Whispering Glaciers — log
Hello world! This is Whispering Glaciers’ development log.
We will be sharing updates on our ongoing research, including insights about Svalbard, the planning of our field trip, artistic and design inspirations, the various testing phases of the project, personal reflections, and, of course, a detailed diary documenting our 10-day expedition in the Svalbard archipelago.
The Whispering Glaciers project takes inspiration from recent observations on the transformations taking place in Svalbard’s ecosystems. Studies suggest that Svalbard is warming four times faster than the global average and is experiencing a severe fast-ice decline. (Rantanen, M., Karpechko, A.Y., Lipponen, A. et al.) This change in weather not only affects the landscape but the ecosystem and the world as a whole.
In the coming years, Svalbard may undergo radical transformations. Sounds, shapes, textures, ecosystem dynamics, and other less visible phenomena could shift into something else. As a consequence, in recent years many have rushed to the archipelago, eager to experience its unique ecosystem before it changes forever.
Whispering Glaciers seeks to create an immersive experience that allows participants to explore the landscapes of the archipelago. This experience will attempt to bring them into close contact with the intricate shapes, textures, colours, ambient tones, and subtle, often inaudible sounds that define this fragile environment. Whispering Glaciers will look into balancing realistic visual representations with more abstract interpretations, challenging conventional perspectives shaped by wildlife films and cinematic portrayals of Svalbard.
Svalbard, Norway, MODIS Land Rapid Response Team, June 7, 2001
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Svalbard is a critical region for studying climate change due to its vast and diverse ice areas. These include glaciers, sea ice, permafrost, and icebergs, each playing a vital role in the global climate system. The total area of the islands is 62,248 km2, and, and, about 59 percent of which is covered by over 2,100 glaciers. Key types include tidewater glaciers, like Kongsbreen, which calve icebergs into fjords; valley glaciers, such as Longyearbreen; and large ice caps, like Austfonna. These polythermal glaciers contain both cold and temperate ice, influencing their dynamics and response to warming.
Sea ice around Svalbard varies seasonally, peaking in winter and retreating in summer. The extent of sea ice has declined in recent decades, impacting ecosystems and serving as a critical climate indicator. It provides a habitat for species like polar bears and Arctic cod, which are under threat as ice diminishes.
Permafrost, which underlies much of Svalbard, is thawing due to rising temperatures. This leads to infrastructure instability, carbon release, and hydrological changes. The ground ice within permafrost plays a key role in maintaining landscape stability.
Icebergs, originating from calving glaciers, are significant for marine ecosystems as they release nutrients while melting. However, they pose challenges for navigation and provide clues about environmental conditions through their shapes and melt rates.
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Kongsbreen glacier
Austfonna glacier (satelite view)
Austfonna glacier
Scheelebreen glacier, 2023
Borebreen glacier, August 2024
We recently came across the work of Dr. Richard Hann, a senior researcher at the Norwegian University of Science and Technology (NTNU), who specializes in icing on unmanned aerial vehicles. Dr. Hann has conducted extensive research on glaciers in Svalbard—such as Tunabreen, Borebreen, Vallåkrabreen, and Wahlenbergbreen—collecting aerial imagery and publishing photos on Kuula, along with 3D glacier models on Sketchfab.
His work is a great contribution to our field trip preparations, helping us in simulating various scenarios for our VR experience. We have begun importing some of his 3D models into Unreal to evaluate rendering quality and performance. These tests will provide deeper insights into the techniques and considerations for capturing glacier and ice imagery, both aerially via drones and from the ground.
To capture unique perspectives and access otherwise unreachable areas of the glaciers, we will be using two drones alongside ground cameras. The first step was selecting the best drones for the task. Since much of our glacier exploration will take place from a boat, one risk quickly became apparent—the possibility of a drone crashing into the water.
We were advised that if a drone went down, we would need to retrieve it from the freezing depths of the sea. This concern played a major role in our decision-making, leading us to choose the SwellPro Splash Drone 4—a waterproof drone capable of landing on water without issue. To complement it, we also acquired the DJI Mavic Pro 3 for its superior image quality. To mitigate the risk of losing it, we equipped it with a foam float system to prevent it from sinking in case of an accident.
French Alps, Aerial view, February 2025
Flying a drone is more complex than it seems. Before I could even start experimenting with it, I had to complete basic training and theoretical courses on drone regulations, pass a test, and ensure I was properly registered. Since I’m flying a drone in the UK, I had to register with the Drone & Model Aircraft Registration Service UK and obtain UK insurance. Additionally, because we’re operating drones in Svalbard, we also had to secure European insurance coverage.
Once all the paperwork was sorted, I finally got my hands on the DJI Mavic Pro 3 and made my first-ever drone takeoff in the French Alps. Over several days, I familiarized myself with the fundamental controls needed to fly safely. I practised takeoffs and landings in different conditions—both with and without snow—learning to launch and catch the drone by hand and maneuver it within tight spaces, simulating the challenges we might encounter in Svalbard.
After mastering these initial steps, I focused on the 360-degree tracking system, which enables the drone to follow and orbit a subject from any angle at varying speeds. This feature will be especially useful for scanning icebergs and other surfaces, allowing us to capture high-quality videos and images for our photogrammetry work.
Drone flying rehearsal, Bellentre, February 2025
Drone flying rehearsal, French Alps, February 2025
With most of the preparations for our field trip and technical explorations slowing getting behind, it's time to refocus on the essentials—the experience we aim to create.
Given the current pace of rising temperatures, Svalbard is poised for radical change in the coming decades. Whispering Glaciers is, in this sense, an attempt to create an immersive, embodied exploration of Svalbard’s landscapes, shaped by our own lived experience during a 10-day expedition through the archipelago.
Our goal is to offer visitors an experience that allows them to freely explore Svalbard’s visual and acoustic environments as they exist in 2025 — the Year of the Glacier. This experience functions as an experiential archive, centring on the landscapes of Svalbard. While the region is home to diverse wildlife, our focus remains on ice—its structures, textures, colours, and behaviours.
We are particularly drawn to capturing the subtle sounds that shape Svalbard’s sonic landscape. Through VR, we seek not only to allow the exploration of visual forms and textures but to amplify often-overlooked sounds—sounds that carry a profound connection to melting, transformation, and, ultimately, disappearance.
The current research is therefore focused on creating a space that allows us to admire the vastness, monumental beauty and uniqueness of such an environment but also reveals its subtle, delicate, and often imperceptible layers. At the same time, it seeks to capture its fleeting, transitional nature—a landscape on the brink of radical transformation or even disappearance.
The installation is expected to have two experiential spaces: 1) a large room with one or more video projections depicting different elements of Svalbard landscapes. 2) a VR experience in which we can explore, by moving in space, different sounds connected to different visual elements of the landscape (glaciers, icebergs, wide spaces covered by snow). The first space is more contemplative and passive, while the second space requires an active engagement, some exploratory investment and curiosity.
The long-expected arrival in Svalbard finally came and the experience started from above, whilst flying over the archipelago before landing. I have followed the suggestions of a local host, who advised me to take a window seat so I could contemplate the landscape during landing and take-off. From above, the view is unforgettable and unique: chains of mountains covered with snow falling on the sea, and at times, separating them, vast white and flat deserts covered by snow. In some locations, the snow covering the mountains and plains along the coastline is already melting, revealing a dark brown rock that separates the blue waters from the white mountain tops. Deep in the fjords it is still possible to observe some parts of frozen sea — however it seems clear that in a matter of days, that ice will be gone and new pathways for boats and tourists will open.
