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Here's how you know
There is still some uncertainty about the full volume of glaciers and ice caps on Earth, but if all of them were to melt, global sea level would rise approximately 70 meters (approximately 230 feet), flooding every coastal city on the planet.
Learn more:
- USGS Water Science School:Glaciers and Icecaps
- National Snow and Ice Data Center:Facts about Glaciers
- U.S. Global Change Research Program:Sea Level Rise
Related Content
- FAQ
- Multimedia
- Publications
- News
What are the impacts of glacier loss, other than losing an aesthetic landscape feature?
Glaciers act as reservoirs of water that persist through summer. Continual melt from glaciers contributes water to the ecosystem throughout dry months, creating perennial stream habitat and a water source for plants and animals. The cold runoff from glaciers also affects downstream water temperatures. Many aquatic species in mountainous environments require cold water temperatures to survive. Some...
Glaciers act as reservoirs of water that persist through summer. Continual melt from glaciers contributes water to the ecosystem throughout dry months, creating perennial stream habitat and a water source for plants and animals. The cold runoff from glaciers also affects downstream water temperatures. Many aquatic species in mountainous environments require cold water temperatures to survive. Some...
Are today's glaciers leftovers from the Pleistocene ice age?
Yes and no. It depends on which glaciers you are considering. Parts of the Antarctic Continent have had continuous glacier cover for perhaps as long as 20 million years. Other areas, such as valley glaciers of the Antarctic Peninsula and glaciers of the Transantarctic Mountains may date from the early Pleistocene. For Greenland, ice cores and related data suggest that all of southern Greenland and...
Yes and no. It depends on which glaciers you are considering. Parts of the Antarctic Continent have had continuous glacier cover for perhaps as long as 20 million years. Other areas, such as valley glaciers of the Antarctic Peninsula and glaciers of the Transantarctic Mountains may date from the early Pleistocene. For Greenland, ice cores and related data suggest that all of southern Greenland and...
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...
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...
How does present glacier extent and sea level compare to the extent of glaciers and global sea level during the Last Glacial Maximum (LGM)?
The Last Glacial Maximum (LGM) occurred about 20,000 years ago, during the last phase of the Pleistocene epoch. At that time, global sea level was more than 400 feet lower than it is today, and glaciers covered approximately: 8% of Earth’s surface 25% of Earth’s land area 33% of Alaska Beginning about 15,000 years ago, continental glaciers retreated and sea level began to rise. Sea level reached...
How does present glacier extent and sea level compare to the extent of glaciers and global sea level during the Last Glacial Maximum (LGM)?
The Last Glacial Maximum (LGM) occurred about 20,000 years ago, during the last phase of the Pleistocene epoch. At that time, global sea level was more than 400 feet lower than it is today, and glaciers covered approximately: 8% of Earth’s surface 25% of Earth’s land area 33% of Alaska Beginning about 15,000 years ago, continental glaciers retreated and sea level began to rise. Sea level reached...
How many glaciers currently exist in Alaska?
Based on the most recent comprehensive survey in 2011, there were about 27,000 glaciers in Alaska. However, the number of glaciers is a misleading statistic. Scientists are more interested in total glacial land coverage as a measure. The number of glaciers is less important since large ones can split up into several as they retreat. The amount of area glaciers occupy in Alaska is trending downward...
Based on the most recent comprehensive survey in 2011, there were about 27,000 glaciers in Alaska. However, the number of glaciers is a misleading statistic. Scientists are more interested in total glacial land coverage as a measure. The number of glaciers is less important since large ones can split up into several as they retreat. The amount of area glaciers occupy in Alaska is trending downward...
How much of the Earth's water is stored in glaciers?
About 2.1% of all of Earth's water is frozen in glaciers. 97.2% is in the oceans and inland seas 2.1% is in glaciers 0.6% is in groundwater and soil moisture less than 1% is in the atmosphere less than 1% is in lakes and rivers less than 1% is in all living plants and animals. About three-quarters of Earth's freshwater is stored in glaciers. Therefore, glacier ice is the second largest reservoir...
About 2.1% of all of Earth's water is frozen in glaciers. 97.2% is in the oceans and inland seas 2.1% is in glaciers 0.6% is in groundwater and soil moisture less than 1% is in the atmosphere less than 1% is in lakes and rivers less than 1% is in all living plants and animals. About three-quarters of Earth's freshwater is stored in glaciers. Therefore, glacier ice is the second largest reservoir...
How old is glacier ice?
