Life

Scientists Explain What Actually Broke Loose Above the Nepal-Tibet Border

This paper reported Thursday that the U.S. Geological Survey had corrected the record on Nepal's flash flood: no earthquake occurred, and the seismic signal that triggered flooding through the Bhote Koshi valley came instead from a glacial collapse. What that coverage did not have time to unpack is the mechanism itself — how a chunk of ice more than a kilometer up a mountainside becomes, in minutes, a 30-foot wall of water racing through towns tens of miles downstream.

The USGS timeline is precise. The landslide of ice and rock struck at 8:37 a.m. local time Wednesday, registering as a magnitude-5.2 seismic event near the Nepal-China border — not an earthquake, but energy released by a mass of ice and rock crashing down a mountainside. [1] Nepal's foreign minister, Shisir Khanal, told the country's parliament the same day that initial reports pointed to an earthquake-triggered landslide; the USGS's subsequent finding overturned that account entirely. [1]

Daniel Shugar, a geomorphologist at the University of Calgary, reconstructed the collapse from satellite imagery for the Guardian: roughly 0.2 square kilometers of ice broke free at an elevation near 5,200 meters and fell about 1,200 meters vertically onto the valley floor below. [1] The imagery showed something else, too — a large amount of snow across the valley had melted in the 24 hours before the collapse. "In other words," Shugar said, "it was probably warm." He added that construction activity in the area could also be a contributing factor, though he had not yet seen weather-station data to confirm the warming observation directly. [1]

Andrew Mackintosh, a glaciologist at Monash University in Melbourne, said it remains unclear whether the failure was confined to the glacier itself or amounted to "the whole mountainside collapsing that included part of the glacier." Either way, the physics of what followed are straightforward: "When a glacier of that scale collapses, it generates a lot of water, and then there's a cascading sequence of events... where the water and the sediment combine and bulks up and creates the flood." [1] That is the difference between this event and a more familiar Himalayan hazard, the glacial lake outburst flood, in which a lake dammed by ice or debris breaches its banks. Experts told the Guardian this collapse was not thought to be a lake-outburst event — the mechanism here is a mass failure that generates its own flood on the way down, rather than releasing water already pooled behind a natural dam. [1]

Mackintosh was candid about the limits of what glaciology can currently say about why this happened now. "These sorts of large glacier collapses are really shocking," he said. "It's hard as a glaciologist not to be alarmed by these events that seem different to what we've observed previously." But he cautioned there have been "so few of these documented that we're not really able to make very clear statements about the specific relationship between glacier collapse and climate change yet" — even as scientists hold "very high confidence" in the separate, better-established link between glacier retreat broadly and climate change. [1] He described mountain permafrost — ground frozen year-round — as a kind of structural glue holding rock and adjacent glaciers together on steep slopes, and noted that warming is degrading that permafrost across the range. The Himalayas are warming roughly twice as fast as the global average, a pace the Guardian notes has already been linked to rising rates of avalanches, landslides and floods across the region. [1]

The scale of Himalayan ice loss underlying that warming trend is not in dispute. A 2023 UN assessment found Nepal's mountains had lost close to a third of their ice in just over 30 years, and that Hindu Kush Himalaya glaciers disappeared 65 percent faster between 2011 and 2020 than in the decade before. [1] The closest prior analog to Wednesday's disaster came in 2021, when a Himalayan glacier broke off and triggered flash flooding in India's Uttarakhand state, leaving roughly 200 people dead or missing; subsequent research found a 27-million-cubic-meter avalanche of rock and ice had transformed into what scientists called "an extraordinarily large and mobile debris flow." [1] Glacial lake outburst floods specifically have killed more than 12,000 people globally, and Nepal alone has more than 2,000 glacial lakes, 21 of them already classified as very high risk — a separate hazard inventory that, notably, did not flag the ice mass that broke off Wednesday, because it was not a lake at all. [1]

That gap — a monitoring system built to watch lakes, failing to watch the mountainside above one — is what glaciologists are now left to reckon with, alongside the harder admission that the field does not yet have enough documented cases of glacier collapse like this one to say how often it will happen again.

-- PRIYA SHARMA, Delhi

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