Erich Peitzsch, Ph.D
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
Status of Glaciers in Glacier National Park
Snow and Avalanche Research
Secondary Glacier Network
Glacier Monitoring Studies
Glacier Research
Climate drivers of large magnitude snow avalanche years in the U.S. northern Rocky Mountains
A regional spatio-temporal analysis of large magnitude snow avalanches using tree rings
Specialized meltwater biodiversity persists despite widespread deglaciation
Reanalysis of the U.S. Geological Survey Benchmark Glaciers: Long-term insight into climate forcing of glacier mass balance
Forecasting for dry and wet avalanches during mixed rain and snow storm events
Detecting snow depth change in avalanche path starting zones using uninhabited aerial systems and structure from motion photogrammetry
Identifying major avalanche years from a regional tree-ring based avalanche chronology for the U.S. Northern Rocky Mountains
Local topography increasingly influences the mass balance of a retreating cirque glacier
On the exchange of sensible and latent heat between the atmosphere and melting snow
Glaciological measurements and mass balances from Sperry Glacier, Montana, USA, years 2005–2015
Using structure from motion photogrammetry to examine glide snow avalanches
Case study: 2016 Natural glide and wet slab avalanche cycle, Going-to-the-Sun Road, Glacier National Park, Montana, USA
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
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Filter Total Items: 17
Status of Glaciers in Glacier National Park
Glaciers on the Glacier National Park (GNP) landscape have ecological value as a source of cold meltwater in the otherwise dry late summer months, and aesthetic value as the park’s namesake features. USGS scientists have studied these glaciers since the late 1800s, building a body of research that documents widespread glacier change over the past century. Ongoing USGS research pairs long-term data...Snow and Avalanche Research
Snow scientists with the USGS are unraveling specific weather, climate, and snowpack factors that contribute to large magnitude avalanches in an effort to understand these events as both a hazard and a landscape–level disturbance. The Snow and Avalanche Project (SNAP) advances our understanding of avalanche-climate interactions and wet snow avalanches, and improves public safety through innovative...Secondary Glacier Network
The Secondary Glacier Network includes six glaciers (Chaney, Grinnell, Stanton, Agassiz, Swiftcurrent, Jackson-Blackfoot Glaciers) that form a north-south transect of approx. 60 km through the region, with Sperry Glacier just south of center. While these glaciers will be monitored less frequently than the benchmark glacier, Sperry, this network will provide data about the variability of processes...Glacier Monitoring Studies
The purpose of the CCME's glacier monitoring studies is to systematically monitor changes in Glacier National Park’s namesake glaciers and to determine the causes of changes, assess their ecological and hydrological effects, and predict future changes and effects.Glacier Research
Climatic warming since the end of the Little Ice Age has resulted in substantial glacier ice loss around the world. Most glaciers have undergone thinning and many exhibit retreat at their margins. Glacier loss triggers a cascade of hydrological and ecological effects that impact plants, animals and can create human hazard and economic hardship. USGS scientists are using a variety of methods and... - Data
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Filter Total Items: 33
Climate 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. FagreA regional spatio-temporal analysis of large magnitude snow avalanches using tree rings
Snow avalanches affect transportation corridors and settlements worldwide. In many mountainous regions, robust records of avalanche frequency and magnitude are sparse or non-existent. However, dendrochronological methods can be used to fill this gap and infer historical avalanche patterns. In this study, we developed a tree-ring-based avalanche chronology for large magnitude avalanche events (sizeAuthorsErich Peitzsch, Jordy Hendrikx, Daniel Kent Stahle, Gregory T. Pederson, Karl W. Birkeland, Daniel B. FagreSpecialized meltwater biodiversity persists despite widespread deglaciation
Glaciers are important drivers of environmental heterogeneity and biological diversity across mountain landscapes. Worldwide, glaciers are receding rapidly due to climate change, with important consequences for biodiversity in mountain ecosystems. However, the effects of glacier loss on biodiversity have never been quantified across a mountainous region, primarily due to a lack of adequate data atAuthorsClint C. Muhlfeld, Timothy Joseph Cline, J. Joseph Giersch, Erich Peitzsch, Caitlyn Florentine, Dean Jacobsen, Scott HotalingReanalysis of the U.S. Geological Survey Benchmark Glaciers: Long-term insight into climate forcing of glacier mass balance
