry said.


ABOUT NCSA

The National Center for Supercomputing Applications at the University of Illinois Urbana-Champaign provides supercomputing, expertise and advanced digital resources for the nation’s science enterprise. At NCSA, University of Illinois faculty, staff, students and collaborators from around the globe use innovative resources to address research challenges for the benefit of science and society. NCSA has been assisting many of the world’s industry giants for over 35 years by bringing industry, researchers and students together to solve grand challenges at rapid speed and scale.

Wednesday, February 05, 2020

UPDATED
Rapid Permafrost Collapse Is Underway, 
Disintegrating Landscapes And Our Predictions

MARLOWE HOOD, AFP 5 FEB 2020
Permafrost in Canada, Alaska and Siberia is abruptly crumbling in ways that could release large stores of greenhouse gases more quickly than anticipated, researchers have warned.

Scientists have long fretted that climate change - which has heated Arctic and subarctic regions at double the global rate - will release planet-warming CO2 and methane that has remained safely locked inside Earth's frozen landscapes for millennia.

It was assumed this process would be gradual, leaving humanity time to draw down carbon emissions enough to prevent permafrost thaw from tipping into a self-perpetuating vicious circle of ice melt and global warming.

But a study published on Monday in Nature Geoscience says projections of how much carbon would be released by this kind of slow-and-steady thawing overlook a less well-known process whereby certain types of icy terrain disintegrate suddenly - sometimes within days.

"Although abrupt permafrost thawing will occur in less than 20 percent of frozen land, it increases permafrost carbon release projections by about 50 percent," said lead author Merritt Turetsky, head of the Institute of Arctic and Alpine Research in Boulder, Colorado.

"Under all future warming scenarios, abrupt thaw leads to net carbon losses into the atmosphere," she told AFP.

Permafrost contains rocks, soil, sand and pockets of pure ground ice. Its rich carbon content is the remains of life that once flourished in the Arctic, including plants, animals and microbes.

This matter - which never fully decomposed - has been frozen for thousands of years.
It stretches across an area nearly as big as Canada and the United States combined, and holds about 1,500 billion tonnes or carbon - twice as much as in the atmosphere and three times the amount humanity has emitted since the start of industrialisation.

Some of this once rock-solid ground has begun to soften, upending indigenous communities and threatening industrial infrastructure across the sub-Arctic region, especially in Russia.
The evidence is mixed as to whether this not-so-permanent permafrost has started to vent significant quantities of methane or CO2. projections are also uncertain, with some scientists saying future emissions may be at least partially offset by new vegetation, which absorbs and stores CO2.

But there is no doubt, experts say, that permafrost will continue to give way as temperatures climb.

'Fast and dramatic'

In a special report published in September, the UN's scientific advisory body for climate change, the IPCC, looked at two scenarios.

If humanity manages - against all odds - to cap global warming at under 2°C, the cornerstone goal of the 2015 Paris climate treaty, "permafrost area shows a decrease of 24 percent by 2100", it concluded.

At the other extreme, if fossil fuel emissions continue to grow over the next 50 years - arguably an equally unlikely prospect - up to 70 percent of permafrost could disappear, the IPPC said.

But both scenarios assume the loss will be gradual, and that may be a mistake, Turetsky suggested.

"We estimate that abrupt permafrost thawing - in lowland lakes and wetlands, together with that in upland hills - could release 60 to 100 billion tonnes of carbon by 2300," she and colleagues noted in a 2019 comment also published by Nature.

One tonne of carbon is equivalent to 3.67 tonnes of carbon dioxide (CO2), which means this would be equivalent to about eight years of global emissions at current rates.

"This is in addition to the 200 billion tonnes of carbon expected to be released in other regions that will thaw gradually," she said.

Current climate models do not account for the possibility of rapid permafrost collapse and the amount of gases it might release, the study notes.

Abrupt thawing is "fast and dramatic", Merritt said, adding: "Forests can become lakes in the course of a month, landslides can occur with no warning, and invisible methane seep holes can swallow snowmobiles whole."
© Agence France-Presse


Arctic sinkholes open in a flash after permafrost melt
Some permafrost zones thaw faster than expected and are reshaping the Arctic landscape.

By Mindy Weisberger - Senior Writer 

Trees struggle to remain upright in a lake formed by abrupt 
permafrost thaw.  (Image: © David Olefeldt)

Arctic permafrost can thaw so quickly that it triggers landslides, drowns forests and opens gaping sinkholes. This rapid melt, described in a new study, can dramatically reshape the Arctic landscape in just a few months.

Fast-melting permafrost is also more widespread than once thought. About 20% of the Arctic's permafrost — a blend of frozen sand, soil and rocks — also has a high volume of ground ice, making it vulnerable to rapid thawing. When the ice that binds the rocky material melts away, it leaves behind a marshy, eroded land surface known as thermokarst.

Previous climate models overlooked this kind of surface in estimating Arctic permafrost loss, researchers reported. That oversight likely skewed predictions of how much sequestered carbon could be released by melting permafrost, and new estimates suggest that permafrost could pump twice as much carbon into the atmosphere as scientists formerly estimated, the study found.

