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 populations.
Predicting and preparing for the wide-ranging consequences of glacier change requires science that helps stakeholders and decision-makers understand connections between glaciers, the environment, and human populations. USGS scientists work collaboratively across climatically diverse glacierized regions to advance our understanding of physical glacier systems and implications of glacier change.
GLACIERS RESPOND TO CLIMATE: Glaciers are intrinsically linked to climate because ice mass gain or loss depends on temperature and precipitation, elements of climate that can be impacted by human actions. Currently, Earth’s glaciers are decreasing in response to climate warming driven largely by increased greenhouse gas emissions. USGS data documenting the extent of glaciers and other mountain cryosphere (frozen) features are available in these published studies by the Climate Change in Mountain Ecosystems (CCME) group.
IMPACTS OF GLACIER LOSS: Loss of glaciers alters habitats in measurable ways. Glacier loss reduces the input of cold freshwater to streams, particularly during late summer months when streamflow is otherwise low. Though studies show that many endemic aquatic species can persist after glaciers have disappeared, the fragmentation and loss of critical habitat may impact genetic diversity and ultimately lead to extinction. In some places, glaciers provide essential drinking water to communities and sustain local livelihoods where meltwater contributes to agricultural practices and recreational use. Glacial melt also contributes to sea level rise and can create flood hazards.
CCME GLACIER RESEARCH: For decades, USGS scientists have studied the physical processes of glaciers, laying the foundation for understanding glacier ecological connections and impacts to society. As glaciers retreat in response to warming temperatures, the USGS Climate Change in Mountain Ecosystems (CCME) group supports a robust glacier research program to study the relationship between climate change and glaciers. Use of both field-based techniques and emerging technologies, like remote sensing, are the hallmarks of continental scale mass balance research at Sperry Glacier. CCME’s focused studies of the glaciers of Glacier National Park provide visitors with understanding of the namesake features and inform management decisions in this protected region.
TRACKING GLACIER LOSS IN GNP: In Glacier National Park (GNP), Montana, average annual temperature warmed over the 20th century by almost double the global average temperature warming. CCME scientists use a variety of methods to track glacier retreat in GNP and have documented a reduction in area of all named glaciers between the Little Ice Age glacial maxima, mid-19th century and 2015.
REPEAT PHOTOGRAPHY: A growing collection of paired glacier images documents glacier loss through the lens of a camera. The USGS’ Repeat Photography Project has been collecting and repeating historic photos of glaciers for over two decades. This photo gallery displays a subset of the collection featuring glaciers across Glacier National Park.
Why study glaciers in Glacier National Park? Glacier National Park
attracts visitors from around the world. Across this glacier-carved landscape, several dozen small mountain glaciers still cling to mountain tops. Glacier National Park is one million acres, protected and recognized internationally as a UNESCO World Heritage Site, an International Peace Park, and a United Nations Biosphere Reserve, indicating the physical and ecological value within its boundaries. The hydrologic, ecologic, and economic impacts linked to glaciers will be measured by loss of habitat, loss of biodiversity, and reduced streamflow for agriculture and recreation. National Park managers, tasked with conserving the landscape and its features for future generations, rely upon USGS science to make informed management decisions and communicate accurate evidenced-based information to the public.
Related Links:
USGS Glacier Retreat Fact Sheet
Below are other science projects associated with this project.
USGS Benchmark Glacier Project
Science in Glacier National Park
Below are data or web applications associated with this project.
Glacier margin time series (1966, 1998, 2005, 2015) of the named glaciers of Glacier National Park, MT, USA
Below are multimedia items associated with this project.
Below are publications associated with this project.
U.S. Geological Survey Benchmark Glacier Project
The U.S. Geological Survey Benchmark Glacier Project combines decades of direct glaciological data with remote sensing data to advance the quantitative understanding of glacier-climate interactions. The global loss of glaciers, and consequent implications for water resources, sea level rise, and ecosystem function underscores the importance of U.S. Geological Survey glaciology research to facilit
Specialized meltwater biodiversity persists despite widespread deglaciation
Parsing complex terrain controls on mountain glacier response to climate forcing
Glacier retreat in Glacier National Park, Montana
Reanalysis of the U.S. Geological Survey Benchmark Glaciers: Long-term insight into climate forcing of glacier mass balance
Glacier recession since the Little Ice Age: Implications for water storage in a Rocky Mountain landscape
Local topography increasingly influences the mass balance of a retreating cirque glacier
Glaciological measurements and mass balances from Sperry Glacier, Montana, USA, years 2005–2015
Glacier-derived August runoff in northwest Montana
Climate change links fate of glaciers and an endemic alpine invertebrate
A century of climate and ecosystem change in Western Montana: What do temperature trends portend?
