My main interests lie in the realm of snow and ice.
Research Interests
Previous projects include investigating wet snow avalanche processes, such as water movement in the snowpack and its implications for wet slab avalanches. Working as an avalanche forecaster for the spring opening of the Going-to-the-Sun Road in Glacier National Park allows me to continue work on wet snow avalanche projects such as glide slab avalanches. I am also interested in investigating ecological change associated with avalanches, avalanche runout probability, and the relationship between climate and avalanches. Other research interests include monitoring mass balance of small mountain catchment glaciers.
Professional Experience
Supervisory Research Physical Scientist, USGS Northern Rocky Mountain Science Center, West Glacier, Montana
Education and Certifications
Ph.D. Earth Sciences, Snow Science. 2020. Montana State University, Bozeman
MS. Earth Sciences (Snow Science). 2009. Montana State University, Bozema
BA. Environmental Studies. 2000. Lewis & Clark College, Portland, OR
Science and Products
Evaluating How Snow Avalanches Impact Mountain Goat Populations in Southeast Alaska
Wet Snow Avalanche Research
Remote Sensing Tools Advance Avalanche Research
Examining Snow Avalanche Frequency and Magnitude
Glaciers—Understanding Climate Drivers
USGS Snow and Avalanche Project
Science in Glacier National Park
Time Series of Glacier Retreat
Climate Change in Mountain Ecosystems (CCME)
Going-to-the-Sun Road Avalanche Forecasting Program
Repeat Photography Project
Brief History of Glaciers in Glacier National Park
Historical simulated snowpack and other hydrometeorology data at 30 m for the Crown of the Continent and vicinity, United States and Canada, water years 1981-2020
Historical simulated snowpack and other hydrometeorology data at 90 m for the Crown of the Continent and vicinity, United States and Canada, water years 1981-2020
Tree ring dataset for a regional avalanche chronology in southeast Alaska, 1396 - 2019
USGS Benchmark Glacier Mass Balance and Project Data
2020 winter timeseries of UAS derived digital surface models (DSMs) from the Hourglass study site, Bridger Mountains, Montana, USA
Glacier-Wide Mass Balance and Compiled Data Inputs
Glaciers of Glacier National Park Repeat Photography Collection
Avalanche occurrence records along the Going-to-the-Sun Road, Glacier National Park, Montana from 2003-2023 (ver. 3.0, July 2023)
Tree ring dataset for a regional avalanche chronology in northwest Montana, 1636-2017
Raw Ground Penetrating Radar Data on North American Glaciers
High Altitude Weather Station Data at USGS Benchmark Glaciers
Comparing snowpack meteorological inputs to support regional wet snow avalanche forecasting
Mapping a glide avalanche with terrestrial lidar in Glacier National Park, USA
The relationship between whumpf observations and avalanche activity in Colorado, USA
Under-forecasting wet avalanche cycles: Case studies and lessons learned from two wet avalanche cycles in northwest Montana and central Colorado
Temporal evolution of slab and weak layer properties during the transition from dry to wet snowpack conditions
Big avalanches in a changing climate: Using tree-ring derived avalanche chronologies to examine avalanche frequency across multiple climate types
Spatial extent of forested avalanche terrain impacted by wildfire across the Sawtooth National Forest
Using tree rings to compare Colorado’s 2019 avalanche cycle to previous large avalanche cycles
Tree-ring derived avalanche frequency and climate associations in a high-latitude, maritime climate
Assessing the seasonal evolution of snow depth spatial variability and scaling in complex mountain terrain
Using tree-rings to unravel avalanche frequency and associated climate drivers in the northern Rocky Mountains
No abstract available.