Frozen water takes up more space than liquid water, so when ice-rich permafrost thaws rapidly — "due to climate change or wildfire or other disturbance" — it transforms a formerly frozen Arctic ecosystem into a flooded, "soupy mess," prone to floods and soil collapse, said lead study author Merritt Turetsky, director of the Institute of Arctic and Alpine Research (INSTAAR) at the University of Colorado Boulder.

"This can happen very quickly, causing relatively dry and solid ecosystems (such as forests) to turn into lakes in the matter of months to years," and the effects can extend into the soil to a depth of several meters, Turetsky told Live Science in an email.

By comparison, "gradual thaw slowly affects soil by centimeters over decades," Turetsky said.

Creating feedback

Across the Arctic, long-frozen permafrost is melting as climate change drives global temperatures higher. Permafrost represents about 15% of Earth's soil, but it holds about 60% of the planet's soil-stored carbon: approximately 1.5 trillion tons (1.4 trillion metric tons) of carbon, according to the National Snow and Ice Data Center.

When permafrost thaws, it releases stored carbon into the atmosphere. This release can then speed up global warming; this cycle is known as climate feedback, the scientists wrote in the study.

Aerial image of a permafrost peatland in Alaska's Innoko National Wildlife Refuge, interspersed with smaller areas of thermokarst wetlands. (Image credit: Miriam Jones, U.S. Geological Survey)

In fact, carbon emissions from about 965,000 square miles (2.5 million square kilometers) of quick-thawed thermokarst could provide climate feedback similar to emissions produced by nearly 7 million square miles (18 million square km) of permafrost that thawed gradually, the researchers reported.

And yet, rapid thawing from permafrost is "not represented in any existing global model," study co-author David Lawrence, a senior scientist with the National Center for Atmospheric Research, said in a statement.

Abrupt permafrost thaw was likely excluded from prior emissions models because it represents such a small percentage of the Arctic's land surface, Turetsky explained.

"Our study proves that models need to account for both types of permafrost thaw — both slow and steady change as well as abrupt thermokarst — if the goal is to quantify climate feedbacks in the Arctic," Turetsky added.

The findings were published online Feb. 3 in the journal Nature Geoscience.

Saturday, June 14, 2025

 

CITIES IN PERIL: Boomtowns built on melting ground

CITIES IN PERIL: Boomtowns built on melting ground
An image from the EU's Copernicus Sentinel-2 satellite showing the Russian city of Norilsk on the Taymyr Peninsula. / European Union, Copernicus Sentinel-2 imagery
By bne IntelliNews June 12, 2025

When Russian settlers began building in what is now Yakutsk in the 17th century, they placed homes on wooden platforms to insulate the permafrost below from the warmth of habitation. Centuries later, Soviet planners employed a modernised version of this technique, erecting cities like Yakutsk and Norilsk on concrete piles to elevate buildings above the permafrost and prevent structural collapse.

This allowed major urban centres to emerge in some of the world’s harshest climates. In winter, temperatures in Yakutsk routinely fall below -50°C; it is the coldest major urban area in the world. Despite this, the city, which lies 450 km south of the Arctic Circle, has thrived. It is now home to over 300,000 people and is the largest city in the world built entirely on continuous permafrost.

Yet climate change is rapidly altering the physical foundations on which these cities rest. Rising global temperatures, especially in the Arctic where warming occurs at more than twice the global average, are causing the once-permanent permafrost to thaw.

Thawing permafrost threatens the structural integrity of homes, roads and vital infrastructure. Pipelines rupture, buildings crack, and entire settlements begin to slump into the ground. The costs – financial, social and ecological – are mounting.

According to data published by Nordic research institute Nordregio, as of 2017 nearly 5mn people lived in permafrost zones in and around the Arctic Circle, including in Canada, Alaska and much of northeast Siberia. These include major urban centres like Norilsk and Yakutsk, as well as dozens of smaller towns. Indigenous communities in these regions, whose traditional ways of life depend on frozen ground for stability and seasonal predictability, are among those most affected.

The Arctic warms 

Permafrost is soil that remains frozen for at least two consecutive years. In many Arctic regions, it has remained frozen for tens or even hundreds of thousands of years. But since the early 2000s, feedback loops of shrinking sea ice, snow loss and warming soils have triggered faster Arctic warming. In the winter of 2024-25, the Arctic experienced record high temperatures as warming accelerated again and is now running seven times faster in the North Barents Sea than the rest of the world, researchers have found, as bne IntelliNews reported. 

This acceleration is already having measurable effects. The UN Environment Programme in 2019 listed permafrost thaw as one of the top 10 emerging environmental threats. In 2000-19, glaciers lost around 267bn tonnes of ice every year, according to a study published by Nature. On March 22, Arctic sea ice reached its lowest maximum extent since satellite records began 47 years ago. Beyond the Arctic, the Himalayas, the Alps and other high mountain ranges are seeing dramatic glacial retreat, with projections from the International Centre for Integrated Mountain Development (ICIMOD) showing at least one-third of Himalayan ice could vanish by 2100.

