Avalanche

An avalanche is a mass of snow and ice falling suddenly down a mountain slope and often taking with it earth, rocks and rubble of every description (WMO, 1992).

Thousands of avalanches occur every year, killing an average of 500 people worldwide. Avalanches occur when massive slabs of snow break loose from a mountainside and shatter like broken glass as they race downhill. These moving masses can reach speeds of 130 km/hour within about five seconds. They cannot always be predicted but the weather conditions, which make them more likely, can be forecast in advance. Most accidents now occur because people ignore warnings. The majority of avalanche incidents are due to slab avalanches with skiers involved. Avalanches are bigger, travel greater distances and are triggered earlier in the year. These changes can be attributed clearly to rising temperatures, which have reached 0.2 to 0.4 degrees annually in some parts of the Himalayas.

Avalanche protection and control measures include early warning which is key (EAWS). By way of controlled explosions, artificial avalanche triggering aims temporarily to safeguard possible starting zones (SLF). Defensive structures prevent the formation of avalanches. In order circumstances, when an avalanche is released, it can be diverted or intercepted by a dam. Other means of protection against avalanches include physical structures for buildings and snow sheds (SLF).

Avalanche risk factors

  • Quick changes in weather, snowpack and terrain.
  • Increasing human populations: winter sports lovers at ski resorts and developers building in vulnerable locations.
  • Climate change.

Vulnerable areas

  • Human settlements in avalanche-prone zones.
  • Rural mountainous villages with no early warning systems.
  • Human settlements with no forest cover.
  • Skiing populations and tourists not educated in avalanche risk.

Risk reduction measures

  • Not constructing buildings, roads, etc. in avalanche hazard areas.
  • Early warning systems at local and national levels.
  • Information on avalanches, their impacts and risks for tourism information offices.
  • Tree planting to protect against the release of avalanches.
  • Building codes and appropriate materials to reinforce resilience.
  • Raising awareness, educating and training residents and visitors on what to do before, during and after an avalanche.

Latest Avalanche additions in the Knowledge Base

The Summary of the Guidelines presented here is the outcome of the work of the Task Force on Climate Change (CC) of the Italian Presidency of the Alpine Convention. The initiative launched during its mandate (2013-2014) is based on the need to implement

The University of Zurich have now analyzed the causes, scope and impact of the Himalayan landslide as part of an international collaboration.
Swiss Federal Research Institute for Forest, Snow and Landscape Research WSL
More than 12,000 deaths have already been attributed to glacial lake outburst floods worldwide
Guardian, the (UK)

Since the end of the 1980s, average annual temperatures in the Espace Mont-Blanc (EMB) have risen between 0.2 and 0.5°C per decade. The rise in temperatures has primarily taken place in spring and summer. No significant trend has been observed in total

Based on the five-level European avalanche danger scale, the avalanche warning services of all European countries assign one of the danger levels to the current situation.
WSL Institute for Snow and Avalanche Research SLF
Climate change played a part in the Chamoli Disaster and that governments should reconsider setting up hydroelectric projects in the higher Himalayas.
The Wire
Cascades of glacier bursts, cloudbursts, heavy rainfall and subsequent landslides are becoming more frequent and complex.
United Nations Economic and Social Commission for Asia and the Pacific (UN-ESCAP)
An expert panel appointed in 2013 had observed that lack of disaster preparedness was a dangerous lacuna.
Live-Mint/Hindustan Times, HT Media Limited

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