More Catastrophic Flow Events may Follow the Chamoli Rock and Ice Avalanche under Climate Change.

An editorial focuses on the potential for increased catastrophic flow events in alpine glacier zones due to climate change, using the Chamoli rock-ice avalanche as a case study. It highlights the severe instability of alpine slopes as a consequence of glacial retreat and warming temperatures, suggesting that such events are likely to become more frequent and severe. It emphasizes the need for ongoing monitoring and assessment of these high-risk areas to mitigate future disasters.