Russia’s Arctic regions are warming even more rapidly. Since 1970, northern Russia has seen temperatures rise by over 3°C – nearly triple the global average. In 2020, the Siberian town of Verkhoyansk registered 38°C, the highest temperature ever recorded in the Arctic. 

Even under moderate emissions scenarios, thawing will continue. According to Nordregio, the number of people living on permafrost could shrink from 4.94mn in 2017 to 1.7mn by 2050 – less because of mass migration, than because the land itself will no longer be frozen. The number of affected settlements could fall from 1,162 to 628 under a moderate emissions scenario.

Russia’s industrial north 

The problem is especially acute in Russia, which has the world’s largest population living on permafrost. Nearly two-thirds of Russian territory is underlain by frozen soil. “Russia and Canada are the two countries in the Arctic most affected by melting permafrost because large proportions of their territories are underlain by frozen soil. Nearly two-thirds of Russia is underlain by permafrost, while half of Canada is,” said Mia Bennett, associate professor at the University of Washington. 

“Canada has dozens of small settlements underlain by permafrost, but only Russia, as the most industrialised and urbanised country in the Arctic, has cities with hundreds of thousands of people, which have been constructed atop permafrost," Bennett told bne IntelliNews. Those cities are Norilsk, a city built up around an enormous nickel mine, and Yakutsk, the capital of the Sakha Republic. Other smaller cities like Vorkuta, whose population is nearly equivalent to that of all of Greenland, also sit on permafrost.” 

Yakutsk, the capital of the Sakha Republic – a vast, resource-rich region comprising a fifth of Russian territory – has continued to grow, fuelled by mining and buoyed by its role as a scientific and cultural hub. But the risks are rising. As permafrost thaws, the delicate balance that allowed these cities to flourish is beginning to unravel. Without drastic action to slow emissions and adapt infrastructure, the future of life on the thawing tundra looks increasingly uncertain.

Buildings crack, roads buckle 

The effects of thawing permafrost are already visible across the Russian Arctic. In Yakutsk, Norilsk and other cities built on what was once permanently frozen ground, cracks are appearing in buildings that have stood for decades, roads are buckling and sinkholes are opening up beneath once-stable infrastructure.

“As global temperatures rise, Arctic warming is affecting permafrost thaw and damaging infrastructure in Arctic cities,” Pavel Devyatkin, senior associate at The Arctic Institute, told bne IntelliNews by email. “In the Russian Arctic city of Norilsk, the subsidence of permafrost has caused buildings to sink or collapse.”

In response, authorities have allocated funds to artificially cool building foundations in Norilsk in an attempt to slow the melt and protect infrastructure. But such efforts are only a stopgap.

Aside from the damage to buildings, Norilsk, the largest Arctic city in Russia, has already suffered one of the region’s worst environmental disasters when thawing ground contributed to the 2020 spill of 20,000 tonnes of diesel fuel on the Taymyr peninsula. The accident, which turned the Ambarnaya river red, was compared by Greenpeace to the 1989 Exxon Valdez oil spill. Satellite footage showed the permafrost beneath the fuel tank had been subsiding, though metals major Norilsk Nickel was also accused of negligence by watchdog Rostekhnadzor.

Beyond the cities, the landscape is transforming. Lakes in permafrost regions are merging into each other, giant sinkholes are appearing, and land is being lost of the Arctic coastlines year after year. In Alaska, the ground beneath the runway at Nome airport, a vital regional link, has thawed, demanding costly repairs. In Norway’s Spitsbergen, hundreds of homes have been destroyed as the soil shifts beneath them.

“In all of these locations, hundreds of buildings built in previous decades, when temperatures were significantly colder and permafrost more reliably frozen, have been damaged and deformed by thawing permafrost. The slumping ground leads their foundations to crumble and crack,” said Bennett. “Many of these buildings have had to be abandoned. Infrastructure outside of cities is also threatened, from roads to runways and military bases.”

Infrastructure at risk 

By 2050, thawing permafrost could damage 20% of Russia’s commercial and industrial buildings, 19% of critical infrastructure valued at $84.4bn, and over half of residential properties worth $20.7bn. The cost of mitigation could range from 0.1% to more than 3% of Russia’s GDP, depending on climate outcomes.

One study using future climate scenarios projected that by mid-century, up to 44% of Arctic roads, 34% of railways, and 17% of buildings could be affected. Melting permafrost will damage 69% of the infrastructure in Russia’s frozen wastes by 2050, causing $275bn worth of damage and affecting the lives of over 3.6mn people, according to a study published in Nature.

Much of this infrastructure was designed with the assumption of stable ground – an assumption that no longer holds. This is a dangerous situation given that permafrost regions (especially in Russia) are not only home to oil and gas fields, but also nuclear power plants and hazardous waste sites. As permafrost loses its load-bearing capacity, the danger of structural failure grows.

Nearly 45% of Russia’s Arctic oil and gas fields lie in zones highly susceptible to thawing. Thousands of kilometres of key pipelines – including the ESPO oil line and future projects like Power of Siberia 2 – must traverse unstable terrain.

