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Climate Change Linked to Deadly Mountain Collapse in Nepal

A glacier and rock collapse in Nepal caused nearly 1,400 deaths and left thousands missing, with scientists linking the disaster to climate change. The collapse, which occurred on August 26, was exacerbated by warming temperatures that destabilized the mountain slope over time. Researchers noted that the region's early warning systems were insufficient to handle the rapid onset of the disaster.

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Walter Immerzeel Friederike Otto

A glacier and rock collapse in Nepal resulted in nearly 1,400 fatalities and left thousands missing. Scientists attribute the disaster to a combination of factors, with climate change significantly contributing to the conditions that led to the collapse. The incident occurred on August 26, when a mountain slope failed, causing flash floods to sweep through valleys in Nepal and Tibet. Initial assessments suggested an earthquake was the cause, but further analysis by glaciologists and climate scientists indicated that warming temperatures had destabilized the slope over time. Walter Immerzeel, a mountain hydrologist at Utrecht University, stated, "This was not a single trigger event," highlighting that multiple processes acted together over years to decades. The collapse began with a large rock avalanche on the north face of Langtang Lirung, which simultaneously caused a section of the glacier to collapse. Approximately 110 million cubic meters of rock and glacier ice fell, equivalent to 44,000 Olympic swimming pools. This type of rock avalanche is rare, occurring at this size only once every 1,000 to 10,000 years. The material fell about 1,400 meters (4,593 feet) to the valley floor, gathering debris and water as it descended, releasing energy comparable to a magnitude 5.2 earthquake. The flood reached the Nepal-China border, 20 kilometers (about 12 miles) downstream, within seven minutes, traveling at an average speed of 170 kilometers per hour (about 106 miles per hour). Researchers from World Weather Attribution noted that rising temperatures from fossil fuel combustion have altered the Himalayas for decades. Near the collapse site, the glacier's edge retreated 75 meters between 1964 and 2000, but from 2010 to 2026, it retreated an additional 373 meters, undermining the rock wall above. Thawing permafrost between 4,500 and 5,500 meters elevation also contributed to instability. July and August were recorded as the warmest months in the area, with climate change increasing temperatures by approximately 1.5 degrees Celsius (2.7 degrees Fahrenheit). On August 24 and 25, temperatures were 2.5 to 2.7 degrees Celsius above the 10-year average, with a maximum temperature about 7 degrees Celsius above the reference mean the day before the collapse. An unusually snowy October in 2025 may have generated additional meltwater. A 2015 earthquake, which registered at magnitude 7.8, may have weakened the rock mass, making the slope more susceptible to failure. Researchers found that the region's early warning systems are designed for rainfall-driven floods, not rapid cascading events like this one, making it difficult to prepare for such disasters. The flood outpaced Nepal's early warning systems, destroying monitoring gauges. The first mass SMS warning was sent 38 minutes after the collapse, but the flood had already reached the border within seven minutes. Friederike Otto, a professor of climate science at Imperial College London, stated, "When warming destabilizes the roof of the world, no amount of local adaptation can fully shield vulnerable people downstream from this scale of destruction." She emphasized the need for faster action to transition to zero fossil fuel emissions to prevent future disasters of this magnitude.

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How climate change worsened Nepal's deadly mountain collapse

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Climate Change Linked to Deadly Mountain Collapse in Nepal