Hansbreen Glacier spotted from the aeroplane, June 2, 2025
The first impressions of Longyearbyen are really interesting and somehow contradictory. First, I became aware, that the place was more open to tourism than I expected from my readings and from all the preparatory work done. When looking at the map, and by watching the photos and documentation that circulate online, Svalbard might come across as a faraway and remote place. However, this impression is almost immediately dissipated as soon as one lands and arrives in Longyearbyen. Despite being a small gathering of wooden buildings, Longyearbyen, shows all the comforts of modern life, including sophisticated restaurants, hotels, cinema, art galleries, museums and supermarkets. So, this is the first strange (and contradictory) feeling: despite the remote location, it’s hard to feel isolated in Longyearbyen, mostly because the population is concentrated on a small piece of land. In comparison, it’s easier to feel more isolated in the Alps or other places on the Norwegian mainland. The sense of isolation, if I can really name it as such, seems to come from the midnight sun effect. Upon arrival, I had the chance to land on a very cold, but very sunny and windless, Longyearbyen. This allowed me to discover the small town while most people were already sleeping or on their way to bed. Being outside, alone with bright sun, on an empty town, was a really peculiar experience that set the tone on what was yet to follow.
Snowscooters parked alongside the Longyearbyen river, June 2, 2025
Snowscooters and wooden houses aligned near the Adventfjorden, June 2, 2025
Wooden houses in Longyearbyen, June 2, 2025
Water pipe network in Longyearbyen, June 2, 2025
While Longyearbyen is a high-end touristic hub, with several fancy restaurants and hotels, interestingly, the place still preserves a certain charm due to its slightly chaotic organisation or lack of it. At times, it seems Longyearbyen was built to last for only a few months or years, as a temporary experiment. Everywhere, around the houses and buildings, one can see a range of equipment and support infrastructure to help locals moving during wintertime — thousands of snow scooters can be seen during June, parked outside, as well as other paraphernalia such as mobile saunas, boating and sea equipment.
After an evening spent exploring Longyearbyen under almost perfect weather conditions, the next day started to change. Adding to the cold weather, the clouds, pushed by moderate to strong winds started to fill the sky above the small town. Coming all the way from Lisbon, André Nascimento, a musician and sound designer, joined the project to help with sound field recordings and sound design. After his arrival, we spent time preparing the equipment, testing, and defining a strategy to store and organise recordings. Then, we started the sound répérage, first by wandering around the town centre, then moving towards the outskirts, the naval area, the church and cemetery, the coal cable centre (Taubanesentralen), and walking along the Longyearbyen river towards the seashore. During this first day of active sound recordings, we focused on capturing the soundscapes of and around Longyearbyen, the sound of birds flocking in the Longyearbyen estuary, the sound of yard dogs howling at the distance, the sounds of the wind, the sounds of passing coal trucks, and the sounds of the river running towards the sea. This day was rich in many aspects — it not only allowed us to have a first understanding and mapping of Longyearbyen from a sonic perspective, showing us the first general different sound sources in and around town, but it also revealed a little bit of the routines of the place. This first day also exposed us immediately to one of the main difficulties in our field work — the wind. The almost omnipresent wind felt throughout the day made the sound recording process quite challenging. Wind, invisible in most photos we see from Svalbard, is an important part of the landscape. One of the main reasons why there are no trees and vegetation is scarce in the archipelago is exactly because wind is an almost permanent condition.
On day 3, we were supposed to leave Longyearbyen towards the north (Nye Alesund). However, our plans were jeopardised by an unfortunate event — during the night, due to strong winds and adverse sea conditions, our guide suffered a sea accident, that would knock out his boat and therefore deeply change our expedition plans. Both this event and the experience from the previous day — the challenges to undertake sound recordings due to omnipresent winds — were sending us a clear message: In Svalbard, you do what you can, not what you want. External/non-human conditions speak louder, and this place makes it very bold. While we waited for a solution, a replacement for the boat, we decided to re-focus on what we had at hand and on the immediate surroundings. This day revealed an interesting aspect — our dependence on others and the limited exploration area. Without a rifle, we become immediately aware of our movement limitations. Outside Longyearbyen, without firearms and other essential equipment and without minimum knowledge of the terrain, you need to rely on others. Nonetheless, spending more time in town and its nearby surroundings allowed us to focus both on natural phenomena, by carefully re-listening to how natural resources intertwine with human made infrastructure, and on the social complexities of the place. It’s hard to do otherwise, when you are suddenly confronted with such a peculiar geographical space and community.
We would learn, for example, that at the end of the month (June 2025), the last coal mine in Norway, the most significant industry in Longyearbyen was going to close, with the shutdown of Mine 7, the last remaining mining operation. For more than a hundred years, coal was extracted from Svalbard. The legacy of this activity is evident not only by the infrastructure that once served to transport the coal from the mines in the mountains to the harbour, the omnipresent trucks that now transport coal from Mine 7 to the harbour, but also by coal itself that marks the landscapes next to the harbour and around the mining sites.
As Zdenka Sokolíčková observed in her book, Svalbard and Longyearbyen are made of paradoxes. We have felt this at several levels. Being a Portuguese, I’ve always seen fishing activities by the sea and generally where there is sea, there’s fish available to buy. We were very surprised when we discovered that the fish caught in Svalbard was sent to mainland Norway to be processed and then sent back again to be sold at COOP Svalbard SA.
Another interesting fact that connects with both the remote location and the geological conditions of Svalbard, was a discovery made in our attempt to visit the interior of the Longyearbyen church. We were advised that the church was closed due to the live stream of a coal miner's funeral. Given that people can’t be buried in Svalbard, his body was taken to mainland Norway, and the funeral was live streamed so locals in Longyearbyen could pay him a last homage.
Lorry carrying coal from Mine 7
Old mining infrastructure links the harbour and the Coal cableway centre
Zdenka Sokolíčková spent several years in Svalbard observing its social dynamics
Despite our growing fascination with Svalbard’s social layers, we were eager to immerse ourselves in landscapes devoid of human presence. While awaiting our boat trip to the tidewater glaciers, we set out for a closer, more accessible one: Foxfonna. Located about 15 km southeast of Longyearbyen, Foxfonna lies on a flat mountain plateau above the EISCAT station.
We walked past the station, leaving behind the mechanical noise of Mine 7, which faded into a silence broken only by occasional bird calls and the sound of our own footsteps. Reaching the plateau felt like stepping into another world — a white desert interrupted by gentle snow-covered hills, reflecting sunlight in sharp variations. The scene felt more like a dream or a digital rendering than reality. This would be one of the strongest and marking experiences I have taken from Svalbard.
We set our sights on a dark snow depth marker in the distance — the only human-made object on the horizon — and began walking towards it. What looked like a short walk took more than 30 minutes, our first direct encounter with the “distance compression” effect common in such wide, featureless landscapes.
Up there, the visual experience dominated, its surrealism amplified by near-total silence. It was as if time itself had slowed. The glacier beneath the snow remained hidden despite our attempts to dig through; it was June, yet winter still clung to the ice. We recorded the ambient stillness and sent a drone aloft to capture the immensity of the plateau and its surroundings.
