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You might think polar bears – and the potential for attack – are the biggest danger the Norwegian island archipelago of Svalbard. But avalanches kill far more people on Svalbard than polar bears ever have.
This story is written by guest contributor Nancy Bazilchuk of NTNU
Looking at how much precipitation fell in Longyearbyen just before the deadly avalanche of Dec. 19, 2015, such a destructive avalanche might not seem possible to many people, said Alexander Prokop, an avalanche researcher at The University Centre in Svalbard.
“They measured 18 millimeters of precipitation at the airport,” Prokop said from his office in Longyearbyen. “But the fracture, the crown height of the avalanche where it broke away from the snow, was up to four meters high.”
Since the tragedy that destroyed 11 homes and killed two people more than a year ago, Norwegian authorities have taken a series of measures to protect Longyearbyen residents in their Arctic homes. They’ve created a new risk assessment map for the town and instituted an avalanche warning system, currently operated by the Norwegian Water Resources and Energy Directorate. The Norwegian Water Resources and Energy Directorate has also published a case study of Longyearbyen that presented possible methods for protecting buildings and other structures from avalanches and damage from permafrost.
But the climate and risk situation in Longyearbyen, the largest town in the island archipelago, is undergoing enormous change because of global warming. At the same time, there is relatively little long-term information about the frequency of weather conditions that increase avalanche and landslide risks, Prokop said.
“The problem here in Svalbard is that they don’t have measurements that are suited to investigating (these kinds of) hazards. They just have precipitation measurements at the airport, which you can’t really use for snow data,” he said.
Prokop and Arne Aalberg, a researcher at The Norwegian University of Science and Technology, plan to change that. Prokop is working to install a network of snowfall measuring instruments around the town. This information is vital to improve avalanche forecasting. At the same time, he and his students have taken detailed measurements after the deadly 2015 avalanche, which are being used to fine-tune a computer model that will also help improve forecasting.
Aalberg, who is now leader of the Arctic Technology group at UNIS in addition to his NTNU affiliation, is focused on snow pressures and forces on buildings or other manmade structures. One of his master’s students is investigating the best way to measure these forces in the hills around Longyearbyen. This information could help with the design of avalanche fences or other kinds of structures to protect existing houses or buildings, Aalberg says.
Arctic, alpine snowpacks differ
Prokop, an Austrian who is also an avid skier, has first-hand knowledge of how communities in the Alps protect their villages from the ravages of avalanches. His latest academic publication, from September last year, is all about a new methodology for planning snow drift fences in alpine terrain.
But while there has been a lot of focus by researchers on avalanche dangers and mitigation in the Alps, much less is known about arctic conditions. And these conditions are quite different.
For one thing, Arctic areas like Svalbard are underlain by permafrost, or permanently frozen ground. That matters because the difference in temperature between the top of the snowpack and the bottom, near the ground, is important in helping create conditions that can trigger an avalanche.
Snow scientists like Prokop call this temperature difference a gradient. If the gradient is big, with a large temperature difference between the top of the snowpack and the bottom, the snowpack is more likely to be unstable.
This is because the big temperature differences allow snow crystals to grow. Big crystals that are poorly bonded to the rest of the snow create a weak layer in the snowpack. A weak layer is exactly what it sounds like: a layer in the snowpack where there is a weak or slippery surface or layer that allows the snow on top to slide off.
Weak layers are very common in Arctic snow packs, in part because the snowpack is often very shallow. A shallow snowpack can make for a bigger temperature gradient. The changing climate has also made weak layers far more prevalent, because climate change has made it more likely that there are crazy temperature changes. It can be bitter cold in Svalbard on one day, but then rain the next, Prokop says. If a rain crust forms on the snow surface, this provides a slippery surface for new snow that might accumulate on top in subsequent snowstorms.
Knowing where the snow accumulates – and how much
It wasn’t a shallow snowpack that caused tonnes of snow to roar into Longyearbyen on Dec. 19, 2015, however. Instead, high winds swept mountaintops clean, and deposited all this collected snow into protected areas, like the hillside called Lia, which is where the avalanche happened.
That’s because wind-drifted snow is another key factor in determining what will cause an avalanche, Prokop says. “The actual amount of snowfall is not that important in Svalbard, but due to heavy winds and a lot of fetch area, a lot of snow can be drifted into an avalanche release area,” he said. “That was the problem with this avalanche.”
Installing snow depth measuring instruments around Longyearbyen will allow Prokop and others to know not only how much snow falls, but also how much snow has been redeposited by the wind. Across the world, avalanche experts consider a daily new snow depth of 30 centimeters – whether wind deposited or freshly fallen – to be a critical amount that can increase avalanche risk.
