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
Location of five benchmark glaciers
Gulkana
Lemon Creek
South Cascade
Sperry
Wolverine
Glacier Mass Balance
Research on Other Glaciers
Additional Resources
South Cascade Glacier
Gulkana Glacier
Lemon Creek Glacier
Additional Research Glaciers
Wolverine Glacier
Sperry Glacier
Mass Balance Summary
Mass Balance Methods - Measuring Glacier Change
Analyzing North American Glacier Change
Biogeochemistry of glaciers
Time Series of Glacier Retreat
Status of Glaciers in Glacier National Park
Annual End-of-Summer Snow Cover on Glaciers in Alaska and Northwest Canada
Firn Density and Stratigraphy Observations from USGS Benchmark Glaciers
Scanned field notebooks from a USGS Benchmark Glacier: South Cascade Glacier, Washington,1957 - 2022
Geodetic Data for USGS Benchmark Glaciers: Orthophotos, Digital Elevation Models, Glacier Boundaries and Surveyed Positions
Glacier-Wide Mass Balance and Compiled Data Inputs: USGS Benchmark Glaciers
Glacier-Wide Mass Balance and Compiled Data Inputs: Juneau Icefield Glaciers
Raw Ground Penetrating Radar Data on North American Glaciers
Geodetic Data for Juneau Icefield Glaciers: Orthophotos, Digital Elevation Models, and Glacier Boundaries
Weather Station Data on the Juneau Icefield
Point Measurements of Surface Mass Balance, Eklutna Glacier, Alaska, 2008-2015
Direct measurements of firn-density evolution from 2016 to 2022 at Wolverine Glacier, Alaska
Accelerating glacier volume loss on Juneau Icefield driven by hypsometry and melt-accelerating feedbacks
How to handle glacier area change in geodetic mass balance
Inventory of glaciers and perennial snowfields of the conterminous USA
Historical Structure from Motion (HSfM): Automated processing of historical aerial photographs for long-term topographic change analysis
Uncertainty of ICESat-2 ATL06- and ATL08-derived snow depths for glacierized and vegetated mountain regions
U.S. Geological Survey Benchmark Glacier Project
Beyond glacier-wide mass balances: Parsing seasonal elevation change into spatially resolved patterns of accumulation and ablation at Wolverine Glacier, Alaska
Topographic controls on ice flow and recession for Juneau Icefield (Alaska/British Columbia)
The imminent calving retreat of Taku Glacier
f. Glaciers and ice caps outside Greenland
Specialized meltwater biodiversity persists despite widespread deglaciation
Glacier Dashboard
The Glacier - Climate Connection
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
Location of five benchmark glaciers
Gulkana
Lemon Creek
South Cascade
Sperry
Wolverine
Glacier Mass Balance
Research on Other Glaciers
Additional Resources