Appearances, however, deceive. Dr. Arwyn Edwards, a researcher in glacier ecology, describes Foxfonna as “a terminally ill glacier,” adding: “This is palliative, and yet nobody cares.” According to his observations during a recent visit to Svalbard, Foxfonna’s ice surface now lies four metres lower than it did last summer and has been steadily shrinking since his first encounter with it in 2011 (source).
Foxfonna location (toposvalbard.npolar.no)
Aerial view of Adventdalen valley, EISCAT station and the edge of Foxfonna glacier
Aerial view of the expedition team hiking in the Foxfonna glacier edge
André and the guide Noémi hiking in Foxfonna
Snow depth measuring pole spotted from afar at Foxfonna glacier
Drone view showing the vastness and whiteness of the Foxfonna plateau
Filipe digging through the snow in an attempt to reach the glacier beneath (Photo credits: André Nascimento)
André attempting to auscultate the glacier with a contact microphone
GPS display of the day’s completed hiking route
Following the Longyearelva (Longyearbyen River) upstream, in the opposite direction of Adventfjorden, we soon reach Longyearbyenbreen — a narrow glacier roughly 4.5 km long. It begins at Teltberget and extends northeast between Lars Hiertafjellet and Nordenskiöldfjellet to the west.
This glacier is particularly compelling: from its base, we can enjoy a panoramic view of the Longyearbyen valley while clearly witnessing the melting process in action. In the narrow channels, ice melts before our eyes, with water flowing steadily towards the valley and joining the Longyearelva. The glacier surface is relatively smooth, with few crevasses and little debris, apart from sizable ice-cored terminal and lateral moraines. Numerous meltwater channels form across the surface during the ablation season, with lateral drainage systems on both sides containing both supraglacial and englacial reaches (Gulley et al., 2009).
Supraglacial meandering channels carve into the ice each summer. Once these channels reach a depth of 8–12 m, the upper part begins to close due to ice deformation. Over time, they transform into englacial meandering tunnels, some descending 20–50 m to the glacier bed (Guðmundsdóttir, 2011).
A short drive from the town centre to Sverdrupbyen, beneath Gruve 1B, left us about an hour’s walk from the glacier’s edge. Even from this distance, the sonic landscape was vivid: the sound of running water flowing from the mountains towards Longyearbyen and finally into Adventfjorden. Around us, numerous water branches of varying widths crisscrossed the terrain, while some sections remained frozen and others were already breaking apart. At times, gusts of wind overpowered the water’s murmur, dominating the soundscape.
As we ascended, we passed scattered rocks of all sizes, many bearing fossils of deciduous trees from the Cretaceous period — a reminder that this landscape was once home to large-leafed forests.
At the glacier’s threshold, we spent time recording ambient sounds: the wind, water rushing through the valley, and — using hydrophones and contact microphones — the delicate trickle and drip of melting ice. Our guide then led us to an area where remnants of winter channels could still be explored. These channels, formed by flowing water during summer, are completely frozen in winter and can be traversed with minimal risk. In June, however, they were already in retreat: some tunnels revealed rocky walls where ice had receded, yet enough remained for us to observe fascinating melt patterns and capture the rhythmic dripping of ice in its final transformation.
Longyearbyenbreen location (toposvalbard.npolar.no)
Fossilised leaf embedded in stone, Longyearbyenbreen, June, 2025
View over the Longyearbyen Valley
Hiking a steep, snowy slope to reach Loongyearbyenbreen channels
André recording the sounds of melting ice.
Close-up of stratified glacier wall
Detail of icicles forming along the stratified glacier wall
While waiting for a free slot on a boat to Borebreen — despite strong winds, icy rain, and fog — we took the opportunity to continue exploring the surrounding areas of Longyearbyen, particularly those accessible only when carrying a firearm. We spent a considerable amount of time observing and recording the soundscapes around Gruve 1B and Gruve 1A, as well as the steep mountains on the left-hand side of the valley. Here, Arctic terns circled the mountaintop, most likely where their nests were hidden.
As a land of exceptional interest for scientific exploration, Svalbard hosts a range of unique infrastructures that shape the surrounding landscape — not only visually, but also sonically. To explore this less perceptible dimension, we moved towards the Seed Vault area, where we extended our recordings to capture electromagnetic soundscapes from both the building and its surroundings. Using an electromagnetic microphone crafted by Lom, we spent the day listening to the “inaudible” — sounds created by electromagnetic waves. This led us on to the mechanical infrastructure of Mine 7, with its distinctive sonic identity, and further to the EISCAT Svalbard Radar and the SOUSY Svalbard Radar (SSR). The latter is an array of antennas in Adventdalen used for troposphere and mesosphere research — studying tides, gravity waves, turbulence, and their interactions, the structure and dynamics of Polar Mesosphere Summer Echoes, as well as Arctic stratosphere–troposphere dynamics linked to the formation of Polar Stratospheric Clouds and to stratosphere–troposphere exchange processes. (source)
After spending some time listening to these technical infrastructures and their surrounding environments, our attention turned to one of the most pressing subjects in Svalbard and the Arctic: thawing permafrost. Very close to the SSR field, on the riverside of the Adventelva, our guide pointed us towards what seemed at first to be nothing more than moss and dried vegetation. After a 15-minute walk, we found cavities and cracks — some wide, some narrow — where the ice beneath the moss was exposed. Around these openings, water had begun to pool, fed by the melting permafrost. It was an unsettling sight — not only because it was the first time we'd had such a direct glimpse of permafrost, but also because of the far-reaching consequences this thawing holds for the Arctic and for the planet as a whole. Recent studies warn that abrupt permafrost thaw could double carbon emissions (Nature, 2019). In some ways, these understated images of thawing permafrost were even more troubling than the familiar photographs of melting glaciers and icebergs.
The strong wind and light snow made both sound recording and filming a challenge. We decided to return in the coming days to give it another try.
Capturing electromagnetic sounds from Mine 7 mechanical infrastructure
Capturing electromagnetic sounds from SSR
Mountain top at Longyeardalen
Close-up of mountain top
Searching for permafrost cracks near Lomdammen
Exposed permafrost layer with visible ice beneath the tundra surface
Preparing for aerial recording near the EISCAT area
After a long wait for a visit to a tidewater glacier, we left Longyearbyen on a cloudy day to explore the front of Borebreen. This glacial structure, located in Oscar II Land on Spitsbergen — the largest island of the Svalbard archipelago — stretches approximately 22 km in length and about 4 km in width. It flows into the northwestern side of Isfjorden, terminating in Borebukta. As a tidewater glacier, Borebreen calves directly into the sea, shaping both its striking visual presence and its submarine landscape. It is also classified as a surge-type glacier, meaning it remains relatively stable for long periods before undergoing rapid advances. Summer ice velocity measurements show that before 2018, Borebreen moved at around 0.6 m/day, but by 2023 its rate had more than doubled to about 2.4 m/day — a dramatic uptick signalling the start of an active surge phase (Harcourt, 2024).
Our guides suggested we visit Borebreen not only for its proximity to Longyearbyen, but also because of its rapid surging behaviour observed in early June. As we approached Borebukta, we were immediately captivated by the sight of melting ice scattered across the water, and even more by the delicate, sizzling sound it produced — an enveloping, crystalline chorus created by countless small fragments melting.