Climate drivers of large magnitude snow avalanche years in the U.S. northern Rocky Mountains
Non-USGS Publications**
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
Science and Products
- Science
Filter Total Items: 17
Evaluating How Snow Avalanches Impact Mountain Goat Populations in Southeast Alaska
Snow avalanches alter mountain environments and have both beneficial and harmful effects on wildlife. Avalanches can benefit wildlife by creating open areas for grazing but can also be deadly when animals are buried in avalanche debris. Avalanches pose high risks to mountain goats because they inhabit rugged and steep terrain, but the actual impacts of avalanches on mountain goats remain unknown. ...Wet Snow Avalanche Research
Wet snow avalanches, including both wet slab and glide avalanches, are dangerous and can be particularly difficult to predict because they are relatively poorly understood compared to dry snow avalanches. They pose significant risk to human life and infrastructure in mountainous areas throughout the world. Wet snow avalanches are caused by weakening in the strength of the snowpack, often triggered...Remote Sensing Tools Advance Avalanche Research
The USGS Snow and Avalanche Project (SNAP) uses remotely sensed technologies to understand snowpack changes that influence water storage, recreation, avalanche hazard and acts as a driver of landscape change. Satellites, uninhabited aerial systems (UAS), and structure-from-motion (SfM) photogrammetry are some of the tools scientists use to collect high resolution imagery that supports ongoing snow...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...Glaciers—Understanding Climate Drivers
Across the globe, glaciers are decreasing in volume and number in response to climate change. Glaciers are important for agriculture, hydropower, recreation, tourism, and biological communities. Loss of glaciers contributes to sea-level rise, creates environmental hazards and can alter aquatic habitats. These are among the cascading effects linked to glacier loss which impact ecosystems and human...USGS Snow and Avalanche Project
Snow avalanches are a widespread natural hazard to humans and infrastructure as well as an important landscape disturbance affecting mountain ecosystems. Forecasting avalanche frequency is challenging on various spatial and temporal scales, and this project aims to fill a gap in snow science by focusing on reconstructing avalanche history on the continental mountain range scale - throughout the...Science in Glacier National Park
Glacier National Park (GNP) is considered a stronghold for a large diversity of plant and animal species and harbors some of the last remaining populations of threatened and endangered species such as grizzly bear and bull trout, as well as non threatened keystone species such as bighorn sheep and black bear. The mountain ecosystems of GNP that support these species are dynamic and influenced by...Time Series of Glacier Retreat
The retreat of glaciers (see PDF at end of page) in Glacier National Park, Montana, has received widespread attention by the media, the public, and scientists because it is a clear and poignant indicator of change in the northern Rocky Mountains of the USA. In 2017, the USGS and Portland State University released a dataset which describes the areas of the 37 named glaciers in Glacier National Park...Climate Change in Mountain Ecosystems (CCME)
Climate change is widely acknowledged to have a profound effect on the biosphere and cryosphere with many and diverse impacts on global resources. Mountain ecosystems in the western U.S., and the U.S. Northern Rocky Mountains in particular, are highly sensitive to climate change. Warming in western Montana is nearly 2 times greater than the rise in global temperatures over the last 100+ years...Going-to-the-Sun Road Avalanche Forecasting Program
As the most popular attraction in Glacier National Park (GNP), the Going-to-the-Sun Road traverses scenic alpine zones and crosses the Continental Divide at Logan Pass (2026m or 6,647' elevation). The Park closes a 56km (34.8 mile) section of the road each winter due to inclement weather, heavy snowfall, and avalanche hazards. Annual spring opening of the road is a highly anticipated event for...Repeat Photography Project