The Arctic also hides an industrial time bomb. Between 10,000 and 20,000 contaminated sites – abandoned bases, toxic sludge pits, mining waste – have relied on permafrost to contain their hazards, according to a paper published by the World Wildlife Fund (WWF). Thawing ground threatens to release these into surrounding ecosystems. In 2016, the Yamal Peninsula saw its first anthrax outbreak in 75 years, triggered by thawed reindeer carcasses. Over 2,000 reindeer died and dozens of human infections followed.

Transport disrupted 

“We are getting collapses of building and bridges, problems with roads and railways. It’s a huge problem, costing millions of dollars, especially if you look at northwest Siberia, where there are already a lot of infrastructure problems. Thawing ice-rich soils in the far north threaten buildings, runways and infrastructure, causing ground shifts and major disruptions for residents,” said Brown University professor Amanda Lynch, in an interview with bne IntelliNews

She warned that travel is becoming more difficult. Communities that rely on frozen rivers and lakes for winter transport find them increasingly unreliable. The ‘transition zone’ between frozen and unfrozen ground is expanding and moving north. 

"At the moment it’s much easier to build an ice road and transport things in winter than to maintain roads and railways over discontinuous permafrost,” she said. 

The most unstable zones are those that freeze and thaw each year, warping roads and buckling rail lines. “It’s very expensive to maintain land based transport infrastructure in that transition zone,” said Lynch. 

“If you go to 2100 everything is thawed and it’s a much simpler problem. But from getting from here to there is very messy.” 

In the meantime, many small settlements may become inaccessible – or at least it will become prohibitively expensive to maintain road connections, although those on navigable rivers will be easier to access. 

Within the next 25 years, an estimated 3.3mn residents risk losing their homes as thawing permafrost undermines the ground beneath them. Across the region, roads, pipelines and buildings that serve more than 4mn people are being damaged. Indigenous communities, in particular, face the erosion not only of their homes but of traditions that have been shaped by the frozen ground for centuries.

In Russia, those displaced are often relocated to cities. There have also been relocations in Alaska and Canada. In Alaska, the village of Newtok has been eroding so rapidly that residents have begun a managed retreat to Mertarvik – making them one of the first Indigenous communities to complete a climate-forced relocation.

Yet relocation is a costly and deeply fraught solution, according to Lynch. “Governments and companies may think in terms of financial costs, but for Indigenous and traditional communities, there are values other than money to take into account,” she said. 

Boomtowns 

By contrast, some Arctic towns are booming as warming temperatures and technological advances open access to oil, gas and mineral reserves. Russia’s Arctic zone alone is believed to hold huge amounts of natural gas, oil, gold, silver and rare earths, making these territories critical to its economy. Gas companies Novatek and TotalEnergies are already operating (liquefied natural gas) LNG megaproject on the Yamal peninsula. In May this year, Russian oil company Rosneft took over Vostok Engineering LLC, which holds the license for Tomtor, one of the world's three biggest rare earth metal deposits, in Yakutia.

Economic activity in the Arctic has accelerated sharply. Until recently, most oil and gas extraction in the region took place onshore. Now, as summer sea ice declines – potentially vanishing entirely by 2035 – the Arctic is opening up to offshore development and expanded shipping. The US Geological Survey (USGS) estimates that 30% of the world’s undiscovered gas and 13% of undiscovered oil lie north of the Arctic Circle. The US Congressional Research Service puts the value of the region’s mineral wealth at around $1 trillion.

Infrastructure is following. In Alaska, work is under way to develop a new deepwater port at Nome, while Russia is investing into its ports at Murmansk, Arkhangelsk and Sabetta. 

"In order to efficiently use the Trans-Arctic shipping route's potential and turn it into one of the main transport lanes in the country, it is important to ensure the development of port infrastructure along its entire length,” said Kremlin aide and Maritime Board chairman Nikolai Patrushev in April, as reported by Interfax.

Lynch noted that Russia is “massively” expanding its Arctic infrastructure. “Russia is leaning in, they see climate change as a net benefit. They are looking at a certain future of warm water deepwater ports.” 

Between 2013 and 2024, the number of unique ships entering the Arctic Polar Code area shot up by 37%, according to the Protection of the Arctic Marine Environment Working Group of the Arctic Council. This included a variety of traffic including tourist vessels through the Northwest Passage, cargo movements through the ‘GIN’ corridor (Greenland, Iceland, Norway), and traffic along Russia’s Northern Sea Route. 

Russia shifts to the East

Since the outbreak of war in Ukraine, Arctic shipping has increased further. “The volume of trade has increased. The war in Ukraine accelerated it because a lot of the shipping up there was always Russian. They operated year round, with a massive ice-breaker fleet,” said Lynch. “With sanctions, the trade relationship with China has become very important.” That has hiked demand on routes such as Subeta to Shanghai. 

As Arctic activity intensifies, so too does the need to manage the risks posed by thawing permafrost. Engineering solutions are emerging to stabilise foundations and protect infrastructure. 

“There are several engineering options for adapting to melting permafrost, including geotextiles, embankments, and other solutions that help to lower the temperatures and insulate the ground to prevent further melting,” says Bennett. “Some of these solutions are being developed outside of the Arctic in places like China, where 40% of the Tibetan Plateau is underlain by permafrost.” 