Mountain glaciers integrate climate processes to provide an unmatched signal of regional climate forcing. However, extracting the climate signal via intercomparison of regional glacier mass balance records can be problematic when methods for extrapolating and calibrating direct glaciological measurements are mixed or inconsistent. To address this problem, we reanalyzed and compared long-term massAuthorsShad O'Neel, Christopher J. McNeil, Louis C. Sass, Caitlyn Florentine, Emily Baker, Erich Peitzsch, Daniel J McGrath, Andrew G. Fountain, Daniel B. FagreForecasting for dry and wet avalanches during mixed rain and snow storm events
Professionals in coastal and some inland mountain ranges regularly face mixed rain-snow events. Professionals in inland ranges frequently deal with persistent slab avalanches failing on old faceted layers buried deep within the snowpack. What happens when you combine these snowpack and weather events? Widespread avalanching involving faceted layers during mixed rain-snow events is rarely observedAuthorsScott Savage, Erich Peitzsch, Simon Trautman, Benjamin VandenBosDetecting snow depth change in avalanche path starting zones using uninhabited aerial systems and structure from motion photogrammetry
Understanding snow depth distribution and change is useful for avalanche forecasting and mitigation, runoff forecasting, and infrastructure planning. Advances in remote sensing are improving the ability to collect snow depth measurements. The development of structure from motion (SfM), a photogrammetry technique, combined with the use of uninhabited aerial systems (UASs) allows for high resolutionAuthorsErich H. Peitzsch, Daniel B. Fagre, Jordy Hendrikx, Karl W. BirkelandIdentifying major avalanche years from a regional tree-ring based avalanche chronology for the U.S. Northern Rocky Mountains
Avalanches not only pose a major hazard to people and infrastructure, but also act as an important ecological disturbance. In many mountainous regions in North America, including areas with existing transportation corridors, reliable and consistent avalanche records are sparse or non-existent. Thus, inferring long-term avalanche patterns and associated contributory climate and weather factors reAuthorsErich H. Peitzsch, Daniel B. Fagre, Gregory T. Pederson, Jordy Hendrikx, Karl W. Birkeland, Daniel StahleLocal topography increasingly influences the mass balance of a retreating cirque glacier
Local topographically driven processes – such as wind drifting, avalanching, and shading – are known to alter the relationship between the mass balance of small cirque glaciers and regional climate. Yet partitioning such local effects from regional climate influence has proven difficult, creating uncertainty in the climate representativeness of some glaciers. We address this problem for Sperry GlaAuthorsCaitlyn Florentine, Joel T. Harper, Daniel B. Fagre, Johnnie Moore, Erich H. PeitzschOn the exchange of sensible and latent heat between the atmosphere and melting snow
The snow energy balance is difficult to measure during the snowmelt period, yet critical for predictions of water yield in regions characterized by snow cover. Robust simplifications of the snowmelt energy balance can aid our understanding of water resources in a changing climate. Research to date has demonstrated that the net turbulent flux (FT) between a melting snowpack and the atmosphere is neAuthorsPaul C. Stoy, Erich H. Peitzsch, David J. A. Wood, Daniel Rottinghaus, Georg Wohlfahrt, Michael Goulden, Helen WardGlaciological measurements and mass balances from Sperry Glacier, Montana, USA, years 2005–2015
Glacier mass balance measurements help to provide an understanding of the behavior of glaciers and their response to local and regional climate. In 2005 the United States Geological Survey established a surface mass balance monitoring program on Sperry Glacier, Montana, USA. This project is the first quantitative study of mass changes of a glacier in the US northern Rocky Mountains and continues tAuthorsAdam Clark, Daniel B. Fagre, Erich H. Peitzsch, Blase A. Reardon, Joel T. HarperUsing structure from motion photogrammetry to examine glide snow avalanches
Structure from Motion (SfM), a photogrammetric technique, has been used extensively and successfully in many fields including geosciences over the past few years to create 3D models and high resolution digital elevation models (DEMs) from aerial or oblique photographs. SfM has recently been used in a limited capacity in snow avalanche research and shows promise as a tool for broader applications.AuthorsErich H. Peitzsch, Jordy Hendrikx, Daniel B. FagreCase study: 2016 Natural glide and wet slab avalanche cycle, Going-to-the-Sun Road, Glacier National Park, Montana, USA
The Going-to-the-Sun Road (GTSR) is the premier tourist attraction in Glacier National Park, Montana. The GTSR also traverses through and under 40 avalanche paths which pose a hazard to National Park Service (NPS) road crews during the annual spring snow plowing operation. Through a joint collaboration between the NPS and the U.S. Geological Survey (USGS), a forecasting program primarily dealing wAuthorsJacob Hutchinson, Erich H. Peitzsch, Adam ClarkNon-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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