Repeat photography provides objective visual evidence of landscape change. USGS scientists created approximately sixty repeat photography pairs that document glacier change in Glacier National Park. These photograph pairs are available as a collection hosted by the USGS Photographic Library and are publicly available for download. Modern (1997 to 2019) photographs were taken from precisely the...Brief History of Glaciers in Glacier National Park
The history of glaciation in Glacier National Park spans thousands of years of glacial growth and recession, carving the steep and striking mountain features we see today. Glaciers have been present within the boundaries of present-day Glacier National Park since as early as 6,500 years ago (Munroe and others, 2012). These modest glaciers varied in size, tracking climatic trends, but did not grow... - Data
Historical simulated snowpack and other hydrometeorology data at 30 m for the Crown of the Continent and vicinity, United States and Canada, water years 1981-2020
This data release contains historical SnowModel (Liston and Elder, 2006) output for the Crown of the Continent and surrounding areas in Montana, USA; and Alberta and British Columbia, Canada from September 1, 1981 through August 31, 2020. Fifteen daily variables were simulated or derived for this release: (1) snow water equivalent (swed), (2) liquid precipitation (rpre), (3) solid precipitation (sHistorical simulated snowpack and other hydrometeorology data at 90 m for the Crown of the Continent and vicinity, United States and Canada, water years 1981-2020
This data release contains historical SnowModel (Liston and Elder, 2006) output for the Crown of the Continent and surrounding areas in Montana and Idaho, USA; and Alberta and British Columbia, Canada from September 1, 1981 through August 31, 2020. Fifteen daily variables were simulated or derived for this release: (1) snow water equivalent (swed), (2) liquid precipitation (rpre), (3) solid precipTree ring dataset for a regional avalanche chronology in southeast Alaska, 1396 - 2019
This dataset includes processed tree ring data from avalanche paths in southeast Alaska, USA. The data were processed in three distinct phases that resulted in this dataset: collection, processing, and avalanche signal analysis. This dataset consists of samples from 434 cross sections from 426 unique trees throughout six avalanche paths in the study region. This resulted in 2706 identified growthUSGS Benchmark Glacier Mass Balance and Project Data
Since the late 1950s, the USGS has maintained a long-term glacier mass-balance program at three North American glaciers. Measurements began on South Cascade Glacier, WA in 1958, expanding to Gulkana and Wolverine glaciers, AK in 1966, and later Sperry Glacier, MT in 2005. Additional measurements have been made on Lemon Creek Glacier, AK to compliment data collected by the Juneau Icefield Research2020 winter timeseries of UAS derived digital surface models (DSMs) from the Hourglass study site, Bridger Mountains, Montana, USA
Unmanned Aerial System (UAS) flights were conducted over the headwaters of the South Fork of Brackett Creek in the Bridger Mountains of SW Montana during the winter of 2020. The flights collected overlapping imagery focused on a steep mountain couloir study site known locally as "the Hourglass." Structure from motion (SfM) photogrammetry was used to process the collected imagery and create digitalGlacier-Wide Mass Balance and Compiled Data Inputs
Since the late 1950s, the USGS has maintained a long-term glacier mass-balance program at three North American glaciers. Measurements began on South Cascade Glacier, WA in 1958, expanding to Gulkana and Wolverine glaciers, AK in 1966, and later Sperry Glacier, MT in 2005. The Juneau Icefield Research Program has measured surface mass balance on Lemon Creek and Taku Glacier since the mid-1940s, witGlaciers of Glacier National Park Repeat Photography Collection
The “Glaciers of Glacier National Park Repeat Photography Collection” is a compilation of photographs documenting the retreat of glaciers in Glacier National Park, Montana, U.S.A. (GNP) through repeat photography. The collection is comprised of 58 image pairs, resulting from twenty-two years of U.S.Geological Survey (USGS) field excursions (1997-2019) for the purpose of photographically documentinAvalanche occurrence records along the Going-to-the-Sun Road, Glacier National Park, Montana from 2003-2023 (ver. 3.0, July 2023)