According Devyatkin, these innovations include reinforced buildings, thick foam pads beneath roads, and expanded monitoring networks. "Governments are developing policies and regulations to work with construction on permafrost, such as mandates on permafrost-specific surveys and assessments before construction begins. There is a political will to address issue and this issue is especially getting more attention in regional and subnational governments.” 

Russia is expected to unveil a strategy later this year to secure its Arctic infrastructure. But despite new engineering and regulatory approaches, experts warn that technical fixes are only part of the solution. The most effective way to mitigate permafrost damage is by curbing global warming.

There is also a dangerous feedback loop at play: as permafrost melts, it releases greenhouse gases – not just carbon dioxide but the much more damaging methane – accelerating global warming. The Intergovernmental Panel on Climate Change (IPCC) has warned that hundreds of gigatonnes of carbon dioxide could be released into the atmosphere as earth that has been frozen for hundreds of thousands of years thaws.

This article is part of a series on the impact of the Climate Crisis on major cities around the world. 

The other articles in the series are: 

Cities confront the rising tide of climate change

Taipei’s climate countdown

Accra under water

Jakarta’s sinking villages

Droughts and heatwaves grip Tehran

Two decades of change are testing Tokyo’s resilience

Rising seas threaten India’s coastal cities

Adapting the concrete heart of São Paulo to a changing climate

Mexico's Acapulco still rebuilding as climate disasters mount

Tuesday, November 10, 2020

Loss of permafrost - a global cause for concern
 
Permafrost is present above 2,500 metres. Melting permafrost was the cause of a landslide on the Matterhorn (pictured), at Zermatt in southern Switzerland, in summer 2003.
 Keystone / Alessandro Della Bella

Switzerland is a pioneering country in the study of permafrost. The thawing of terrain that used to be permanently frozen is becoming more and more prevalent, and it has planet-wide repercussions. 

 This content was published on November 10, 2020

The locals call it "Hell’s Gate" because of the noises that seem to come from the bowels of the earth. For scientists, the Batagaika crater, in Eastern Siberia, has nothing very diabolical about it. The sounds it makes are the result of a geophysical phenomenon that has been known for quite some time: the melting of permafrost, the layer of permanently frozen ground.
 
The Batagaika crater in northeast Russia is 1.5km wide and up to 100 metres deep. It is the largest crater in the world and was caused by the thawing of permafrost. ©yuri Kozyrev / Noor

This change, driven by global warming, is happening not just on the Siberian tundra, but throughout a northern hemisphere area of about 23 million square km, or twice the size of the US. Found mainly in the Arctic regions, from Russia to Canada, permafrost is also present in the high mountain terrain right across the Alps. In Switzerland, it is found above an altitude of 2,500 metres.

As well as causing major disturbances to the terrain itself, thawing of permafrost can undermine the stability of mountain slopes and trigger natural disasters. These developments are a worry to people living in the affected regions, but the potential repercussions around the world are also a major cause of concern. According to a 2019 report by the United Nations, the loss of permafrost is one of five major threats to the environment that have hitherto been underestimated.

Permafrost warms up


Some 5% of Switzerland’s national territory is made up of permafrost, mostly in terrain covered by rock debris and on cliff walls at high altitudes. In comparison, the proportion covered by glaciers is about 2.5%.

"It is clear that in the past twenty years, the temperature of permafrost has been rising throughout the Swiss Alps", says Jeannette Noetzli of the Institute for Snow and Avalanche Research.

It’s not just the temperature of the surrounding air that determines the condition of the permafrost, she points out. The sun’s rays and the snow cover have to be taken into account as well.

Unlike peaks above the 4,000-metre level and the polar regions, where permafrost is really cold, in Alpine regions most of its temperature is close to zero, Noetzli explains. "So we have less of a thermic 'reserve' and we are that much closer to melting point."

What is known as the “active layer” is getting thicker. This is the top level of the permafrost which melts during the summer and freezes again in the winter.
External Content

Sensors and cameras on the Matterhorn

Jeannette Noetzli heads PERMOS, the permafrost monitoring network in Switzerland. Created in 2000, it is the first national network dedicated to studying change in permafrost. Switzerland has the world’s largest collection of data on high-altitude permafrost, and it includes a chronological series covering a period of over 30 years.

Researchers are able to make use of advanced technologies: probes that go down a hundred metres, devices to measure the terrain’s electrical resistance, GPS, wireless sensors and high-resolution video cameras. On the Hörnli ridge of the Matterhorn, 3,500 metres up, a network of 17 sensors is transmitting data in real time to the computing centre at the Federal Institute of Technology in Zurich (this is the PermaSense project).
 
Replacement of a temperature-measuring device above the Corvatsch-Murtèl glacier in canton Graubünden in southeast Switzerland. Jeannette Noetzli, PERMOS

Risk of landslides


The unfreezing of the permafrost has a negative impact on the stability of mountainsides, because it takes away their “stickiness”, as Cécile Pellet of the geosciences department at the University of Fribourg explains.

