Climate change led to Nepal landslide, scientists find
Climate change contributed to the conditions that led to last month's catastrophic rock and ice collapse on Nepal's northern border by thinning glaciers and thawing the frozen ground that helped hold the mountain together, scientists have concluded.
Scientists have determined that climate change played a significant role in the recent catastrophic landslide in Nepal's northern region. An analysis by World Weather Attribution experts and glaciologists revealed the disaster was not caused by a single weather event, but rather a combination of climatic and geological factors that progressively destabilized the mountain.
Global warming resulting from the burning of fossil fuels has caused the freezing point in the Himalayas to rise by approximately 100 meters per decade. This has exposed previously frozen rock and permafrost to warmer temperatures for extended periods. Simultaneously, significant glacier thinning and retreat have removed the ice that previously helped stabilize the mountain slope.
The two months preceding the disaster were the hottest July and August on record in the area. Heavy snowfall in October and November of the previous year may have also contributed by generating substantial meltwater during the months leading up to the collapse. The scientists emphasized that the mountain itself has been experiencing substantial glacier recession, removing stabilizing ice while increasing the availability of meltwater.
However, the most significant long-term change is occurring within the mountain as centuries-old frozen rock, soil, and sediment are thawing, allowing water to penetrate cracks and weaken slopes previously held together by ice. The report emphasizes that the disaster was a "compound crisis" in which multiple processes acted together rather than one single weather event causing the collapse.
Scientists are particularly concerned that the consequences of warming already experienced in the Himalayas will continue to unfold for decades. Once warming has occurred, it effectively locks in further glacier loss and destabilization of mountain slopes. Limiting further warming through rapid reductions in greenhouse gas emissions and phasing out fossil fuels remains critical to reducing the extent of future destabilization.
Written by urgent.news from RTE News's reporting — not their text. Machine-written — may contain errors; check the original before relying on it.
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