We learned that glacial ice forms from compressed snow over hundreds to thousands of years, trapping tiny pockets of atmospheric air — miniature time capsules of past climates. In some ice, these bubbles are under significant pressure from the weight of overlying layers. When pieces of glacier or iceberg break off and float in seawater, the warmer environment begins melting them from the outside in. As the ice thins, pressurised bubbles are suddenly exposed, bursting with sharp pops and crackles — a bit like the fizz of a carbonated drink, but sharper and more resonant due to the sudden release and the high pressure within. The greater the pressure difference between the trapped air and the surrounding seawater, the crisper the sound.
If the ice is especially cold and the water relatively warm, melting accelerates, releasing more bubbles in rapid succession. Water transmits these high-frequency sounds with striking clarity, creating an intense, immersive soundscape. Oceanographers sometimes call this the Bergie Seltzer effect.
While we had expected to hear the thunderous crashes of ice calving into the sea, we had not anticipated this intricate, crystalline symphony — a sonic experience that became one of the most vivid moments of our stay in Svalbard, both aurally and visually. We recorded the melting sounds with various microphones, including a hydrophone that revealed low-frequency textures with greater depth.
As we drew closer to the glacier wall, our attention shifted to the interplay of shapes, textures, and the deep blue tones of the ice. The heavy cloud cover softened the light, yet the glacier’s colours remained mesmerising. From time to time, somewhere out of sight, we heard the sharp, gunshot-like report of ice collapsing into the water. After a long sound recording session, we spent considerable time photographing the glacier front from multiple perspectives, taking close-up shots to capture its intricate details and sweeping along the entire wall from left to right — and back again.
Field recording of floating ice and ambient sounds in front of Borebreen (Photo credits: Marcel Schütz)
Floating ice in front of Borebreen.
Floating ice in front of Borebreen.
Filipe recording floating ice sizzling sounds using a Zoom recorder (Photo credits: Marcel Schütz)
André recording floating ice sizzling sounds with a hydrophone (Photo credits: Marcel Schütz)
Due to bad weather conditions, we were unable to continue our expedition at sea and visit other tidewater glaciers. Instead, we decided to return to the banks of the Adventelva River to take a closer look at the thawing permafrost. This time, closer to Longyearbyen, we encountered an even more dramatic scene than in our previous observations. From the roadside, we could see patches of brown moss and tundra vegetation breaking apart, revealing white, crystalline ice beneath. The ice lifted and supported the vegetation in irregular mounds, while meltwater pooled and small streams wound between them. Clear signs of erosion and ground collapse caused by the melting permafrost hinted at what the field we had observed earlier might look like in the near future.
The rest of the day was spent exploring the landscapes of Bjorndalen (bears valley), an eight-kilometre-long valley running along a south–north axis before opening into Isfjorden. It is drained by the Bjordalselva and its tributaries, all fed by glacial meltwater. Vegetation is limited to the surrounding tundra, home to wild reindeer.
On the opposite side of Longyearbyen, we spent some time capturing the Adventdalen valley from a drone’s perspective. The flight began at Tredalshytta and ended roughly 4 km away, near Lomdammen. The footage revealed a striking travelling shot, tracing the intricate network of Adventelva’s channels as they wove their way towards the sea.
Permafrost thawing observed on the banks of the Adventelva River.
Permafrost thawing observed on the banks of the Adventelva River.
As our departure from Svalbard was approaching, on the final day — despite strong winds and a heavy, overcast sky — we managed to charter a sturdy boat to take us back to Borebreen. Our aim was to re-record the floating ice, this time with a binaural microphone to enhance the stereo image and spatial depth.
Curiously, upon arrival at Borebukta, we found the landscape had changed. Just two days earlier, the bay in front of the glacier had been crowded with ice pieces of varying sizes. According to our guides, an easterly wind had pushed much of the ice away. A few scattered pieces remained, enough to allow us to proceed with our recordings. Yet, perhaps due to the colder temperatures, the sizzling sounds we had heard so vividly two days before were now noticeably more subdued. It was, once again, a reminder of how rapidly the landscape shifts, and how dynamic the Svalbard environment is.
After spending considerable time capturing these sounds and trying to record the sharp reports of collapsing ice blocks, we decided to make a short land expedition to see the glacier front from another angle. We boarded a small support zodiac and left the main boat, heading towards the right side of the glacier (Boremorenen). From there, we hiked for nearly an hour until we reached a higher vantage point overlooking the glacier. This position allowed us to continue our environmental sound recordings while also taking privileged, high-resolution photographs of the glacier’s mass and intricate crevasses.
Back in Longyearbyen, we spent the last hours of our stay in the Bolterdalen and Adventdalen valleys, carrying out aerial filming.
Filipe taking close-up photos of the Borebreen glacier front in multiple sections
Floating ice near Borebreen glacier
Borebreen glacier front close-up
Borebreen glacier lateral view
Filipe recording the floating ice melting with a binaural microphone
André recording the floating ice melting with a zoom recorder
Mountain on the left side of Borebreen Glacier
After ten days of residency and fieldwork in Svalbard, we left with mixed feelings. Despite long days of hard work in difficult weather and challenging hikes that would have benefited from a fitter, better-prepared version of ourselves, we departed with the sense that much was still left to do and discover. The residency was first disrupted by our guide’s accident, and later by the demanding weather conditions we had to work through. Most days were windy, cold, and rainy — by far the greatest challenge for sound recording, video work, and drone operations. Our aim was to auscultate Svalbard and its glaciers, yet the wind often made this mission extremely difficult, and at times impossible. Sea expeditions were also curtailed by the weather, limiting our ability to visit a greater number of glaciers.
These setbacks, while at times frustrating, brought valuable insights. We came to understand — and accept — that Svalbard is an environment that resists predictability, where perfect light and acoustic conditions are rare and fleeting. One must be ready, and when those brief moments arrive, make the most of them. In this sense, what we experienced and collected lends the project a more authentic tone; it reflects Svalbard as it truly is at this time of year, rather than an idealized vision.
Although we felt the absence of certain opportunities, we gained much: knowledge of the ecosystems, of the historical and social layers of Svalbard, and an extensive collection of the sound and visual materials we had sought. Even more importantly, we made unexpected discoveries along the way — the extraordinary sonic experience of crackling floating ice, which left a lasting impression and will undoubtedly shape the final outcome of the project; the tangible, unsettling reality of thawing permafrost, visible right before us; and other moments of revelation that no amount of prior research could have anticipated.
As I had hoped, this expedition allowed me to immerse myself fully in Svalbard, experiencing it directly rather than shaping the project from afar through idealized or commonplace depictions of such a rich and nuanced environment. We wanted to carefully listen to the glaciers melting — and we did. At times the sound was quiet and discreet; at others it was punctuated by sudden, gunshot-like bangs; and sometimes it was a delicate sizzling, curiously reminiscent of hot oil in a frying pan, circling back to the very idea of global warming — ironically making me wonder how such a cold place could evoke such a warm image.
If there is one regret, it is not having been able to spend more time in the wild — with the space to explore, observe, and document the transformations of this fragile landscape at a slower, more deliberate pace. But, as always, one needs an entry door. Next time, we will return with a more nuanced approach, ready to go deeper, and to bring back even greater inspiration, awareness, and humility.
Whispering Glaciers — log
Hello world! This is Whispering Glaciers’ development log.
We will be sharing updates on our ongoing research, including insights about Svalbard, the planning of our field trip, artistic and design inspirations, the various testing phases of the project, personal reflections, and, of course, a detailed diary documenting our 10-day expedition in the Svalbard archipelago.