The Glacier - Climate Connection
The Glacier-Climate Connection geonarrative tells the story of the U.S. Geological Survey Benchmark Glacier Project, one of the longest running studies of glaciers on Earth.
Below are FAQ associated with this project.
How do we know glaciers are shrinking?
Repeat photography and aerial / satellite photo analysis provide evidence of glacier loss in terms of shape and area. The USGS Benchmark Glacier project has collected mass balance data on a network of glaciers in Alaska, Washington, and Montana for decades, quantifying trends of mass loss at all sites. Extensive field data collection at these sites includes twice yearly visits to measure seasonal...
- Overview
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 populations.
Predicting and preparing for the wide-ranging consequences of glacier change requires science that helps stakeholders and decision-makers understand connections between glaciers, the environment, and human populations. USGS scientists work collaboratively across climatically diverse glacierized regions to advance our understanding of physical glacier systems and implications of glacier change.
The three visible glaciers in this photo, Grinnell, Gem and The Salamander Glaciers, have unique rates of retreat, but all have decreased in volume and area since their mid-19th century maximum extent (Credit: John Scurlock (Photographer & Pilot), USGS. Public domain.) GLACIERS RESPOND TO CLIMATE: Glaciers are intrinsically linked to climate because ice mass gain or loss depends on temperature and precipitation, elements of climate that can be impacted by human actions. Currently, Earth’s glaciers are decreasing in response to climate warming driven largely by increased greenhouse gas emissions. USGS data documenting the extent of glaciers and other mountain cryosphere (frozen) features are available in these published studies by the Climate Change in Mountain Ecosystems (CCME) group.
IMPACTS OF GLACIER LOSS: Loss of glaciers alters habitats in measurable ways. Glacier loss reduces the input of cold freshwater to streams, particularly during late summer months when streamflow is otherwise low. Though studies show that many endemic aquatic species can persist after glaciers have disappeared, the fragmentation and loss of critical habitat may impact genetic diversity and ultimately lead to extinction. In some places, glaciers provide essential drinking water to communities and sustain local livelihoods where meltwater contributes to agricultural practices and recreational use. Glacial melt also contributes to sea level rise and can create flood hazards.
CCME GLACIER RESEARCH: For decades, USGS scientists have studied the physical processes of glaciers, laying the foundation for understanding glacier ecological connections and impacts to society. As glaciers retreat in response to warming temperatures, the USGS Climate Change in Mountain Ecosystems (CCME) group supports a robust glacier research program to study the relationship between climate change and glaciers. Use of both field-based techniques and emerging technologies, like remote sensing, are the hallmarks of continental scale mass balance research at Sperry Glacier. CCME’s focused studies of the glaciers of Glacier National Park provide visitors with understanding of the namesake features and inform management decisions in this protected region.
TRACKING GLACIER LOSS IN GNP: In Glacier National Park (GNP), Montana, average annual temperature warmed over the 20th century by almost double the global average temperature warming. CCME scientists use a variety of methods to track glacier retreat in GNP and have documented a reduction in area of all named glaciers between the Little Ice Age glacial maxima, mid-19th century and 2015.
REPEAT PHOTOGRAPHY: A growing collection of paired glacier images documents glacier loss through the lens of a camera. The USGS’ Repeat Photography Project has been collecting and repeating historic photos of glaciers for over two decades. This photo gallery displays a subset of the collection featuring glaciers across Glacier National Park.
Repeat photography documents the retreat of Boulder Glacier, 1910 – 2007. (Credit: 1910 photo by Morton Elrod, GNP Archives, 2007 photo by Dan Fagre, USGS. Public domain.) Why study glaciers in Glacier National Park? Glacier National Park
attracts visitors from around the world. Across this glacier-carved landscape, several dozen small mountain glaciers still cling to mountain tops. Glacier National Park is one million acres, protected and recognized internationally as a UNESCO World Heritage Site, an International Peace Park, and a United Nations Biosphere Reserve, indicating the physical and ecological value within its boundaries. The hydrologic, ecologic, and economic impacts linked to glaciers will be measured by loss of habitat, loss of biodiversity, and reduced streamflow for agriculture and recreation. National Park managers, tasked with conserving the landscape and its features for future generations, rely upon USGS science to make informed management decisions and communicate accurate evidenced-based information to the public.
