Avalanche Probability

Avalanche probability refers to the likelihood that a small disturbance, like shifting snow, will trigger a larger, uncontrollable slide down a mountain. It depends on conditions such as snowpack stability, recent weather, and slope angle. When conditions are favorable, even a minor change can cause a large avalanche, indicating higher probability. Conversely, stable conditions mean the risk is low. Understanding avalanche probability helps mountaineers and skiers assess danger and make informed decisions to stay safe in mountain environments.