The Whispering Glaciers project takes inspiration from recent observations on the transformations taking place in Svalbard’s ecosystems. Studies suggest that Svalbard is warming four times faster than the global average and is experiencing a severe fast-ice decline. (Rantanen, M., Karpechko, A.Y., Lipponen, A. et al.) This change in weather not only affects the landscape but the ecosystem and the world as a whole.
In the coming years, Svalbard may undergo radical transformations. Sounds, shapes, textures, ecosystem dynamics, and other less visible phenomena could shift into something else. As a consequence, in recent years many have rushed to the archipelago, eager to experience its unique ecosystem before it changes forever.
Whispering Glaciers seeks to create an immersive experience that allows participants to explore the landscapes of the archipelago. This experience will attempt to bring them into close contact with the intricate shapes, textures, colours, ambient tones, and subtle, often inaudible sounds that define this fragile environment. Whispering Glaciers will look into balancing realistic visual representations with more abstract interpretations, challenging conventional perspectives shaped by wildlife films and cinematic portrayals of Svalbard.
Svalbard, Norway, MODIS Land Rapid Response Team, June 7, 2001
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Svalbard is a critical region for studying climate change due to its vast and diverse ice areas. These include glaciers, sea ice, permafrost, and icebergs, each playing a vital role in the global climate system. The total area of the islands is 62,248 km2, and, and, about 59 percent of which is covered by over 2,100 glaciers. Key types include tidewater glaciers, like Kongsbreen, which calve icebergs into fjords; valley glaciers, such as Longyearbreen; and large ice caps, like Austfonna. These polythermal glaciers contain both cold and temperate ice, influencing their dynamics and response to warming.
Sea ice around Svalbard varies seasonally, peaking in winter and retreating in summer. The extent of sea ice has declined in recent decades, impacting ecosystems and serving as a critical climate indicator. It provides a habitat for species like polar bears and Arctic cod, which are under threat as ice diminishes.
Permafrost, which underlies much of Svalbard, is thawing due to rising temperatures. This leads to infrastructure instability, carbon release, and hydrological changes. The ground ice within permafrost plays a key role in maintaining landscape stability.
Icebergs, originating from calving glaciers, are significant for marine ecosystems as they release nutrients while melting. However, they pose challenges for navigation and provide clues about environmental conditions through their shapes and melt rates.
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Kongsbreen glacier
Austfonna glacier (satelite view)
Austfonna glacier
Scheelebreen glacier, 2023
Borebreen glacier, August 2024
We recently came across the work of Dr. Richard Hann, a senior researcher at the Norwegian University of Science and Technology (NTNU), who specializes in icing on unmanned aerial vehicles. Dr. Hann has conducted extensive research on glaciers in Svalbard—such as Tunabreen, Borebreen, Vallåkrabreen, and Wahlenbergbreen—collecting aerial imagery and publishing photos on Kuula, along with 3D glacier models on Sketchfab.
His work is a great contribution to our field trip preparations, helping us in simulating various scenarios for our VR experience. We have begun importing some of his 3D models into Unreal to evaluate rendering quality and performance. These tests will provide deeper insights into the techniques and considerations for capturing glacier and ice imagery, both aerially via drones and from the ground.
To capture unique perspectives and access otherwise unreachable areas of the glaciers, we will be using two drones alongside ground cameras. The first step was selecting the best drones for the task. Since much of our glacier exploration will take place from a boat, one risk quickly became apparent—the possibility of a drone crashing into the water.
We were advised that if a drone went down, we would need to retrieve it from the freezing depths of the sea. This concern played a major role in our decision-making, leading us to choose the SwellPro Splash Drone 4—a waterproof drone capable of landing on water without issue. To complement it, we also acquired the DJI Mavic Pro 3 for its superior image quality. To mitigate the risk of losing it, we equipped it with a foam float system to prevent it from sinking in case of an accident.
French Alps, Aerial view, February 2025
Flying a drone is more complex than it seems. Before I could even start experimenting with it, I had to complete basic training and theoretical courses on drone regulations, pass a test, and ensure I was properly registered. Since I’m flying a drone in the UK, I had to register with the Drone & Model Aircraft Registration Service UK and obtain UK insurance. Additionally, because we’re operating drones in Svalbard, we also had to secure European insurance coverage.
Once all the paperwork was sorted, I finally got my hands on the DJI Mavic Pro 3 and made my first-ever drone takeoff in the French Alps. Over several days, I familiarized myself with the fundamental controls needed to fly safely. I practised takeoffs and landings in different conditions—both with and without snow—learning to launch and catch the drone by hand and maneuver it within tight spaces, simulating the challenges we might encounter in Svalbard.
After mastering these initial steps, I focused on the 360-degree tracking system, which enables the drone to follow and orbit a subject from any angle at varying speeds. This feature will be especially useful for scanning icebergs and other surfaces, allowing us to capture high-quality videos and images for our photogrammetry work.
With most of the preparations for our field trip and technical explorations slowing getting behind, it's time to refocus on the essentials—the experience we aim to create.
Given the current pace of rising temperatures, Svalbard is poised for radical change in the coming decades. Whispering Glaciers is, in this sense, an attempt to create an immersive, embodied exploration of Svalbard’s landscapes, shaped by our own lived experience during a 10-day expedition through the archipelago.
Our goal is to offer visitors an experience that allows them to freely explore Svalbard’s visual and acoustic environments as they exist in 2025 — the Year of the Glacier. This experience functions as an experiential archive, centring on the landscapes of Svalbard. While the region is home to diverse wildlife, our focus remains on ice—its structures, textures, colours, and behaviours.
We are particularly drawn to capturing the subtle sounds that shape Svalbard’s sonic landscape. Through VR, we seek not only to allow the exploration of visual forms and textures but to amplify often-overlooked sounds—sounds that carry a profound connection to melting, transformation, and, ultimately, disappearance.
The current research is therefore focused on creating a space that allows us to admire the vastness, monumental beauty and uniqueness of such an environment but also reveals its subtle, delicate, and often imperceptible layers. At the same time, it seeks to capture its fleeting, transitional nature—a landscape on the brink of radical transformation or even disappearance.
The installation is expected to have two experiential spaces: 1) a large room with one or more video projections depicting different elements of Svalbard landscapes. 2) a VR experience in which we can explore, by moving in space, different sounds connected to different visual elements of the landscape (glaciers, icebergs, wide spaces covered by snow). The first space is more contemplative and passive, while the second space requires an active engagement, some exploratory investment and curiosity.
The long-expected arrival in Svalbard finally came and the experience started from above, whilst flying over the archipelago before landing. I have followed the suggestions of a local host, who advised me to take a window seat so I could contemplate the landscape during landing and take-off. From above, the view is unforgettable and unique: chains of mountains covered with snow falling on the sea, and at times, separating them, vast white and flat deserts covered by snow. In some locations, the snow covering the mountains and plains along the coastline is already melting, revealing a dark brown rock that separates the blue waters from the white mountain tops. Deep in the fjords it is still possible to observe some parts of frozen sea — however it seems clear that in a matter of days, that ice will be gone and new pathways for boats and tourists will open.