The age of the oldest glacier ice in Antarctica may approach 1,000,000 years old The age of the oldest glacier ice in Greenland is more than 100,000 years old The age of the oldest Alaskan glacier ice ever recovered (from a basin between Mt. Bona and Mt. Churchill) is about 30,000 years old. Glacier flow moves newly formed ice through the entire length of a typical Alaskan valley glacier in 100...
The age of the oldest glacier ice in Antarctica may approach 1,000,000 years old The age of the oldest glacier ice in Greenland is more than 100,000 years old The age of the oldest Alaskan glacier ice ever recovered (from a basin between Mt. Bona and Mt. Churchill) is about 30,000 years old. Glacier flow moves newly formed ice through the entire length of a typical Alaskan valley glacier in 100...
Is glacier ice a type of rock?
Glacier ice, like limestone (for example), is a type of rock. Glacier ice is actually a mono-mineralic rock (a rock made of only one mineral, like limestone which is composed of the mineral calcite). The mineral ice is the crystalline form of water (H 2 O). Most glacier ice forms through the metamorphism of tens of thousands of individual snowflakes into crystals of glacier ice. Each snow flake is...
Glacier ice, like limestone (for example), is a type of rock. Glacier ice is actually a mono-mineralic rock (a rock made of only one mineral, like limestone which is composed of the mineral calcite). The mineral ice is the crystalline form of water (H 2 O). Most glacier ice forms through the metamorphism of tens of thousands of individual snowflakes into crystals of glacier ice. Each snow flake is...
Is there a size criterion for a glacier?
While there is no global standard for what size a body of ice must be to be considered a glacier, USGS scientists in Glacier National Park use the commonly accepted guideline of 0.1 square kilometers (about 25 acres) as the minimum size of a glacier. Below this size, ice is generally stagnant and does not have enough mass to move. Learn more: Status of Glaciers in Glacier National Park
While there is no global standard for what size a body of ice must be to be considered a glacier, USGS scientists in Glacier National Park use the commonly accepted guideline of 0.1 square kilometers (about 25 acres) as the minimum size of a glacier. Below this size, ice is generally stagnant and does not have enough mass to move. Learn more: Status of Glaciers in Glacier National Park
North America sites for Geologic Records of High Sea Levels
North America sites for Geologic Records of High Sea Levels
North America sites for Geologic Records of High Sea Levels
The distribution of water on, in, and above the Earth
The distribution of water on, in, and above the Earth
The distribution of water on, in, and above the Earth
The World's Water - Distribution of Earth's Water
The World's Water - Distribution of Earth's Water
PubTalk 9/2015 — Coral Reefs, Climate Change, and Atoll Sustainability
PubTalk 9/2015 — Coral Reefs, Climate Change, and Atoll Sustainability
PubTalk 9/2015 — Coral Reefs, Climate Change, and Atoll Sustainability
Will Micronesians become the U.S.'s first climate change refugees?
by Curt Storlazzi, USGS Research Geologist and Oceanographer
Will Micronesians become the U.S.'s first climate change refugees?
by Curt Storlazzi, USGS Research Geologist and Oceanographer
Cape Cod Sea Level Rise
U. S. Geological Survey Scientists Carol Johnson, Eric White and Tim McCobb prepare to deploy geophysical equipment in a coastal embayment April 9, 2015 in Falmouth, Massachusetts.
U. S. Geological Survey Scientists Carol Johnson, Eric White and Tim McCobb prepare to deploy geophysical equipment in a coastal embayment April 9, 2015 in Falmouth, Massachusetts.
Iceberg on Lake Superior
An iceberg floating in Lake Superior, June 2014. Photographed from the R/V Kiyi.
An iceberg floating in Lake Superior, June 2014. Photographed from the R/V Kiyi.
Wave-driven flooding and overwash on Roi-Namur Atoll
Wave-driven flooding and overwash on Roi-Namur Atoll
Wave-driven flooding and overwash on Roi-Namur Atoll
Wave-driven flooding and overwash on Roi-Namur Atoll, Republic of the Marshall Islands
Wave-driven flooding and overwash on Roi-Namur Atoll, Republic of the Marshall Islands
Wave-driven flooding and overwash on Roi-Namur Atoll
Wave-driven flooding and overwash on Roi-Namur Atoll
Wave-driven flooding and overwash on Roi-Namur Atoll
Wave-driven flooding and overwash on Roi-Namur Atoll, Republic of the Marshall Islands
Wave-driven flooding and overwash on Roi-Namur Atoll, Republic of the Marshall Islands
Impacts of Melting Glaciers on Gulf of Alaska
Impacts of Melting Glaciers on Gulf of Alaska
Impacts of Melting Glaciers on Gulf of Alaska
For questions about this project, please contact the speaker, John Crusius at jcrusius@usgs.gov, (206) 543-6978. The northern Gulf of Alaska (GoA) maintains a productive ecosystem, with commercially important fisheries.
