Examining Snow Avalanche Frequency and Magnitude
Snow avalanches pose substantial risks to human safety, commerce, and infrastructure in mountainous regions across the globe. Avalanches also act as drivers of important ecological change by creating and modifying habitat for flora and fauna. To better understand the dynamic processes of avalanches at multiple scales, the USGS Snow and Avalanche project uses a variety of methods to study avalanche magnitude and frequency. By advancing the understanding and predictive capabilities of avalanche disturbance, scientists aim to reduce the hazard to humans and more fully understand the ecological role of avalanches. Results from this project provide land-use planners, natural resource managers, and avalanche forecasters a more thorough understanding of how avalanches act as both a hazard and a driver of landscape change.
What is an avalanche?
An avalanche is a mass of snow sliding, tumbling, or flowing down an inclined surface. Slab avalanches can be particularly powerful and destructive due to the speed and force of the mass of snow and the rush of air that sometimes precedes the avalanche. For a slab avalanches to occur, these four conditions are necessary:
- A sufficiently steep slope (most avalanches occur on slopes between 30 and 45 degrees)
- A weak layer in the snowpack
- A slab of snow above that weak layer
- A trigger initiates the fracture and collapse of the weak layer. Triggers can be the accumulation of snow, rain, wind loading, or human/animal disturbance
How do avalanches impact society?
Hazard - When avalanches intersect with humans, there can be substantial cost associated with impacts to commerce, damage to infrastructure, and loss of human life. In the western United States, avalanches are the most frequently occurring lethal form of mass movement and, on an annual basis, cause more fatalities than earthquakes and all other forms of slope failure combined (Voight et al, 1990). They can also impact roads and railways causing substantial damage and disruption to commerce.
Disturbance - Ecologically, avalanches are instrumental in modifying the landscape and adding ecological complexity to mountain ecosystems. By creating and maintaining paths free of large trees, avalanches disturbance creates a mosaic of vegetation types which support a diverse range of plant and animal species.
Challenge – Avalanches are a complex phenomenon due to the complicated interactions of weather, climate, and snowpack structure, and USGS research assessing current and future trends in avalanche activity aims to fill a knowledge gap needed to improve forecasting and public safety, to protect resources, and to lend insight into the ecological role of avalanches.
Snow and Avalanche Project Research Goals
The ability to improve avalanche forecasting in the context of a changing climate depends on a solid understanding of the interplay between the drivers that contribute to avalanche frequency, magnitude, and character. USGS scientists and their collaborators study avalanches across multiple climatic zones throughout the U.S. Rocky Mountains. Dendrochronology (the study of tree rings) and remote sensing provide scientists opportunities to assess avalanche frequency and behavior in the context of changing climate. Research goals seek to address:
1) how avalanche frequency and character vary across space and time
2) what are the primary climate and atmospheric drivers of avalanche variability
Avalanche science – the past informs the future
To understand the relationships between avalanche cycles and climate, scientists can look back in time using dendrochronology, the study of tree rings, and create a chronology of past avalanche events. Annual growth rings of trees that survive avalanches often hold records of large magnitude avalanche events due to tree damage. This mechanical damage can be visible in many forms including scars, reaction wood, or traumatic resin ducts. USGS scientists collect many tree samples across avalanche path study areas and carefully cross-date the growth rings to build a historic record of large magnitude avalanches for each site.
By coupling these avalanche chronologies with historic climate data, USGS scientists tease apart the topographic and climate factors that contribute to avalanche occurrence at local and regional scales. These techniques assist with the understanding of avalanche cycles in the broader context of atmospheric circulation patterns, such as the Pacific Decadal Oscillation (PDO) or El Niño Southern Oscillation (El Niño and La Niña). Through careful dissection of the connections between past climate and avalanche cycles, USGS scientists aim to provide improved avalanche forecasts to reduce the loss of property and life.
Results from the northern Rocky Mountains
Additional Resources:
- USGS Snow and Avalanche Project overview
- Flathead Avalanche Center - avalanche forecasts for Flathead, Swan & Whitefish Ranges & Glacier National Park
- National Avalanche Center and the American Avalanche Association - avalanche information and backcountry avalanche forecasts for the United States
- Going-to-the-Sun Road Avalanche Forecasting Program - Glacier National Park has implemented an avalanche forecasting program to increase safety during the hazardous plowing season. On-site snowpack and start zone evaluations lead to enhanced avalanche forecasting and real-time snow safety.
- Unraveling the History of Avalanches in Juneau blog
- Going to the Sun Road Avalanche Story Map
Below are data or web applications associated with this project.
Below are multimedia items associated with this project.
Below are publications associated with this project.
Case study: 2016 Natural glide and wet slab avalanche cycle, Going-to-the-Sun Road, Glacier National Park, Montana, USA
Using structure from motion photogrammetry to examine glide snow avalanches
Examining spring wet slab and glide avalanche occurrence along the Going-to-the-Sun Road corridor, Glacier National Park, Montana, USA
Timing of wet snow avalanche activity: An analysis from Glacier National Park, Montana, USA.