Hansbreen Glacier spotted from the aeroplane, June 2, 2025
The first impressions of Longyearbyen are really interesting and somehow contradictory. First, I became aware, that the place was more open to tourism than I expected from my readings and from all the preparatory work done. When looking at the map, and by watching the photos and documentation that circulate online, Svalbard might come across as a faraway and remote place. However, this impression is almost immediately dissipated as soon as one lands and arrives in Longyearbyen. Despite being a small gathering of wooden buildings, Longyearbyen, shows all the comforts of modern life, including sophisticated restaurants, hotels, cinema, art galleries, museums and supermarkets. So, this is the first strange (and contradictory) feeling: despite the remote location, it’s hard to feel isolated in Longyearbyen, mostly because the population is concentrated on a small piece of land. In comparison, it’s easier to feel more isolated in the Alps or other places on the Norwegian mainland. The sense of isolation, if I can really name it as such, seems to come from the midnight sun effect. Upon arrival, I had the chance to land on a very cold, but very sunny and windless, Longyearbyen. This allowed me to discover the small town while most people were already sleeping or on their way to bed. Being outside, alone with bright sun, on an empty town, was a really peculiar experience that set the tone on what was yet to follow.
Snowscooters parked alongside the Longyearbyen river, June 2, 2025
Snowscooters and wooden houses aligned near the Adventfjorden, June 2, 2025
Wooden houses in Longyearbyen, June 2, 2025
Water pipe network in Longyearbyen, June 2, 2025
While Longyearbyen is a high-end touristic hub, with several fancy restaurants and hotels, interestingly, the place still preserves a certain charm due to its slightly chaotic organisation or lack of it. At times, it seems Longyearbyen was built to last for only a few months or years, as a temporary experiment. Everywhere, around the houses and buildings, one can see a range of equipment and support infrastructure to help locals moving during wintertime — thousands of snow scooters can be seen during June, parked outside, as well as other paraphernalia such as mobile saunas, boating and sea equipment.
After an evening spent exploring Longyearbyen under almost perfect weather conditions, the next day started to change. Adding to the cold weather, the clouds, pushed by moderate to strong winds started to fill the sky above the small town. Coming all the way from Lisbon, André Nascimento, a musician and sound designer, joined the project to help with sound field recordings and sound design. After his arrival, we spent time preparing the equipment, testing, and defining a strategy to store and organise recordings. Then, we started the sound répérage, first by wandering around the town centre, then moving towards the outskirts, the naval area, the church and cemetery, the coal cable centre (Taubanesentralen), and walking along the Longyearbyen river towards the seashore. During this first day of active sound recordings, we focused on capturing the soundscapes of and around Longyearbyen, the sound of birds flocking in the Longyearbyen estuary, the sound of yard dogs howling at the distance, the sounds of the wind, the sounds of passing coal trucks, and the sounds of the river running towards the sea. This day was rich in many aspects — it not only allowed us to have a first understanding and mapping of Longyearbyen from a sonic perspective, showing us the first general different sound sources in and around town, but it also revealed a little bit of the routines of the place. This first day also exposed us immediately to one of the main difficulties in our field work — the wind. The almost omnipresent wind felt throughout the day made the sound recording process quite challenging. Wind, invisible in most photos we see from Svalbard, is an important part of the landscape. One of the main reasons why there are no trees and vegetation is scarce in the archipelago is exactly because wind is an almost permanent condition.
On day 3, we were supposed to leave Longyearbyen towards the north (Nye Alesund). However, our plans were jeopardised by an unfortunate event — during the night, due to strong winds and adverse sea conditions, our guide suffered a sea accident, that would knock out his boat and therefore deeply change our expedition plans. Both this event and the experience from the previous day — the challenges to undertake sound recordings due to omnipresent winds — were sending us a clear message: In Svalbard, you do what you can, not what you want. External/non-human conditions speak louder, and this place makes it very bold. While we waited for a solution, a replacement for the boat, we decided to re-focus on what we had at hand and on the immediate surroundings. This day revealed an interesting aspect — our dependence on others and the limited exploration area. Without a rifle, we become immediately aware of our movement limitations. Outside Longyearbyen, without firearms and other essential equipment and without minimum knowledge of the terrain, you need to rely on others. Nonetheless, spending more time in town and its nearby surroundings allowed us to focus both on natural phenomena, by carefully re-listening to how natural resources intertwine with human made infrastructure, and on the social complexities of the place. It’s hard to do otherwise, when you are suddenly confronted with such a peculiar geographical space and community.
We would learn, for example, that at the end of the month (June 2025), the last coal mine in Norway, the most significant industry in Longyearbyen was going to close, with the shutdown of Mine 7, the last remaining mining operation. For more than a hundred years, coal was extracted from Svalbard. The legacy of this activity is evident not only by the infrastructure that once served to transport the coal from the mines in the mountains to the harbour, the omnipresent trucks that now transport coal from Mine 7 to the harbour, but also by coal itself that marks the landscapes next to the harbour and around the mining sites.
As Zdenka Sokolíčková observed in her book, Svalbard and Longyearbyen are made of paradoxes. We have felt this at several levels. Being a Portuguese, I’ve always seen fishing activities by the sea and generally where there is sea, there’s fish available to buy. We were very surprised when we discovered that the fish caught in Svalbard was sent to mainland Norway to be processed and then sent back again to be sold at COOP Svalbard SA.
Another interesting fact that connects with both the remote location and the geological conditions of Svalbard, was a discovery made in our attempt to visit the interior of the Longyearbyen church. We were advised that the church was closed due to the live stream of a coal miner's funeral. Given that people can’t be buried in Svalbard, his body was taken to mainland Norway, and the funeral was live streamed so locals in Longyearbyen could pay him a last homage.
Lorry carrying coal from Mine 7
Old mining infrastructure links the harbour and the Coal cableway centre
Zdenka Sokolíčková spent several years in Svalbard observing its social dynamics
Despite our growing fascination with Svalbard’s social layers, we were eager to immerse ourselves in landscapes devoid of human presence. While awaiting our boat trip to the tidewater glaciers, we set out for a closer, more accessible one: Foxfonna. Located about 15 km southeast of Longyearbyen, Foxfonna lies on a flat mountain plateau above the EISCAT station.
We walked past the station, leaving behind the mechanical noise of Mine 7, which faded into a silence broken only by occasional bird calls and the sound of our own footsteps. Reaching the plateau felt like stepping into another world — a white desert interrupted by gentle snow-covered hills, reflecting sunlight in sharp variations. The scene felt more like a dream or a digital rendering than reality. This would be one of the strongest and marking experiences I have taken from Svalbard.
We set our sights on a dark snow depth marker in the distance — the only human-made object on the horizon — and began walking towards it. What looked like a short walk took more than 30 minutes, our first direct encounter with the “distance compression” effect common in such wide, featureless landscapes.
Up there, the visual experience dominated, its surrealism amplified by near-total silence. It was as if time itself had slowed. The glacier beneath the snow remained hidden despite our attempts to dig through; it was June, yet winter still clung to the ice. We recorded the ambient stillness and sent a drone aloft to capture the immensity of the plateau and its surroundings.
Appearances, however, deceive. Dr. Arwyn Edwards, a researcher in glacier ecology, describes Foxfonna as “a terminally ill glacier,” adding: “This is palliative, and yet nobody cares.” According to his observations during a recent visit to Svalbard, Foxfonna’s ice surface now lies four metres lower than it did last summer and has been steadily shrinking since his first encounter with it in 2011 (source).
