Scientists are baffled to find 3,100 glaciers SURGING – as they warn it might be much more ‘troublesome’ than glacial retreat

While many of the world’s glaciers are in rapid retreat, scientists have been baffled to find 3,100 that are ‘surging’. 

While this might sound like a good thing, the experts warn that it could be even more ‘troublesome’ than glacial retreat.

During a surge, a glacier sends large amounts of ice built up over decades racing downhill, where it rapidly melts in the warm lower-altitude weather.

Surge–prone glaciers make up a large proportion of lost ice in some regions, and experts warn that some are even ‘surging themselves to death’.

While this is bad news for the glaciers themselves, the outlook is even worse for the people who live beside them. 

Unlike most glaciers, which move gradually forward, surging glaciers shift in short bursts of rapid movement lasting a few years, followed by decades-long periods of quiet. 

Lead author Dr Harold Lovell, a glaciologist from the University of Portsmouth, says: ‘They save up ice like a savings account and then spend it all very quickly like a Black Friday event.

‘But while they only represent one per cent of all glaciers worldwide, they affect just under one–fifth of global glacier area, and their behaviour can result in serious and sometimes catastrophic natural disasters that affect thousands of people.’

Scientists have discovered 3,100 glaciers that are not retreating but surging (illustrated), as they warn that this could be even more ‘troubling’ 

Scientists aren’t entirely sure what triggers surges, but research suggests they are probably related to conditions in the glacier’s underside, where ice meets the ground.

These glaciers store massive reserves of ice until heavy rainfall or hot weather trigger a buildup of water beneath the ice, reducing friction and allowing the glacier to slide downhill.

Although it might temporarily look like the glacier is advancing, the results are often catastrophic for the glacier.

Dr Lovell told the Daily Mail: ‘When glaciers surge, they very quickly spend all the ice they have built up over a long period of time. This ice then melts away in warmer temperatures at lower elevations, leaving the glacier very vulnerable. 

‘There are examples of glaciers “surging themselves to death” – losing so much ice during a surge that they cannot recover in the current warmer climate.’

Surging glaciers are also highly concentrated in just a few dense clusters in the Arctic, High Mountain Asia, and the Andes, where there is the right balance of temperature and precipitation.

The problem is that these surges result in huge changes to the environment around the glacier, which can be devastating for nearby settlements.

Glacier surging creates serious hazards for people living near the ice, as the advance threatens to swallow homes, trigger flooding, create landslides, and fill waterways with dangerous icerbergs

The threat posed by the world’s surge–prone glaciers (illustrated) is made worse by the fact that these events are so unpredictable 

Why are surging glaciers dangerous?

  1. Glacier advance: Ice overruns buildings, roads and farmland.
  2. River blockages: Surging glaciers dam rivers, creating dangerous lakes that can release devastating floods.
  3. Meltwater outbursts from beneath the glacier: These also release potentially devastating floods.
  4. Sudden detachments of glaciers: Cause large ice and rock avalanches.
  5. Widespread crevassing: High ice velocities fracture glacier surfaces, making travel extremely hazardous in regions where glaciers serve as highways between settlements and are used for tourism activities, and affecting climbing routes where glaciers provide access to mountain peaks.
  6. Iceberg hazards: When glaciers surge into the sea, they release numerous icebergs in a short time, creating risks for shipping and marine tourism
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Glacier advances can overrun roads, farmland, and even buildings, as well as blocking rivers, creating lakes that can release dangerous floods.

During a surge, meltwater that has built up beneath the glacier can suddenly be released in the form of a devastating flash flood.

The rapid movement forward also makes the glacier less stable, creating a network of widespread crevasses that can be perilous for anyone travelling over the ice.

In extreme cases, the glacier may begin to break up, releasing hazardous icebergs or suddenly detaching in a large ice and rock avalanche.

In their paper, published in Nature Reviews Earth & Environment, the researchers identified the 81 glaciers that pose the greatest danger when they surge.

Most of these are in the Karakoram Mountains, which span China, India, and Pakistan, where populated valleys and critical infrastructure sit directly below surging glaciers such as the Shisper and Kyagar.

However, they can also be found all over the world, with serious threats posed by the Tweedsmuir Glacier in Alaska-Yukon and the Kolka Glacier in the Caucasus.

This risk is made worse by the fact that surges are very hard to predict, and climate change is only making them less reliable.

Of the 81 most dangerous glaciers in the world, most are in the Karakoram mountain range, where inhabited valleys sit directly below surging glaciers such as the Shisper glacier (pictured)

In some areas, glaciers are now so thin that they don’t have the ice to surge, but others are now surging more than ever.

Dr Lovell says: ‘We have been able to piece together the growing body of evidence that shows how climate change is affecting glacier surges, including where and how often they happen.

‘This includes instances of extreme weather such as heavy rainfall events or very warm summers, triggering earlier than expected surges, suggesting an increasing unpredictability in their behaviour.’

Surges might stop altogether in places like Iceland, where glaciers are shrinking rapidly and struggling to build up ice.

But they could become more frequent in parts of High Mountain Asia and in the Canadian and Russian Arctic due to warmer temperatures and increased meltwater.

