Building Trust Is Key In Warnings On Melting Glaciers, Pg13
Himalayan disasters like rock-ice avalanches and debris flows, exacerbated by deglaciation, demand robust cross-border early warning systems and community trust for effective mitigation.
A recent disaster in Nepal and Tibet, similar to the 2021 Chamoli disaster, originated from a rock-ice avalanche that transformed into a devastating debris flow.
Initial reports incorrectly suggested an earthquake or a Glacial Lake Outburst Flood (GLOF), but the event was a rock-ice avalanche hitting the valley floor.
Globally, 15 million people face GLOF danger, with over 9 million in High Mountain Asia and nearly 3 million in India.
A significant number of casualties in both the Nepal/Tibet and Chamoli disasters were workers in hydropower infrastructure located in the path of these flows.
The article highlights the challenge of predicting rock-ice avalanches compared to GLOFs, as there are no large lakes to monitor.
Detailed Insights:
The disaster in Nepal and Tibet, referred to as the Rasuwa disaster, was not a GLOF but a rock-ice avalanche, making it harder to plan for.
Rock-ice avalanches can originate from hundreds of thousands of steep, rapidly deglaciating slopes with thawing permafrost in the Himalaya.
While current warning systems can alert those further downstream, they are insufficient for immediate impact zones due to challenges in detection and communication.
A denser seismic station network is proposed as a potential solution to detect landslide-generated earthquakes and flood events.
Implementing such a network requires significant cross-border cooperation across the Himalaya and substantial financial investment.
Building trust within communities regarding warnings and ensuring they know how to respond is crucial for saving lives, though not necessarily the affected areas.
Key Concepts Involved:
Glacial Lake Outburst Flood (GLOF): A sudden release of a significant volume of water from a glacial lake, often caused by the failure of a natural dam.
Rock-ice Avalanche: A rapid flow of rock and ice fragments down a slope, often triggered by thawing permafrost or seismic activity.
Permafrost: Ground (soil, rock, or sediment) that remains frozen for two or more consecutive years, common in high-altitude and polar regions.
Seismic Station Network: A system of interconnected sensors designed to detect and record ground motion caused by earthquakes or other seismic events.