Starting in 2003, the U.S. Geological Survey (USGS) Northern Rocky Mountain Science Center in West Glacier, MT, in collaboration with the National Park Service, collected avalanche observations along the Going to the Sun Road during the spring road-clearing operations. The spring road-clearing along Going to the Sun Road utilized a team of avalanche specialists from the USGS and Glacier National PTree ring dataset for a regional avalanche chronology in northwest Montana, 1636-2017
This dataset includes processed tree ring data from avalanche paths in Glacier National Park and the Flathead National Forest in northwest Montana. The data were processed in three distinct phases that resulted in this dataset: collection, processing, and avalanche signal analysis. This dataset consists of samples from 647 trees with 2304 growth disturbances identified from 12 avalanche paths.Raw Ground Penetrating Radar Data on North American Glaciers
U.S. Geological Survey researchers conducted time-series ground-penetrating radar (GPR) surveys with a Sensors and Software 500-MHz Pulse Ekko Pro system. This data release contains ground-based (ski and snowmobile) as well as airborne common-offset profiles. All profiles are linked to coincident GPS observations. Additionally, common-midpoint data was collected at specific glacier locations. CoinHigh Altitude Weather Station Data at USGS Benchmark Glaciers
Since the late 1950s, the USGS has maintained a long-term glacier mass-balance program at three North American glaciers. Measurements began on South Cascade Glacier, WA in 1958, expanding to Gulkana and Wolverine glaciers, AK in 1966, and later Sperry Glacier, MT in 2005. Additional measurements have been made on Lemon Creek Glacier, AK to compliment data collected by the Juneau Icefield Research - Multimedia
- Publications
Filter Total Items: 32
Comparing snowpack meteorological inputs to support regional wet snow avalanche forecasting
Wet snow avalanches are predicted to increase in frequency with climate change and are often difficult to forecast. Improving our understanding of wet snow avalanche timing will help with current forecasting challenges. The onset of wet snow avalanching is closely tied to the temporal progression of liquid water flow through the seasonal snowpack. Measuring the flow of water through the snowpack iAuthorsZachary Miller, Simon Horton, Christoph Mitterer, Erich PeitzschMapping a glide avalanche with terrestrial lidar in Glacier National Park, USA
Thorough documentation of large avalanche events is important for forecasting efforts, infrastructure planning, and investigating the processes involved in avalanche formation and release. However, due in part to the isolated and dangerous nature of avalanche terrain, collecting in-situ, spatially continuous, and quantitative information surrounding avalanches remains difficult. Advances in remoteAuthorsJames W. Dillon, Zachary Miller, Erich Peitzsch, Kevin D. HammondsThe relationship between whumpf observations and avalanche activity in Colorado, USA
Triggering whumpfs is a primary indicator of unstable snowpack conditions. Although backcountry travelers and avalanche forecasters rely on whumpfs as a warning sign of potential avalanches, there is little formal research to confirm this relationship. This study investigated the temporal correlation between whumpfs and avalanche activity in data from Colorado's Front Range and southern San Juan MAuthorsJason Konigsberg, Ron Simenhois, Karl Birkeland, Erich Peitzsch, Doug Chabot, Ethan GreeneUnder-forecasting wet avalanche cycles: Case studies and lessons learned from two wet avalanche cycles in northwest Montana and central Colorado
Predicting the timing and location of natural wet avalanche events is challenging, especially the release of wet slabs. In this study, we describe the existing snowpack structure, weather, and observed avalanche activity for two separate wet avalanche cycles in different avalanche climate types: northwest Montana and central Colorado. In both cases, the regional avalanche forecast centers initiallAuthorsZachary Guy, Erich PeitzschTemporal evolution of slab and weak layer properties during the transition from dry to wet snowpack conditions