By
For questions about this project, please contact the speaker, John Crusius at jcrusius@usgs.gov, (206) 543-6978. The northern Gulf of Alaska (GoA) maintains a productive ecosystem, with commercially important fisheries.
By
The Cold Facts About Melting Glaciers
Most glaciers in Washington and Alaska are dramatically shrinking in response to a warming climate.
Most glaciers in Washington and Alaska are dramatically shrinking in response to a warming climate.
Glacier 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,
Authors
Caitlyn Florentine
Land subsidence and relative sea-level rise in the southern Chesapeake Bay region
The southern Chesapeake Bay region is experiencing land subsidence and rising water levels due to global sea-level rise; land subsidence and rising water levels combine to cause relative sea-level rise. Land subsidence has been observed since the 1940s in the southern Chesapeake Bay region at rates of 1.1 to 4.8 millimeters per year (mm/yr), and subsidence continues today.This land subsidence he
Authors
Jack Eggleston, Jason Pope
Assessing hazards along our Nation's coasts
Coastal areas are essential to the economic, cultural, and environmental health of the Nation, yet by nature coastal areas are constantly changing due to a variety of events and processes. Extreme storms can cause dramatic changes to our shorelines in a matter of hours, while sea-level rise can profoundly alter coastal environments over decades. These changes can have a devastating impact on coast
Authors
Hilary F. Stockdon, Cheryl J. Hapke, E. Robert Thieler, Nathaniel G. Plant
U.S. Geological Survey Climate and Land Use Change Science Strategy—A Framework for Understanding and Responding to Global Change
Executive SummaryThe U.S. Geological Survey (USGS), a nonregulatory Federal science agency with national scope and responsibilities, is uniquely positioned to serve the Nation’s needs in understanding and responding to global change, including changes in climate, water availability, sea level, land use and land cover, ecosystems, and global biogeochemical cycles. Global change is among the most ch
Authors
Virginia R. Burkett, David A. Kirtland, Ione L. Taylor, Jayne Belnap, Thomas M. Cronin, Michael D. Dettinger, Eldrich L. Frazier, John W. Haines, Thomas R. Loveland, Paul C.D. Milly, Robin O'Malley, Robert S. Thompson, Alec G. Maule, Gerard McMahon, Robert G. Striegl
The United States National Climate Assessment - Alaska Technical Regional Report
The Alaskan landscape is changing, both in terms of effects of human activities as a consequence of increased population, social and economic development and their effects on the local and broad landscape; and those effects that accompany naturally occurring hazards such as volcanic eruptions, earthquakes, and tsunamis. Some of the most prevalent changes, however, are those resulting from a changi
Authors
Carl J. Markon, Sarah F. Trainor, F. Stuart Chapin
State of the Earth’s cryosphere at the beginning of the 21st century : glaciers, global snow cover, floating ice, and permafrost and periglacial environments: Chapter A in Satellite image atlas of glaciers of the world
This chapter is the tenth in a series of 11 book-length chapters, collectively referred to as “this volume,” in the series U.S. Geological Survey Professional Paper 1386, Satellite Image Atlas of Glaciers of the World. In the other 10 chapters, each of which concerns a specific glacierized region of Earth, the authors used remotely sensed images, primarily from the Landsat 1, 2, and 3 series of sp
Authors
Richard S. Williams, Jane G. Ferrigno
USGS science for the Nation's changing coasts; shoreline change assessment
The coastline of the United States features some of the most popular tourist and recreational destinations in the world and is the site of intense residential, commercial, and industrial development. The coastal zone also has extensive and pristine natural areas, with diverse ecosystems providing essential habitat and resources that support wildlife, fish, and human use. Coastal erosion is a wides
Authors
E. Robert Thieler, Cheryl J. Hapke
Coastal change along the shore of northeastern South Carolina— The South Carolina Coastal Erosion Study
The U.S. Geological Survey, in cooperation with the South Carolina Sea Grant Consortium, conducted a 7-year, multidisciplinary study of coastal erosion in northeastern South Carolina. Shoreline behavior along the coast of Long Bay is dictated by waves, tidal currents, and sediment supply that act within the overall constraints of the regional geologic setting. Beaches are thin ribbons of sand that
Authors
W. C. Schwab, P. T. Gayes, R.A. Morton, N. W. Driscoll, W. E. Baldwin, W. A. Barnhardt, J. F. Denny, M.S. Harris, M.P. Katuna, T.R. Putney, G. Voulgaris, J.C. Warner, E.E. Wright