"Losing the permafrost can lead to rockslides", she told the Valais newspaper Le Nouvelliste. However, as the PERMOS researcher points out, there can be more than one reason when this kind of event happens, as was the case in Bondo in 2017. The geology of the place itself may be a contributing factor.

It would be too much of a generalisation to say that the Alps are going to become a more dangerous place due to global warming and the melting of permafrost, thinks Noetzli. "But we are noticing major changes in sensitive areas. As a result, mountain climbers may have to look for different routes to take in some places".

Danger for tourist infrastructure


One thing is certain, however: the decline of the permafrost and the increasing movement seen in rock debris has the potential to be a problem for buildings and structures of all kinds sited at a high altitude: chalets for mountain-climbers, cableways, railways, telecommunications equipment, avalanche barriers, and so on.

All this infrastructure is important for tourism, communication, power supply, and prevention of natural hazards in Switzerland. For example, the Gornergrat railway near the Matterhorn and the Jungfrau railway in the Bernese Alps were built partly over permafrost.

Cable-car operators will need to invest in new construction to strengthen the pillars supporting their infrastructure. In canton Uri, for exmaple, a new concrete base has had to be put in for the Gemsstock cable car line, which goes up to an altitude of almost 3,000 metres.
Worrying global trends

The repercussions of the thawing of permafrost will be seen not just at local or regional level.

As the permafrost melts, ancient microorganisms trapped inside the ice could get out into the atmosphere and become reactivated, infecting humans and animals. To learn more, see our article on this topic featuring Swiss expert Beat Frey, who is a researcher at the Snow and Avalanche Institute studying Alpine permafrost. He calls this issue "a major unknown".

Furthermore, organic carbon which has accumulated over the course of millennia in the ice layer will increasingly find itself being released into the atmosphere in the form of CO2 and methane, which is likely to add to global warming – a vicious circle.

This issue concerns above all the Arctic regions, where rising temperatures (two to four times the global average) are bringing the collapse of the permafrost that much closer, experts warn. According to the estimates, frozen terrain holds about 1,600 billion metric tons of carbon – double what is in the atmosphere.

Tuesday, May 18, 2021

More than 60% of Russian territory is permafrost. Now it is melting

Climate change is about to dramatically change the Russian North. The country is now starting the building of a new permafrost monitoring system.
Melting permafrost in the Yamal-Nenets region. Photo: Yanao.ru


Read in Russian | Читать по-русски
By
Atle Staalesen

May 14, 2021

Russian authorities have made the Arctic a top priority and big sums are invested in new regional industry and infrastructure.

But the melting of the permafrost could potentially stagger plans. Across the country’s north, buildings, roads and industrial installations are slowly sliding into the ground.

Decision makers in Moscow now increasingly see the permafrost melting as an issue of concern, and measures are taken to step up mapping.

According to Minister of Natural Resources Aleksandr Kozlov, a state monitoring system for the permafrost will be established, and this system will be anchored in federal legislation.

“65 percent of Russia’s territory is located in the permafrost zone, but this is not mentioned in a single federal program document, despite the fact that the permafrost area is a vital component in the natural environment, of which the landscape, vegetation and coastline is dependent,” Kozlov says in a statement.

The melting already has major consequences for people living in the region, he explains.

“We see how the melting of the permafrost is triggering accidents at industrial and housing objects, therefore it is obvious that the state needs a system for monitoring and early-warning of negative consequences of the degradation of the permafrost,” he underlines.


“We have to protect the nature from environmental catastophe,” he says.

The new monitoring system will be based on existing research installations managed by state meteorological authority Roshydromet, and two development phases are envisaged.

The first pilot phase will cover the period 2022-2024 and be based on experiences and methodology applied in Spitsbergen, Franz Josef Land and Severnaya Zemlya, the Ministry of Natural Resources informs.

In addition to the federal monitoring system come several regional initiatives. In the Yamal-Nenets region, a laboratory for permafrost studies will this year be opened.

The lab is developed on an initiative from governor Dmitry Artyukhov, the regional government informs. It is believed to be the first of its kind in Russia.

“Climate change and the melting of the permafrost is a huge challenge not only to Yamal, but to the whole of Russia,” Artyukhov says.

Wednesday, March 16, 2022

First-of-its-kind research reveals rapid changes to the Arctic seafloor as submerged permafrost thaws

First-of-its-kind research reveals rapid changes to the Arctic seafloor as submerged permafrost thaws
MBARI’s autonomous underwater vehicle (AUV) is recovered after completing a successful
 seafloor mapping mission in the Arctic Ocean. The remotely operated vehicle (ROV, 
foreground) is used to conduct visual surveys of the newly mapped seafloor. 
Credit: Charlie Paull © 2016 MBARI

A new study from MBARI researchers and their collaborators is the first to document how the thawing of permafrost, submerged underwater at the edge of the Arctic Ocean, is affecting the seafloor. The study was published in the Proceedings of the National Academy of Sciences on March 14, 2022.

Numerous peer-reviewed studies show that thawing permafrost creates unstable land which negatively impacts important Arctic infrastructure, such as roads, train tracks, buildings, and airports. This infrastructure is expensive to repair, and the impacts and costs are expected to continue increasing.