“That is a key amount where you have to take action,” he said.
Building a predictive model
Another way to improve the ability to predict avalanches is by creating a computer model, where you enter different snow conditions for different locations and see what the model predicts.
Prokop and his students took action right after the deadly 2015 avalanche to collect vital information to build exactly this kind of predictive model.
“What we did was try to document the event, what actually happened,” he said.
“What did the snowpack look like? How much snow had drifted in? What about the wind? We had pictures and laser scanning, and we created a high-resolution snow surface model so we can actually know how much snow was released” during the avalanche.
The proximity of the avalanche slope to the town, and the fact that people took pictures of the slope as the wind piled up snow on the slope and around buildings also helped provide very useful information, Prokop said.
“This is very important and is often missing, because you don’t see where the avalanche was released or no one can go up there,” he said. “Here in Longyearbyen, it is easy to go there, and we have pictures prior to the avalanche.”
Prokop has a master’s student who is working with information from other avalanches that occurred around Longyearbyen to fine-tune the model. Then, he says, you can just change the snow height and see how far the avalanche would travel, or how much snow it might deposit.
Snow loads and protective fences
While Prokop is studying avalanches, Aalberg, as a building engineer, is interested in understanding what kinds of forces the snow exerts before it slides away in an avalanche. This kind of information is important if the town were to decide to build some kind of protective structure to prevent avalanches from happening.
Elsewhere in Norway and in other avalanche-prone areas, for example, towns erect a series of snow fences on slopes where enough snow might build up and tumble down as an avalanche.
There are at least two types of fences, Aalberg says. The first kind are composed of open fences (which are essentially wind screens, half of the area of which is open). These structures slow the wind which causes the snow to be deposited on the leeward side of the fence.
“It’s a kind of engineered re-location of snow accumulation,” Aalberg said. “It piles up in suitable, ‘safe’ areas, instead of on the road or on a railway or whatever you are trying to protect.” The challenge with this kind of snow fence is that it requires a fairly large area for the snow to accumulate, he says.
The second kind of protection that can be built includes fences, walls, or soil dams that are placed in series along the slope. These structures do not necessarily prevent snow accumulation, but help anchor the snow so it can’t begin sliding and cause an avalanche. Snow will still accumulate, but is “anchored” safely if the fences are well anchored in the ground.
However, “if you are going to take any safety actions, you need to know how much force a structure will experience,” Aalberg said. Although there has been a fair amount of research on these kinds of forces on mainland Norway, Svalbard experiences far different conditions than on the mainland, he said.
“No one can guarantee that the design manuals from the mainland will work,” Aalberg said. “But if you are thinking about building something that will hold the snow back, you have to know how the snow behaves.”
Aalberg hopes to collect data over several years using a pressure plate measuring system that has been developed as part of one of his master’s student’s research. Then, he said, if the town decides to build some kind of protective structures, engineers will have the information they need.
Whether the town will choose to build snow fences or other protective structures remains an open question, however.
“Svalbard is a place where there are so many historic structures,” which are protected by Norwegian law, he said. Then there’s the actual physical effect of building big fences on the mountainsides around the town.
“It would be ugly,” he said. “It would be a bit of an attack on the environment. It would take 50 years for the vegetation (that would have to be disturbed to build the structures) to come back.”
More dangerous than polar bears
While the Norwegian Water Resources and Energy Directorate has now started providing avalanche forecasts for Svalbard, Prokop says he wants to create a sustainable avalanche safety system that is based on the island archipelago itself.
“We want to help the town to know when it is dangerous and when it is not, and how to behave,” Prokop said. Such an automated system also needs to be independent of local, knowledgeable individuals, he said, even though local knowledge is very important.
“People stay in Svalbard an average four years and then they leave,” he said. “The problem is that then the knowledge also leaves.”
As one example of this, Prokop pointed out that there had been a hazard map created for the Longyearbyen area in 1992, which showed that Lia, the area where the avalanche occurred, was at risk. All in all, the tragedy was an important, if distressing reminder, of the power of the environment.
“It might be interesting for people to know that in the last 15 years, seven people died from avalanches,” he said. “But in the last 35 years, only three people have died from polar bear attacks. It is more likely that you will die from an avalanche in Svalbard than from a polar bear. ”
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This article first appeared in NTNU’s and Sintef’s science publication Gemini Research News.
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Reference: Alexander Prokop, Emily S. Procter, “A new methodology for planning snow drift fences in alpine terrain,” Cold Regions Science and Technology, Volume 132, December 2016, Pages 33-43, ISSN 0165-232X.