Fifty-year record of glacier change reveals shifting climate in the Pacific Northwest and Alaska, USA
Fifty years of U.S. Geological Survey (USGS) research on glacier change shows recent dramatic shrinkage of glaciers in three climatic regions of the United States. These long periods of record provide clues to the climate shifts that may be driving glacier change. The USGS Benchmark Glacier Program began in 1957 as a result of research efforts during the International Geophysical Year (Meier a
Authors
A strategy for monitoring glaciers
Glaciers are important features in the hydrologic cycle and affect the volume, variability, and water quality of runoff. Assessing and predicting the effect of glaciers on water resources require a monitoring program to provide basic data for this understanding. The monitoring program of the U.S. Geological Survey employs a nested approach whereby an intensively studied glacier is surrounded by le
Authors
Andrew G. Fountain, Robert M. Krimmel, Dennis C. Trabant
Sea level change: lessons from the geologic record
Rising sea level is potentially one of the most serious impacts of climatic change. Even a small sea level rise would have serious economic consequences because it would cause extensive damage to the world's coastal regions. Sea level can rise in the future because the ocean surface can expand due to warming and because polar ice sheets and mountain glaciers can melt, increasing the ocean
Authors
Glaciers: A water resource
Most Americans have never seen a glacier, and most would say that glaciers are rare features found only in inaccessible, isolated wilderness mountains. Are they really so rare? Or are they really potentially important sources of water supply?
Authors
Mark Meier, Austin Post
New US Geological Survey-led Research Helps California Coastal Managers Prioritize Planning and Mitigation Efforts Due to Rising Seas and Storms
New U.S. Geological Survey-led coastal modeling research presents state, federal, and commercial entities with varying storm and sea level-rise...
Glaciers Rapidly Shrinking and Disappearing: 50 Years of Glacier Change in Montana
Glaciers Rapidly Shrinking and Disappearing: 50 Years of Glacier Change in Montana
The warming climate has dramatically reduced the size of 39 glaciers in Montana since 1966, some by as much as 85 percent, according to data released...
Rising Sea Levels, Coastal Development’s Effect on Gulf Coast Wetlands
Rising Sea Levels, Coastal Development’s Effect on Gulf Coast Wetlands
As coastal development along the Gulf Coastcontinuesto expand, tidal saline wetlands could have difficulty adjusting to rising sea levels.
Sea Level Rise and Storm Wave Flooding Threaten Seabirds
Sea Level Rise and Storm Wave Flooding Threaten Seabirds
Islands used by tropical seabirds are highly vulnerable to sea level rise according to a new study released today.
Study Shows Sea Level Rise to Threaten West Coast Tidal Wetlands Over the Next 100 Years
Study Shows Sea Level Rise to Threaten West Coast Tidal Wetlands Over the Next 100 Years
The U.S. Geological Survey and Oregon State University released a report this week examining Pacific Northwest tidal wetland vulnerability to sea...
From Icefield to Ocean - What Glacier Change Might Mean for the Future of Alaska
From Icefield to Ocean - What Glacier Change Might Mean for the Future of Alaska
Frozen bodies of ice cover nearly 10 percent of the state of Alaska, but the influence of glaciers on the environment, tourism, fisheries, hydropower...
Related Content
- FAQ
What are the impacts of glacier loss, other than losing an aesthetic landscape feature?
Glaciers act as reservoirs of water that persist through summer. Continual melt from glaciers contributes water to the ecosystem throughout dry months, creating perennial stream habitat and a water source for plants and animals. The cold runoff from glaciers also affects downstream water temperatures. Many aquatic species in mountainous environments require cold water temperatures to survive. Some...
Glaciers act as reservoirs of water that persist through summer. Continual melt from glaciers contributes water to the ecosystem throughout dry months, creating perennial stream habitat and a water source for plants and animals. The cold runoff from glaciers also affects downstream water temperatures. Many aquatic species in mountainous environments require cold water temperatures to survive. Some...
Are today's glaciers leftovers from the Pleistocene ice age?
Yes and no. It depends on which glaciers you are considering. Parts of the Antarctic Continent have had continuous glacier cover for perhaps as long as 20 million years. Other areas, such as valley glaciers of the Antarctic Peninsula and glaciers of the Transantarctic Mountains may date from the early Pleistocene. For Greenland, ice cores and related data suggest that all of southern Greenland and...