Using advanced underwater mapping technology, MBARI researchers and their collaborators revealed that dramatic changes are happening to the  as a result of thawing permafrost. In some areas, deep sinkholes have formed, some larger than a city block of six-story buildings. In other areas, ice-filled hills called pingos have risen from the seafloor.

"We know that big changes are happening across the Arctic landscape, but this is the first time we've been able to deploy technology to see that changes are happening offshore too," said Charlie Paull, a geologist at MBARI and one of the lead authors of the study. "This groundbreaking research has revealed how the thawing of submarine permafrost can be detected, and then monitored once baselines are established."

While the degradation of terrestrial Arctic permafrost is attributed in part to increases in mean annual temperature from human-driven climate change, the changes the research team has documented on the seafloor associated with submarine permafrost derive from much older, slower climatic shifts related to our emergence from the last ice age. Similar changes appear to have been happening along the seaward edge of the former permafrost for thousands of years.

"There isn't a lot of long-term data for the seafloor temperature in this region, but the data we do have aren't showing a warming trend. The changes to seafloor terrain are instead being driven by heat carried in slowly moving groundwater systems," explained Paull.

First-of-its-kind research reveals rapid changes to the Arctic seafloor as submerged permafrost thaws
Repeated mapping surveys with MBARI’s autonomous underwater vehicles (AUVs) 
revealed a massive sinkhole developed over just nine years.
 Credit: Eve Lundsten © 2022 MBARI

"This research was made possible through international collaboration over the past decade that has provided access to modern marine research platforms such as MBARI's autonomous robotic technology and icebreakers operated by the Canadian Coast Guard and the Korean Polar Research Institute," said Scott Dallimore, a research scientist with the Geological Survey of Canada, Natural Resources Canada, who led the study with Paull. "The Government of Canada and the Inuvialuit people who live on the coast of the Beaufort Sea highly value this research as the complex processes described have implications for the assessment of geohazards, creation of unique marine habitat, and our understanding of biogeochemical processes."

Background

The Canadian Beaufort Sea, a remote area of the Arctic, has only recently become accessible to scientists as  drives the retreat of sea ice.

Since 2003, MBARI has been part of an  to study the seafloor of the Canadian Beaufort Sea with the Geological Survey of Canada, the Department of Fisheries and Oceans Canada, and since 2013, with the Korean Polar Research Institute.

MBARI used autonomous underwater vehicles (AUVs) and ship-based sonar to map the bathymetry of the seafloor down to a resolution of a one-meter square grid, or roughly the size of a dinner table.

Paull and the team of researchers will return to the Arctic this summer aboard the R/V Araon, a Korean icebreaker. This trip with MBARI's long-time Canadian and Korean collaborators—along with the addition of the United States Naval Research Laboratory—will help refine our understanding of the decay of submarine .

Two of MBARI's AUVs will map the seafloor in remarkable detail and MBARI's MiniROV—a portable remotely operated vehicle—will enable further exploration and sampling to complement the mapping surveys.Researchers discover mysterious holes in the seafloor off Central California

More information: Rapid seafloor changes associated with the degradation of Arctic submarine permafrost, Proceedings of the National Academy of Sciences (2022). DOI: 10.1073/pnas.2119105119

Journal information: Proceedings of the National Academy of Sciences 

Provided by Monterey Bay Aquarium Research Institute 

Melting Permafrost Is Creating Giant Craters And Hills On The Arctic Seafloor


By Stephen Luntz

15 MAR 2022, 08:36


Submarine surveys of the seafloor beneath the Arctic Ocean have revealed deep craters appearing off the Canadian coastline. The scientists involved attribute these to gasses released as permafrost melts. The causes, so far, lie long before humans started messing with the planet’s thermostat, but that could be about to change.

For millions of years, soil has been frozen solid over large areas of the planet, both on land and under the ocean, even where snow melts at the surface to leave no permanent ice sheet. Known as permafrost, this frozen layer traps billions of tonnes of carbon dioxide and methane. It is thought the sudden melting of similar areas around 55 million years ago set off the Palaeocene-Eocene Thermal Maximum, when temperatures rose sharply over the space of a few thousand years.

Now the permafrost is melting again, revealed in plumes of bubbles coming to the surface in shallow oceans, the collapsing of Arctic roadsruined scientific equipment, and great craters that suddenly appeared in Siberia. For the first time, scientists have revealed in Proceedings of the National Academy of Sciences what all this is doing to part of the Arctic Ocean’s seafloor.

Dr Charles Paull of Monterey Bay Aquarium Research Institute and co-authors ran four surveys of the storied Beaufort Sea between 2010 and 2019 using autonomous underwater vehicles assisted by icebreakers at the surface. They restricted their observations to depths between 120 and 150 meters (400-500 feet) as in most places this captures the permafrost's outer margin.

The paper reports numerous steep-sided depressions up to 28 meters (92 feet), along with ice-filled hills up to 100 meters (330 feet) wide known as pingos. Some of these, including a deep depression 225 meters (738 feet) long and 95 meters (312 feet) across, appeared between successive surveys, rather than being long-standing features. Others expanded in the time the team were watching.

