Item: REVISITING AVALANCHE DESTRUCTIVE SCALE AND ASSOCIATED MASS ESTIMATES
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Title: REVISITING AVALANCHE DESTRUCTIVE SCALE AND ASSOCIATED MASS ESTIMATES
Proceedings: Proceedings, International Snow Science Workshop, Whistler, BC, Canada, 2026
Authors:
- Erich H. Peitzsch [ U.S. Geological Survey, Northern Rocky Mountain Science Center, West Glacier, MT, USA ] [ Montana State University, Department of Earth Sciences, Bozeman, Montana, USA ]
- John M. Sykes [ Simon Fraser University, Avalanche Research Program, Burnaby, BC, Canada ] [ U.S. Geological Survey, Northern Rocky Mountain Science Center, West Glacier, MT, USA ]
- Zachary M. Guy [ Crested Butte Avalanche Center, Crested Butte, CO, USA ]
- Ron Simenhois [ Colorado Avalanche Information Center, Denver, CO, USA ]
- Bruce Jamieson [ Dept of Civil Engineering, University of Calgary, AB, Canada ]
Date: 2026-09-28
Abstract: Avalanche destructive (D) size classifications are essential for forecasting, communication, and risk management, yet size estimation remains one of the more subjective elements of avalanche assessment. Practitioners typically rely on visual impressions of destructive potential, path length, and estimated mass and volume. Recent work indicates that size is often underestimated even by experienced observers, especially when based on photographs or distant observations. Although mass is central to defining destructive size, the empirical foundations of mass–size relationships have rarely been revisited, and expert variability in size assignment could be decreased if more consistent operational tools were available. We evaluated whether a simple, practitioner-focused calculation tool using slab dimensions, snow density, and snow water equivalent can provide reliable mass estimates that correspond meaningfully with existing destructive size classes. Using this tool, we estimated avalanche mass and compared the results to observer-assigned D sizes. We also simulated mass outputs using a dense flow avalanche simulation module and compared observer estimates and simple-tool outputs to recent volume-based methods for D-size classification. Across 143 well-documented dry snow avalanches from multiple avalanche climates, the size estimation tool tends to classify avalanches larger than field-based observers. We found a mean bias of 0.47 D-size units and a typical (mean absolute) disagreement of 0.56. Our results show that 95% of events landed within one whole D-class of each other and 71% within a half-class. Agreement between the simple tool mass estimates and dense flow avalanche simulations was generally strong, though discrepancies emerged in cases with substantial entrainment or complex terrain. We compared the size tool to the simulation module with entrainment (n=4) and without entrainment (n=8). With entrainment, the two methods estimate the same D-size class in 4 of 4 comparable events and 7 of 8 events without entrainment. Also, the simulation module estimates larger sizes than the observer in 7 of 8 cases without entrainment and all 4 cases with entrainment. These findings support that development of practical, mass-based tools could improve D-size consistency and emphasize the value of revisiting historical mass–size relationships. The accompanying application offers practitioners an accessible and operationally useful resource for improving D-size estimation from field observations.
Object ID: ISSW2026_O8.3.pdf
DOI: https://doi.org/10.15788/1790098668
Language of Article: English
Presenter(s): Erich Peitzsch
Keywords: Destructive Scale, Avalanche Size, Avalanche Mass.
Page Number(s): 921 - 931
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