The researchers even suggest that surges could be seen in the Antarctic Peninsula, where surging glaciers have never been seen before.

Co–author Professor Gwenn Glowers, of Simon Fraser University in Canada, says: ‘Just as we’re starting to develop a more comprehensive understanding of the mechanisms behind glacier surges, climate change is rewriting the rules.

‘Extreme weather events that might have been rare even 50 years ago could become triggers for unexpected surges. Given that surges cause hazards in some settings, this makes protecting vulnerable communities much more difficult.’

The 81 most dangerous surging glaciers on Earth

  1. Ghiacciaio del Belvedere, European Alps
  2. Vernagtferner, European Alps
  3. Tweedsmuir Glacier, Alaska-Yukon
  4. Sít’ Tlein (Malaspina) Glacier, Alaska-Yukon
  5. Hubbard/Valerie Glacier, Alaska-Yukon
  6. Bering Glacier, Alaska-Yukon
  7. Náłúdäy (Lowell) Glacier, Alaska-Yukon
  8. Dań Zhùr (Donjek) Glacier, Alaska-Yukon
  9. Steele Glacier, Alaska-Yukon
  10. Flat Creek Glacier, Alaska-Yukon
  11. Henteel No’ Loo’ (Muldrow) Glacier, Alaska-Yukon
  12. Black Rapids Glacier, Alaska-Yukon
  13. Glaciar Grande del Nevado del Plomo, Andes
  14. Horcones Inferior Glacier, Andes
  15. Juncal Sur Glaciar, Andes
  16. Cachapoal Glaciar, Andes
  17. Tinguiririca 3, Andes
  18. Mittie Glacier, Canadian Arctic
  19. Kolka Glacier, Caucasus
  20. Devdorak Glacier, Caucasus
  21. Davidov Glacier, Central Tien Shan
  22. Lysii Glacier, Central Tien Shan
  23. Northern Inylchek Glacier, Central Tien Shan
  24. Sortebræ, Greenland
  25. Zelunglung Glacier, Eastern Himalaya
  26. Karayaylak/Kelayayilake Glacier, Eastern Pamir
  27. Xiaoma Glacier, Eastern Tibetan Mountains (Tibetan Plateau)
  28. Breiðamerkurjökull east (Norðlingalægðarjökull), Iceland
  29. Skeiðarárjökull, Iceland
  30. Eystri-Hagafellsjökull, Iceland
  31. Shisper (Shishper, Shispare) Glacier, Karakoram
  32. Chong Kumden Glacier, Karakoram
  33. Aktash Glacier, Karakoram
  34. Kichik Kumden Glacier, Karakoram
  35. Kyagar (Keyajir) Glacier, Karakoram
  36. Shinghi (Singkhu, Telamukanli) Glacier, Karakoram
  37. North Gasherbrum Glacier, Karakoram
  38. Urdok Glacier, Karakoram
  39. Khurdopin Glacier, Karakoram
  40. Malangutti Glacier, Karakoram
  41. Yazdghil Glacier, Karakoram
  42. Ghulkin Glacier, Karakoram
  43. Aling Glacier, Karakoram
  44. Yengutz Har Glacier, Karakoram
  45. Yukshin Gardan Glacier, Karakoram
  46. Batura Glacier, Karakoram
  47. Bualtar (Hopar) Glacier, Karakoram
  48. Sultan Chussku Glacier, Karakoram
  49. Balt Bare Glacier, Karakoram
  50. Balthar Glacier, Karakoram
  51. Karamber Glacier, Karakoram
  52. Chillinji Glacier, Karakoram
  53. Chhatteboi Glacier, Karakoram
  54. Warghut Glacier, Karakoram
  55. Sotkher Rabot Glacier, Karakoram
  56. Saklei Shuyinj Glacier, Karakoram
  57. Biafo Glacier, Karakoram
  58. Tashing (Toshain) Glacier, Karakoram
  59. Kutiah Glacier, Karakoram
  60. North Terong Glacier, Karakoram
  61. Chiring Glacier, Karakoram
  62. Sedongpu Glacier, Nyainqentanglha (Tibetan Plateau)
  63. Midui Glacier, Nyainqentanglha (Tibetan Plateau)
  64. Zawadzkibreen, Svalbard
  65. Penckbreen, Svalbard
  66. Moršnevbreen, Svalbard
  67. Scheelebreen, Svalbard
  68. Sefströmbreen, Svalbard
  69. Hinlopenbreen, Svalbard
  70. Fjortende Julibreen, Svalbard
  71. Bråsvellbreen, Svalbard
  72. Austfonna Basin-3, Svalbard
  73. Etonbreen, Svalbard
  74. Aru-1 Glacier, Tibetan Interior (Tibetan Plateau)
  75. Aru-2 Glacier, Tibetan Interior (Tibetan Plateau)
  76. Unnamed Glacier, Petra Pervogo Range, Western Pamir
  77. Unnamed Glacier, Petra Pervogo Range, Western Pamir
  78. Didal Glacier, Western Pamir
  79. Ravak Glacier, Western Pamir
  80. Medvezhiy Glacier, Western Pamir
  81. Geographical Society Glacier, Western Pamir

Source: Harold Lovell, et al., (2026)