The depressions are the result of groundwater ascending up the continental slope. Sometimes the groundwater freezes from contact with colder material, causing the ground surface to heave upwards and produce pingos.

“We know that big changes are happening across the Arctic landscape, but this is the first time we’ve been able to deploy technology to see that changes are happening offshore too,” Paull said in a statement. “This groundbreaking research has revealed how the thawing of submarine permafrost can be detected, and then monitored once baselines are established.”

The research was possible because the Beaufort Sea, once too icebound for research like this, is melting fast. That trend is, the authors agree, a consequence of human emissions of Greenhouse gases. The same goes for the widespread disappearance of permafrost on land.

However, the extra heat those gasses put into the global system has yet to penetrate to the depths Paull and co-authors were studying. Here, temperatures operate on a much slower cycle, buffered by so much water, and are still responding to the warming that took place as the last glacial era ended. At the current rate, it would take more than a thousand years to produce the topography the team observed.

“There isn’t a lot of long-term data for the seafloor temperature in this region, but the data we do have aren’t showing a warming trend,” Paull said. “The changes to seafloor terrain are instead being driven by heat carried in slowly moving groundwater systems.”

The natural melting of Ice Age permafrost releases gasses that warm the planet, part of a reinforcing interglacial era cycle, but the effect is slow enough to present little problem for humans or other species. As human-induced atmospheric heat permeates the oceans at these levels things could accelerate dramatically, and the authors see their work as establishing a baseline so we know if that occurs.


Giant, 90ft Deep Craters Are Appearing on the Arctic Seafloor

ON 3/14/22 

Enormous craters measuring 90 feet in depth have appeared on the seafloor of the Arctic Ocean.

The craters, scientists say, are forming as a result of thawing submerged permafrost on the edge of the Beaufort Sea in northern Canada, with retreating glaciers from the last ice age driving the change and not recent climate warming.

Permafrost is ground that is permanently frozen—in some cases for hundreds of thousands of years. In the Arctic, which is warming faster than any other region of Earth, permafrost is thawing, causing the ground to become unstable.

As the soil thaws, organic matter trapped within starts to break down, causing the release of methane and other greenhouse gasses. As these gasses are released, pressure builds.

On land, the impact is clear. In Siberia, there is footage showing the land wobbling "like jelly" beneath people's feet.

Eventually, when the pressure reaches a tipping point, the land explodes, leaving massive craters behind. One person who witnessed this happening described it as being "as if the earth was breathing."


What happens when permafrost on the bottom of the sea thaws is less clear, however.

In 2019, scientists in Siberia discovered a patch of ocean where the sea was "boiling" with methane, with concentrations of the gas around seven times higher than the global average.

Two years earlier, a different team of researchers found evidence of huge craters—some over 3,000 feet wide—on the floor of the Barents Sea, north of Norway and Russia. They said these craters had formed as a result of methane explosions that took place thousands of years earlier
.
To better understand what impact thawing permafrost is having beneath the ocean, researchers led by Charles K. Paull, a senior scientist at California's Monterey Bay Aquarium Research Institute, used advanced mapping technology to observe changes to the seafloor over the course of a decade.

They conducted surveys in the Beaufort Sea between 2010 and 2019 to map topographical changes resulting from thawing permafrost.

Findings showed that at depths between around 400 and 500 feet, huge depressions with steep sides were forming. The largest was 90 feet deep. Their findings are published in scientific journal PNAS.

Paull told Newsweek they were shocked at their findings, with the craters far larger than they had anticipated.

He said the team does not believe the craters formed in explosive events: "The evidence suggests that the submarine features we observed forming are essentially sink-holes and retreating scarps, collapsing into void space left behind by the thawing of ice-rich permafrost."

Unlike terrestrial permafrost, climate change is not driving the seafloor to thaw. Instead, the shift is the result of older climatic shifts relating to the end of the last ice age, around 11,700 years ago. Heat is being carried to the permafrost via slow-moving groundwater systems.

The team plans to return to the Arctic this summer to look more closely at the decaying seafloor permafrost.

Julian Murton, Professor of Permafrost Science at the U.K.'s University of Sussex, who was not involved in the study, told Newsweek he was surprised at how quickly the seafloor topography had changed.

"Some changes are as rapid or even more rapid than the better-known landsurface topographic changes driven by thaw of ice-rich permafrost in the Arctic," he said. "I had assumed that thermal inertia associated with thick relict permafrost and with overlying seawater led to slow changes in seafloor topography.

"Clearly this assumption is shown to be wrong, at least locally, by this fascinating, high-resolution study."

Paull said the longer term consequences of seafloor permafrost thaw is unclear: "Since some methane is trapped in permafrost, thawing permafrost inevitably releases methane, an important greenhouse gas," he said.

"However, we don't have data to understand whether the rate of methane release from decaying submarine permafrost has changed in recent times in this area.

"The changes we've documented derive from much older, slower climatic shifts related to Earth's emergence from the last ice age, and appear to have been happening along the edge of the permafrost for thousands of years. Whether anthropogenic climate change will accelerate the process remains unknown."

Researchers observed huge sinkholes appearing on the ocean floor over a nine-year survey