Glaciers and Climate Project Active
Mountain glaciers are dynamic reservoirs of frozen water closely coupled to ecosystems and climate. Glacier change in North America has major socioeconomic impacts, including global sea level change, tourism disruption, natural hazard risk, fishery effects, and water resource alteration. Understanding and quantifying precise connections between glaciers and climate is critical to decision makers, land managers, and the public, who are affected by these consequences of glacier change. The USGS Glaciers and Climate 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 contemporary methods to reveal glacier-climate 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
Glacier Mass Balance
Research on Other Glaciers
Additional Resources
Surface Mass Balance of the Columbia Glacier, Alaska, 1978 and 2010 Balance Years
A complex relationship between calving glaciers and climate
Re-analysis of Alaskan benchmark glacier mass-balance data using the index method
Fifty-year record of glacier change reveals shifting climate in the Pacific Northwest and Alaska, USA
Comparison of geodetic and glaciological mass-balance techniques, Gulkana Glacier, Alaska, U.S.A
How many stakes are required to measure the mass balance of a glacier?
A strategy for monitoring glaciers
Mountain glaciers are dynamic reservoirs of frozen water closely coupled to ecosystems and climate. Glacier change in North America has major socioeconomic impacts, including global sea level change, tourism disruption, natural hazard risk, fishery effects, and water resource alteration. Understanding and quantifying precise connections between glaciers and climate is critical to decision makers, land managers, and the public, who are affected by these consequences of glacier change. The USGS Glaciers and Climate 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 contemporary methods to reveal glacier-climate 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
Glacier Mass Balance
Research on Other Glaciers
Additional Resources