Related Links:
USGS Glacier Retreat Fact Sheet
- Science
Below are other science projects associated with this project.
USGS Benchmark Glacier Project
Scientists with the USGS Benchmark Glacier Project study the process and impacts of glacier change, including sea-level rise, water resources, environmental hazards and ecosystem links. At the core of this research are mass balance measurements at five glaciers in the United States. Since the 1960s, these glaciers have been studied using direct observations of glaciers and meteorology. The project...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... - Data
Below are data or web applications associated with this project.
Glacier margin time series (1966, 1998, 2005, 2015) of the named glaciers of Glacier National Park, MT, USA
This dataset was created to develop a time series and history of glacier recession in Glacier National Park (GNP), Montana, USA. The dataset delineates the 1966, 1998, 2005 and 2015 perimeters of the 37 named glaciers of Glacier National Park and two additional glaciers on U.S. Forest Services Flathead National Forest land (the Bob Marshall Wilderness Complex) which borders GNP to the south. Estab - Multimedia
Below are multimedia items associated with this project.
- Publications
Below are publications associated with this project.
U.S. Geological Survey Benchmark Glacier Project
The U.S. Geological Survey Benchmark Glacier Project combines decades of direct glaciological data with remote sensing data to advance the quantitative understanding of glacier-climate interactions. The global loss of glaciers, and consequent implications for water resources, sea level rise, and ecosystem function underscores the importance of U.S. Geological Survey glaciology research to facilit
Specialized 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 atParsing complex terrain controls on mountain glacier response to climate forcing
Glaciers are a key indicator of changing climate in the high mountain landscape. Glacier variations across a mountain range are ultimately driven by regional climate forcing. However, changes also reflect local, topographically driven processes such as snow avalanching, snow wind-drifting, and radiation shading as well as the initial glacier conditions such as hypsometry and ice thickness. Here weGlacier retreat in Glacier National Park, Montana
Currently, the volume of land ice on Earth is decreasing, driving consequential changes to global sea level and local stream habitat. Glacier retreat in Glacier National Park, Montana, U.S.A., is one example of land ice loss and glacier change. The U.S. Geological Survey Benchmark Glacier Project conducts glaciological research and collects field measurements across select North American glaciers,Reanalysis 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 massGlacier recession since the Little Ice Age: Implications for water storage in a Rocky Mountain landscape
Glacial ice is a significant influence on local climate, hydrology, vegetation, and wildlife. We mapped a complete set of glacier areas from the Little Ice Age (LIA) using very high-resolution satellite imagery (30-cm) within Glacier National Park, a region that encompasses over 400,000 hectares. We measured glacier change across the park using LIA glacier area as a baseline and used this to estimLocal 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 GlaGlaciological 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 tGlacier-derived August runoff in northwest Montana
The second largest concentration of glaciers in the U.S. Rocky Mountains is located in Glacier National Park (GNP), Montana. The total glacier-covered area in this region decreased by ∼35% over the past 50 years, which has raised substantial concern about the loss of the water derived from glaciers during the summer. We used an innovative weather station design to collect in situ measurements on fClimate change links fate of glaciers and an endemic alpine invertebrate
Climate warming in the mid- to high-latitudes and high-elevation mountainous regions is occurring more rapidly than anywhere else on Earth, causing extensive loss of glaciers and snowpack. However, little is known about the effects of climate change on alpine stream biota, especially invertebrates. Here, we show a strong linkage between regional climate change and the fundamental niche of a rare aA century of climate and ecosystem change in Western Montana: What do temperature trends portend?
The physical science linking human-induced increases in greenhouse gasses to the warming of the global climate system is well established, but the implications of this warming for ecosystem processes and services at regional scales is still poorly understood. Thus, the objectives of this work were to: (1) describe rates of change in temperature averages and extremes for western Montana, a region c - Web Tools
The Glacier - Climate Connection
The Glacier-Climate Connection geonarrative tells the story of the U.S. Geological Survey Benchmark Glacier Project, one of the longest running studies of glaciers on Earth.
- FAQ
Below are FAQ associated with this project.
How do we know glaciers are shrinking?
Repeat photography and aerial / satellite photo analysis provide evidence of glacier loss in terms of shape and area. The USGS Benchmark Glacier project has collected mass balance data on a network of glaciers in Alaska, Washington, and Montana for decades, quantifying trends of mass loss at all sites. Extensive field data collection at these sites includes twice yearly visits to measure seasonal...