Time lapse photography as an approach to understanding glide avalanche activity
Avalanche ecology and large magnitude avalanche events: Glacier National Park, Montana, USA
Using GIS and Google Earth for the creation of the Going-to-the-Sun Road Avalanche Atlas, Glacier National Park, Montana, USA
Snow avalanches pose substantial risks to human safety, commerce, and infrastructure in mountainous regions across the globe. Avalanches also act as drivers of important ecological change by creating and modifying habitat for flora and fauna. To better understand the dynamic processes of avalanches at multiple scales, the USGS Snow and Avalanche project uses a variety of methods to study avalanche magnitude and frequency. By advancing the understanding and predictive capabilities of avalanche disturbance, scientists aim to reduce the hazard to humans and more fully understand the ecological role of avalanches. Results from this project provide land-use planners, natural resource managers, and avalanche forecasters a more thorough understanding of how avalanches act as both a hazard and a driver of landscape change.
What is an avalanche?
An avalanche is a mass of snow sliding, tumbling, or flowing down an inclined surface. Slab avalanches can be particularly powerful and destructive due to the speed and force of the mass of snow and the rush of air that sometimes precedes the avalanche. For a slab avalanches to occur, these four conditions are necessary:
- A sufficiently steep slope (most avalanches occur on slopes between 30 and 45 degrees)
- A weak layer in the snowpack
- A slab of snow above that weak layer
- A trigger initiates the fracture and collapse of the weak layer. Triggers can be the accumulation of snow, rain, wind loading, or human/animal disturbance
How do avalanches impact society?
Hazard - When avalanches intersect with humans, there can be substantial cost associated with impacts to commerce, damage to infrastructure, and loss of human life. In the western United States, avalanches are the most frequently occurring lethal form of mass movement and, on an annual basis, cause more fatalities than earthquakes and all other forms of slope failure combined (Voight et al, 1990). They can also impact roads and railways causing substantial damage and disruption to commerce.
Disturbance - Ecologically, avalanches are instrumental in modifying the landscape and adding ecological complexity to mountain ecosystems. By creating and maintaining paths free of large trees, avalanches disturbance creates a mosaic of vegetation types which support a diverse range of plant and animal species.
Challenge – Avalanches are a complex phenomenon due to the complicated interactions of weather, climate, and snowpack structure, and USGS research assessing current and future trends in avalanche activity aims to fill a knowledge gap needed to improve forecasting and public safety, to protect resources, and to lend insight into the ecological role of avalanches.
Snow and Avalanche Project Research Goals
The ability to improve avalanche forecasting in the context of a changing climate depends on a solid understanding of the interplay between the drivers that contribute to avalanche frequency, magnitude, and character. USGS scientists and their collaborators study avalanches across multiple climatic zones throughout the U.S. Rocky Mountains. Dendrochronology (the study of tree rings) and remote sensing provide scientists opportunities to assess avalanche frequency and behavior in the context of changing climate. Research goals seek to address:
1) how avalanche frequency and character vary across space and time
2) what are the primary climate and atmospheric drivers of avalanche variability
Avalanche science – the past informs the future
To understand the relationships between avalanche cycles and climate, scientists can look back in time using dendrochronology, the study of tree rings, and create a chronology of past avalanche events. Annual growth rings of trees that survive avalanches often hold records of large magnitude avalanche events due to tree damage. This mechanical damage can be visible in many forms including scars, reaction wood, or traumatic resin ducts. USGS scientists collect many tree samples across avalanche path study areas and carefully cross-date the growth rings to build a historic record of large magnitude avalanches for each site.
By coupling these avalanche chronologies with historic climate data, USGS scientists tease apart the topographic and climate factors that contribute to avalanche occurrence at local and regional scales. These techniques assist with the understanding of avalanche cycles in the broader context of atmospheric circulation patterns, such as the Pacific Decadal Oscillation (PDO) or El Niño Southern Oscillation (El Niño and La Niña). Through careful dissection of the connections between past climate and avalanche cycles, USGS scientists aim to provide improved avalanche forecasts to reduce the loss of property and life.
Results from the northern Rocky Mountains
Additional Resources:
- USGS Snow and Avalanche Project overview
- Flathead Avalanche Center - avalanche forecasts for Flathead, Swan & Whitefish Ranges & Glacier National Park
- National Avalanche Center and the American Avalanche Association - avalanche information and backcountry avalanche forecasts for the United States
- Going-to-the-Sun Road Avalanche Forecasting Program - Glacier National Park has implemented an avalanche forecasting program to increase safety during the hazardous plowing season. On-site snowpack and start zone evaluations lead to enhanced avalanche forecasting and real-time snow safety.
- Unraveling the History of Avalanches in Juneau blog
- Going to the Sun Road Avalanche Story Map
Below are data or web applications associated with this project.
Below are multimedia items associated with this project.
Below are publications associated with this project.