ABSTRACT The 5 August 2025 Dharali debris-flow disaster in Uttarakhand exemplifies how climate-driven cryosphere change is reshaping hazard regimes in the Himalaya. Multiple high-intensity debris flow surges from the cirque-glacier fed Kheer Ganga stream destroyed roadside settlement built on an old debris-flow fan deposit. In the recent times, warming-induced glacier retreat, permafrost degradation, and rain-on-snow events exacerbate sediment mobilisation from paraglacial valleys and chronic landslides, creating a non-linear increase in cascading flood-landslide events. Yet despite repeated scientific warnings, rapid urban expansion and unregulated tourism continue to occupy geomorphologically unsafe zones in the Himalayan region. This paper argues that resilience in Himalayan valleys demands integration of high-resolution hazard mapping, terrain-sensitive land-use policy, and community-based early warning systems. Strategic avoidance of high-risk alluvial fans, enforcement of environmental regulations, and adoption of advanced monitoring technologies are essential to safeguard lives and infrastructure under the threat posed by climate change.
Sharma et al. (Fri,) studied this question.