Foxfonna location (toposvalbard.npolar.no)
Aerial view of Adventdalen valley, EISCAT station and the edge of Foxfonna glacier
Aerial view of the expedition team hiking in the Foxfonna glacier edge
André and the guide Noémi hiking in Foxfonna
Snow depth measuring pole spotted from afar at Foxfonna glacier
Drone view showing the vastness and whiteness of the Foxfonna plateau
Filipe digging through the snow in an attempt to reach the glacier beneath (Photo credits: André Nascimento)
André attempting to auscultate the glacier with a contact microphone
GPS display of the day’s completed hiking route
Following the Longyearelva (Longyearbyen River) upstream, in the opposite direction of Adventfjorden, we soon reach Longyearbyenbreen — a narrow glacier roughly 4.5 km long. It begins at Teltberget and extends northeast between Lars Hiertafjellet and Nordenskiöldfjellet to the west.
This glacier is particularly compelling: from its base, we can enjoy a panoramic view of the Longyearbyen valley while clearly witnessing the melting process in action. In the narrow channels, ice melts before our eyes, with water flowing steadily towards the valley and joining the Longyearelva. The glacier surface is relatively smooth, with few crevasses and little debris, apart from sizable ice-cored terminal and lateral moraines. Numerous meltwater channels form across the surface during the ablation season, with lateral drainage systems on both sides containing both supraglacial and englacial reaches (Gulley et al., 2009).
Supraglacial meandering channels carve into the ice each summer. Once these channels reach a depth of 8–12 m, the upper part begins to close due to ice deformation. Over time, they transform into englacial meandering tunnels, some descending 20–50 m to the glacier bed (Guðmundsdóttir, 2011).
A short drive from the town centre to Sverdrupbyen, beneath Gruve 1B, left us about an hour’s walk from the glacier’s edge. Even from this distance, the sonic landscape was vivid: the sound of running water flowing from the mountains towards Longyearbyen and finally into Adventfjorden. Around us, numerous water branches of varying widths crisscrossed the terrain, while some sections remained frozen and others were already breaking apart. At times, gusts of wind overpowered the water’s murmur, dominating the soundscape.
As we ascended, we passed scattered rocks of all sizes, many bearing fossils of deciduous trees from the Cretaceous period — a reminder that this landscape was once home to large-leafed forests.
At the glacier’s threshold, we spent time recording ambient sounds: the wind, water rushing through the valley, and — using hydrophones and contact microphones — the delicate trickle and drip of melting ice. Our guide then led us to an area where remnants of winter channels could still be explored. These channels, formed by flowing water during summer, are completely frozen in winter and can be traversed with minimal risk. In June, however, they were already in retreat: some tunnels revealed rocky walls where ice had receded, yet enough remained for us to observe fascinating melt patterns and capture the rhythmic dripping of ice in its final transformation.
Longyearbyenbreen location (toposvalbard.npolar.no)
Fossilised leaf embedded in stone, Longyearbyenbreen, June, 2025
View over the Longyearbyen Valley
Hiking a steep, snowy slope to reach Loongyearbyenbreen channels
André recording the sounds of melting ice.
Close-up of stratified glacier wall
Detail of icicles forming along the stratified glacier wall
While waiting for a free slot on a boat to Borebreen — despite strong winds, icy rain, and fog — we took the opportunity to continue exploring the surrounding areas of Longyearbyen, particularly those accessible only when carrying a firearm. We spent a considerable amount of time observing and recording the soundscapes around Gruve 1B and Gruve 1A, as well as the steep mountains on the left-hand side of the valley. Here, Arctic terns circled the mountaintop, most likely where their nests were hidden.
As a land of exceptional interest for scientific exploration, Svalbard hosts a range of unique infrastructures that shape the surrounding landscape — not only visually, but also sonically. To explore this less perceptible dimension, we moved towards the Seed Vault area, where we extended our recordings to capture electromagnetic soundscapes from both the building and its surroundings. Using an electromagnetic microphone crafted by Lom, we spent the day listening to the “inaudible” — sounds created by electromagnetic waves. This led us on to the mechanical infrastructure of Mine 7, with its distinctive sonic identity, and further to the EISCAT Svalbard Radar and the SOUSY Svalbard Radar (SSR). The latter is an array of antennas in Adventdalen used for troposphere and mesosphere research — studying tides, gravity waves, turbulence, and their interactions, the structure and dynamics of Polar Mesosphere Summer Echoes, as well as Arctic stratosphere–troposphere dynamics linked to the formation of Polar Stratospheric Clouds and to stratosphere–troposphere exchange processes. (source)
After spending some time listening to these technical infrastructures and their surrounding environments, our attention turned to one of the most pressing subjects in Svalbard and the Arctic: thawing permafrost. Very close to the SSR field, on the riverside of the Adventelva, our guide pointed us towards what seemed at first to be nothing more than moss and dried vegetation. After a 15-minute walk, we found cavities and cracks — some wide, some narrow — where the ice beneath the moss was exposed. Around these openings, water had begun to pool, fed by the melting permafrost. It was an unsettling sight — not only because it was the first time we'd had such a direct glimpse of permafrost, but also because of the far-reaching consequences this thawing holds for the Arctic and for the planet as a whole. Recent studies warn that abrupt permafrost thaw could double carbon emissions (Nature, 2019). In some ways, these understated images of thawing permafrost were even more troubling than the familiar photographs of melting glaciers and icebergs.
The strong wind and light snow made both sound recording and filming a challenge. We decided to return in the coming days to give it another try.
Capturing electromagnetic sounds from Mine 7 mechanical infrastructure
Capturing electromagnetic sounds from SSR
Mountain top at Longyeardalen
Close-up of mountain top
Searching for permafrost cracks near Lomdammen
Exposed permafrost layer with visible ice beneath the tundra surface
Preparing for aerial recording near the EISCAT area
After a long wait for a visit to a tidewater glacier, we left Longyearbyen on a cloudy day to explore the front of Borebreen. This glacial structure, located in Oscar II Land on Spitsbergen — the largest island of the Svalbard archipelago — stretches approximately 22 km in length and about 4 km in width. It flows into the northwestern side of Isfjorden, terminating in Borebukta. As a tidewater glacier, Borebreen calves directly into the sea, shaping both its striking visual presence and its submarine landscape. It is also classified as a surge-type glacier, meaning it remains relatively stable for long periods before undergoing rapid advances. Summer ice velocity measurements show that before 2018, Borebreen moved at around 0.6 m/day, but by 2023 its rate had more than doubled to about 2.4 m/day — a dramatic uptick signalling the start of an active surge phase (Harcourt, 2024).
Our guides suggested we visit Borebreen not only for its proximity to Longyearbyen, but also because of its rapid surging behaviour observed in early June. As we approached Borebukta, we were immediately captivated by the sight of melting ice scattered across the water, and even more by the delicate, sizzling sound it produced — an enveloping, crystalline chorus created by countless small fragments melting.
We learned that glacial ice forms from compressed snow over hundreds to thousands of years, trapping tiny pockets of atmospheric air — miniature time capsules of past climates. In some ice, these bubbles are under significant pressure from the weight of overlying layers. When pieces of glacier or iceberg break off and float in seawater, the warmer environment begins melting them from the outside in. As the ice thins, pressurised bubbles are suddenly exposed, bursting with sharp pops and crackles — a bit like the fizz of a carbonated drink, but sharper and more resonant due to the sudden release and the high pressure within. The greater the pressure difference between the trapped air and the surrounding seawater, the crisper the sound.
