Mountain glaciers are dynamic reservoirs of frozen water, deeply interconnected with their surrounding ecosystems. Glacier change in North America has major societal impacts, including to water resources, natural hazard risk, tourism disruption, fisheries, and global sea level change. Understanding and quantifying precise connections between changing glaciers, the surrounding landscape and climate is critical to decision makers, land managers, and the public, who are affected by these consequences of glacier change. The USGS Benchmark Glacier Project is aimed at solving complex scientific problems in snow and ice across North America to promote enhanced monitoring, analysis, and prediction of mountain glacier change. Utilizing expertise across USGS, this project combines legacy glacier monitoring with remote sensing and contemporary analytical methods to create novel insight and deliver relevant, actionable science.
USGS Benchmark Glacier Project
The flagship research effort of the Glaciers and Climate Project is a multi-glacier, decades-long study of glacier-climate response. Since the 1950s, glacier mass-balance measurements have been systematically collected at five benchmark glaciers, beginning with South Cascade (WA) and later including Gulkana, Wolverine and Lemon Creek Glaciers (AK). Sperry Glacier (MT), monitored since 2005, was added to complete the geographically diverse network in 2013.
Results from this monitoring form the longest continuous record of North American glacier mass balance, which capture seasonal and year-to-year variability. These intensively studied glaciers provide insight into the connection between climate and glaciers at multiple scales.
Historic glacier monitoring has involved various mission areas across USGS, but research was unified into one cohesive program in 2019 (O'Neel and others, 2019). Common field methodologies coupled with long-term, consistently analyzed records, are the hallmark of the Benchmark Glacier Project. Such consistency among sites allows glacier records from different climate zones of North America to be directly compared in order to better understand the impacts of mountain glacier change response of glaciers. Four of the glaciers are considered ‘reference’ glaciers in the World Glacier Monitoring Service’s internationally coordinated glacier monitoring network.
The USGS Benchmark Glacier Project also incorporates data collected from spaceborne and airborne platforms, enabling scientists to document three-dimensional glacier change at regional scales. This application of remotely sensed data broadens the project’s scope and relevance to facilitate glacier change projections, which guide sea level and water resource management strategies.
Benchmark Glaciers
Location of five benchmark glaciers
Gulkana
Lemon Creek
South Cascade
Sperry
Wolverine
Glacier Mass Balance
Research on Other Glaciers
Additional Resources
Glacier-Wide Mass Balance and Input Data
This data release includes compiled inputs to calculate glacier-wide mass balances, including point mass balances, time-variable area-altitude distributions, geodetic mass changes, and daily values of temperature and precipitation from proximal weather stations. If the input data is complete, there are also files with calculated glacier-wide mass balances.
Glaciological and marine geological controls on terminus dynamics of Hubbard Glacier, southeast Alaska Glaciological and marine geological controls on terminus dynamics of Hubbard Glacier, southeast Alaska
Icefield-to-ocean linkages across the northern Pacific coastal temperate rainforest ecosystem Icefield-to-ocean linkages across the northern Pacific coastal temperate rainforest ecosystem
Unusually loud ambient noise in tidewater glacier fjords: a signal of ice melt Unusually loud ambient noise in tidewater glacier fjords: a signal of ice melt
Glacier-derived August runoff in northwest Montana Glacier-derived August runoff in northwest Montana
Storage and release of organic carbon from glaciers and ice sheets Storage and release of organic carbon from glaciers and ice sheets
Oceanic and atmospheric forcing of Larsen C Ice-Shelf thinning Oceanic and atmospheric forcing of Larsen C Ice-Shelf thinning
Climate change and the Rocky Mountains Climate change and the Rocky Mountains
Assessing streamflow sensitivity to variations in glacier mass balance Assessing streamflow sensitivity to variations in glacier mass balance
Analysis of a GRACE global mascon solution for Gulf of Alaska glaciers Analysis of a GRACE global mascon solution for Gulf of Alaska glaciers
Surface Mass Balance of the Columbia Glacier, Alaska, 1978 and 2010 Balance Years Surface Mass Balance of the Columbia Glacier, Alaska, 1978 and 2010 Balance Years
A complex relationship between calving glaciers and climate A complex relationship between calving glaciers and climate
Re-analysis of Alaskan benchmark glacier mass-balance data using the index method Re-analysis of Alaskan benchmark glacier mass-balance data using the index method
Mountain glaciers are dynamic reservoirs of frozen water, deeply interconnected with their surrounding ecosystems. Glacier change in North America has major societal impacts, including to water resources, natural hazard risk, tourism disruption, fisheries, and global sea level change. Understanding and quantifying precise connections between changing glaciers, the surrounding landscape and climate is critical to decision makers, land managers, and the public, who are affected by these consequences of glacier change. The USGS Benchmark Glacier Project is aimed at solving complex scientific problems in snow and ice across North America to promote enhanced monitoring, analysis, and prediction of mountain glacier change. Utilizing expertise across USGS, this project combines legacy glacier monitoring with remote sensing and contemporary analytical methods to create novel insight and deliver relevant, actionable science.
USGS Benchmark Glacier Project
The flagship research effort of the Glaciers and Climate Project is a multi-glacier, decades-long study of glacier-climate response. Since the 1950s, glacier mass-balance measurements have been systematically collected at five benchmark glaciers, beginning with South Cascade (WA) and later including Gulkana, Wolverine and Lemon Creek Glaciers (AK). Sperry Glacier (MT), monitored since 2005, was added to complete the geographically diverse network in 2013.
Results from this monitoring form the longest continuous record of North American glacier mass balance, which capture seasonal and year-to-year variability. These intensively studied glaciers provide insight into the connection between climate and glaciers at multiple scales.
Historic glacier monitoring has involved various mission areas across USGS, but research was unified into one cohesive program in 2019 (O'Neel and others, 2019). Common field methodologies coupled with long-term, consistently analyzed records, are the hallmark of the Benchmark Glacier Project. Such consistency among sites allows glacier records from different climate zones of North America to be directly compared in order to better understand the impacts of mountain glacier change response of glaciers. Four of the glaciers are considered ‘reference’ glaciers in the World Glacier Monitoring Service’s internationally coordinated glacier monitoring network.
The USGS Benchmark Glacier Project also incorporates data collected from spaceborne and airborne platforms, enabling scientists to document three-dimensional glacier change at regional scales. This application of remotely sensed data broadens the project’s scope and relevance to facilitate glacier change projections, which guide sea level and water resource management strategies.
Benchmark Glaciers
Location of five benchmark glaciers
Gulkana
Lemon Creek
South Cascade
Sperry
Wolverine
Glacier Mass Balance
Research on Other Glaciers
Additional Resources
Glacier-Wide Mass Balance and Input Data
This data release includes compiled inputs to calculate glacier-wide mass balances, including point mass balances, time-variable area-altitude distributions, geodetic mass changes, and daily values of temperature and precipitation from proximal weather stations. If the input data is complete, there are also files with calculated glacier-wide mass balances.