Wet-snow slab avalanches are destructive and may become more prevalent in a warming climate. This type of avalanche remains challenging to forecast because the underlying processes leading to wet-snow slab avalanche release are poorly understood. In this study, we examine the temporal evolution of weak layer and slab liquid water content (LWC), critical cut length, and propagation saw test (PST) rAuthorsJosh Lipkowitz, Erich Peitzsch, Jean Dixon, Marcus Kalb, Douglas McCabe, Griffin Ditmar, Christoph MittererBig avalanches in a changing climate: Using tree-ring derived avalanche chronologies to examine avalanche frequency across multiple climate types
Large-magnitude snow avalanches pose a hazard to humans and infrastructure worldwide. Analyzing the spatiotemporal behavior of avalanches and the contributory climate factors is important for understanding historical variability in climate-avalanche relationships as well as improving avalanche forecasting. This study uses established dendrochronological methods to develop long-term regional avalanAuthorsErich Peitzsch, Gregory T. Pederson, Justin Martin, Eran Hood, Ethan Greene, Karl Birkeland, Kelly Elder, Gabriel Wolken, Nickolas E. Kichas, Daniel Kent Stahle, John HarleySpatial extent of forested avalanche terrain impacted by wildfire across the Sawtooth National Forest
Forest structure is a major driver of mountain snowpacks and avalanche occurrence. Healthy forests can reduce the incidence of dangerous slab avalanches, slow avalanches when in motion, shorten their runout distances, and act as a safety buffer for backcountry users, infrastructure, and transportation corridors. Since 1984, wildfire area in the seasonal snow zone of the western United States has iAuthorsZachary Miller, John Sykes, Megan Guinn, Benjamin VandenBos, Scott Savage, Erich PeitzschUsing tree rings to compare Colorado’s 2019 avalanche cycle to previous large avalanche cycles
Large magnitude avalanches (size ≥D3) impact settlements, transportation corridors, and public safety worldwide. In Colorado, United States, avalanches have killed more people than any other natural hazard since 1950. In March 2019, a historically large magnitude avalanche cycle occurred throughout the entire mountainous portion of Colorado resulting in more than 1000 reported avalanches during aAuthorsErich Peitzsch, Ethan Greene, Jason Konigsberg, Gregory T. Pederson, Justin Martin, Nickolas Kichas, Daniel Kent Stahle, Adrien Favillier, Nicolas Eckert, Karl Birkeland, Kelly ElderTree-ring derived avalanche frequency and climate associations in a high-latitude, maritime climate
Snow avalanches are a natural hazard in mountainous areas worldwide with severe impacts that include fatalities, damage to infrastructure, disruption to commerce, and landscape disturbance. Understanding long-term avalanche frequency patterns, and associated climate and weather influences, improves our understanding of how climate change may affect avalanche activity. We used dendrochronological tAuthorsErich Peitzsch, Eran Hood, John Harley, Daniel Kent Stahle, Nicholas E. Kichas, Gabriel J. WolkenAssessing the seasonal evolution of snow depth spatial variability and scaling in complex mountain terrain
Dynamic natural processes govern snow distribution in mountainous environments throughout the world. Interactions between these different processes create spatially variable patterns of snow depth across a landscape. Variations in accumulation and redistribution occur at a variety of spatial scales, which are well established for moderate mountain terrain. However, spatial patterns of snow depth vAuthorsZachary Miller, Erich Peitzsch, Eric A. Sproles, Karl W. Birkeland, Ross T. PalomakiUsing tree-rings to unravel avalanche frequency and associated climate drivers in the northern Rocky Mountains
No abstract available.
AuthorsErich PeitzschClimate drivers of large magnitude snow avalanche years in the U.S. northern Rocky Mountains
Large magnitude snow avalanches pose a hazard to humans and infrastructure worldwide. Analyzing the spatiotemporal behavior of avalanches and the contributory climate factors is important for understanding historical variability in climate-avalanche relationships as well as improving avalanche forecasting. We used established dendrochronological methods to develop a long-term (1867–2019) regionalAuthorsErich Peitzsch, Gregory T. Pederson, Karl W. Birkeland, Jordy Hendrikx, Daniel B. FagreNon-USGS Publications**
Peitzsch, E. 2008. Wet slab avalanches: theory and recent research…or what do we really know about wet slabs?, The Avalanche Review, 26:4, 20-21.**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
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