If the ice is especially cold and the water relatively warm, melting accelerates, releasing more bubbles in rapid succession. Water transmits these high-frequency sounds with striking clarity, creating an intense, immersive soundscape. Oceanographers sometimes call this the Bergie Seltzer effect.
While we had expected to hear the thunderous crashes of ice calving into the sea, we had not anticipated this intricate, crystalline symphony — a sonic experience that became one of the most vivid moments of our stay in Svalbard, both aurally and visually. We recorded the melting sounds with various microphones, including a hydrophone that revealed low-frequency textures with greater depth.
As we drew closer to the glacier wall, our attention shifted to the interplay of shapes, textures, and the deep blue tones of the ice. The heavy cloud cover softened the light, yet the glacier’s colours remained mesmerising. From time to time, somewhere out of sight, we heard the sharp, gunshot-like report of ice collapsing into the water. After a long sound recording session, we spent considerable time photographing the glacier front from multiple perspectives, taking close-up shots to capture its intricate details and sweeping along the entire wall from left to right — and back again.
Field recording of floating ice and ambient sounds in front of Borebreen (Photo credits: Marcel Schütz)
Floating ice in front of Borebreen.
Floating ice in front of Borebreen.
Filipe recording floating ice sizzling sounds using a Zoom recorder (Photo credits: Marcel Schütz)
André recording floating ice sizzling sounds with a hydrophone (Photo credits: Marcel Schütz)
Due to bad weather conditions, we were unable to continue our expedition at sea and visit other tidewater glaciers. Instead, we decided to return to the banks of the Adventelva River to take a closer look at the thawing permafrost. This time, closer to Longyearbyen, we encountered an even more dramatic scene than in our previous observations. From the roadside, we could see patches of brown moss and tundra vegetation breaking apart, revealing white, crystalline ice beneath. The ice lifted and supported the vegetation in irregular mounds, while meltwater pooled and small streams wound between them. Clear signs of erosion and ground collapse caused by the melting permafrost hinted at what the field we had observed earlier might look like in the near future.
The rest of the day was spent exploring the landscapes of Bjorndalen (bears valley), an eight-kilometre-long valley running along a south–north axis before opening into Isfjorden. It is drained by the Bjordalselva and its tributaries, all fed by glacial meltwater. Vegetation is limited to the surrounding tundra, home to wild reindeer.
On the opposite side of Longyearbyen, we spent some time capturing the Adventdalen valley from a drone’s perspective. The flight began at Tredalshytta and ended roughly 4 km away, near Lomdammen. The footage revealed a striking travelling shot, tracing the intricate network of Adventelva’s channels as they wove their way towards the sea.
Permafrost thawing observed on the banks of the Adventelva River.
Permafrost thawing observed on the banks of the Adventelva River.
As our departure from Svalbard was approaching, on the final day — despite strong winds and a heavy, overcast sky — we managed to charter a sturdy boat to take us back to Borebreen. Our aim was to re-record the floating ice, this time with a binaural microphone to enhance the stereo image and spatial depth.
Curiously, upon arrival at Borebukta, we found the landscape had changed. Just two days earlier, the bay in front of the glacier had been crowded with ice pieces of varying sizes. According to our guides, an easterly wind had pushed much of the ice away. A few scattered pieces remained, enough to allow us to proceed with our recordings. Yet, perhaps due to the colder temperatures, the sizzling sounds we had heard so vividly two days before were now noticeably more subdued. It was, once again, a reminder of how rapidly the landscape shifts, and how dynamic the Svalbard environment is.
After spending considerable time capturing these sounds and trying to record the sharp reports of collapsing ice blocks, we decided to make a short land expedition to see the glacier front from another angle. We boarded a small support zodiac and left the main boat, heading towards the right side of the glacier (Boremorenen). From there, we hiked for nearly an hour until we reached a higher vantage point overlooking the glacier. This position allowed us to continue our environmental sound recordings while also taking privileged, high-resolution photographs of the glacier’s mass and intricate crevasses.
Back in Longyearbyen, we spent the last hours of our stay in the Bolterdalen and Adventdalen valleys, carrying out aerial filming.
Filipe taking close-up photos of the Borebreen glacier front in multiple sections
Floating ice near Borebreen glacier
Borebreen glacier front close-up
Borebreen glacier lateral view
Filipe recording the floating ice melting with a binaural microphone
André recording the floating ice melting with a zoom recorder
Mountain on the left side of Borebreen Glacier
After ten days of residency and fieldwork in Svalbard, we left with mixed feelings. Despite long days of hard work in difficult weather and challenging hikes that would have benefited from a fitter, better-prepared version of ourselves, we departed with the sense that much was still left to do and discover. The residency was first disrupted by our guide’s accident, and later by the demanding weather conditions we had to work through. Most days were windy, cold, and rainy — by far the greatest challenge for sound recording, video work, and drone operations. Our aim was to auscultate Svalbard and its glaciers, yet the wind often made this mission extremely difficult, and at times impossible. Sea expeditions were also curtailed by the weather, limiting our ability to visit a greater number of glaciers.
These setbacks, while at times frustrating, brought valuable insights. We came to understand — and accept — that Svalbard is an environment that resists predictability, where perfect light and acoustic conditions are rare and fleeting. One must be ready, and when those brief moments arrive, make the most of them. In this sense, what we experienced and collected lends the project a more authentic tone; it reflects Svalbard as it truly is at this time of year, rather than an idealized vision.
Although we felt the absence of certain opportunities, we gained much: knowledge of the ecosystems, of the historical and social layers of Svalbard, and an extensive collection of the sound and visual materials we had sought. Even more importantly, we made unexpected discoveries along the way — the extraordinary sonic experience of crackling floating ice, which left a lasting impression and will undoubtedly shape the final outcome of the project; the tangible, unsettling reality of thawing permafrost, visible right before us; and other moments of revelation that no amount of prior research could have anticipated.
As I had hoped, this expedition allowed me to immerse myself fully in Svalbard, experiencing it directly rather than shaping the project from afar through idealized or commonplace depictions of such a rich and nuanced environment. We wanted to carefully listen to the glaciers melting — and we did. At times the sound was quiet and discreet; at others it was punctuated by sudden, gunshot-like bangs; and sometimes it was a delicate sizzling, curiously reminiscent of hot oil in a frying pan, circling back to the very idea of global warming — ironically making me wonder how such a cold place could evoke such a warm image.
If there is one regret, it is not having been able to spend more time in the wild — with the space to explore, observe, and document the transformations of this fragile landscape at a slower, more deliberate pace. But, as always, one needs an entry door. Next time, we will return with a more nuanced approach, ready to go deeper, and to bring back even greater inspiration, awareness, and humility.
Noroff School of Technology and Digital Media
Noroff Education AS, Tordenskjoldsgate 9
4612 Kristiansand S
Norway
Dr. Filipe Pais
filipe.pais@noroff.no
Website design by Joana Pestana and Nuno Maio
Dr. Erik Geslin
erik.geslin@noroff.no
Noroff School of
Technology and Digital Media
Noroff Education AS, Tordenskjoldsgate 9
4612 Kristiansand S
Norway
Dr. Filipe Pais
filipe.pais@noroff.no
Dr. Erik Geslin
erik.geslin@noroff.no
Website design by Joana Pestana and Nuno Maio