Yes and no. It depends on which glaciers you are considering. Parts of the Antarctic Continent have had continuous glacier cover for perhaps as long as 20 million years. Other areas, such as valley glaciers of the Antarctic Peninsula and glaciers of the Transantarctic Mountains may date from the early Pleistocene. For Greenland, ice cores and related data suggest that all of southern Greenland and...
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...
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...
How does present glacier extent and sea level compare to the extent of glaciers and global sea level during the Last Glacial Maximum (LGM)?
The Last Glacial Maximum (LGM) occurred about 20,000 years ago, during the last phase of the Pleistocene epoch. At that time, global sea level was more than 400 feet lower than it is today, and glaciers covered approximately: 8% of Earth’s surface 25% of Earth’s land area 33% of Alaska Beginning about 15,000 years ago, continental glaciers retreated and sea level began to rise. Sea level reached...
How does present glacier extent and sea level compare to the extent of glaciers and global sea level during the Last Glacial Maximum (LGM)?
The Last Glacial Maximum (LGM) occurred about 20,000 years ago, during the last phase of the Pleistocene epoch. At that time, global sea level was more than 400 feet lower than it is today, and glaciers covered approximately: 8% of Earth’s surface 25% of Earth’s land area 33% of Alaska Beginning about 15,000 years ago, continental glaciers retreated and sea level began to rise. Sea level reached...
How many glaciers currently exist in Alaska?
Based on the most recent comprehensive survey in 2011, there were about 27,000 glaciers in Alaska. However, the number of glaciers is a misleading statistic. Scientists are more interested in total glacial land coverage as a measure. The number of glaciers is less important since large ones can split up into several as they retreat. The amount of area glaciers occupy in Alaska is trending downward...
Based on the most recent comprehensive survey in 2011, there were about 27,000 glaciers in Alaska. However, the number of glaciers is a misleading statistic. Scientists are more interested in total glacial land coverage as a measure. The number of glaciers is less important since large ones can split up into several as they retreat. The amount of area glaciers occupy in Alaska is trending downward...
How much of the Earth's water is stored in glaciers?
About 2.1% of all of Earth's water is frozen in glaciers. 97.2% is in the oceans and inland seas 2.1% is in glaciers 0.6% is in groundwater and soil moisture less than 1% is in the atmosphere less than 1% is in lakes and rivers less than 1% is in all living plants and animals. About three-quarters of Earth's freshwater is stored in glaciers. Therefore, glacier ice is the second largest reservoir...
About 2.1% of all of Earth's water is frozen in glaciers. 97.2% is in the oceans and inland seas 2.1% is in glaciers 0.6% is in groundwater and soil moisture less than 1% is in the atmosphere less than 1% is in lakes and rivers less than 1% is in all living plants and animals. About three-quarters of Earth's freshwater is stored in glaciers. Therefore, glacier ice is the second largest reservoir...
How old is glacier ice?
The age of the oldest glacier ice in Antarctica may approach 1,000,000 years old The age of the oldest glacier ice in Greenland is more than 100,000 years old The age of the oldest Alaskan glacier ice ever recovered (from a basin between Mt. Bona and Mt. Churchill) is about 30,000 years old. Glacier flow moves newly formed ice through the entire length of a typical Alaskan valley glacier in 100...
The age of the oldest glacier ice in Antarctica may approach 1,000,000 years old The age of the oldest glacier ice in Greenland is more than 100,000 years old The age of the oldest Alaskan glacier ice ever recovered (from a basin between Mt. Bona and Mt. Churchill) is about 30,000 years old. Glacier flow moves newly formed ice through the entire length of a typical Alaskan valley glacier in 100...
Is glacier ice a type of rock?
Glacier ice, like limestone (for example), is a type of rock. Glacier ice is actually a mono-mineralic rock (a rock made of only one mineral, like limestone which is composed of the mineral calcite). The mineral ice is the crystalline form of water (H 2 O). Most glacier ice forms through the metamorphism of tens of thousands of individual snowflakes into crystals of glacier ice. Each snow flake is...
Glacier ice, like limestone (for example), is a type of rock. Glacier ice is actually a mono-mineralic rock (a rock made of only one mineral, like limestone which is composed of the mineral calcite). The mineral ice is the crystalline form of water (H 2 O). Most glacier ice forms through the metamorphism of tens of thousands of individual snowflakes into crystals of glacier ice. Each snow flake is...
Is there a size criterion for a glacier?
While there is no global standard for what size a body of ice must be to be considered a glacier, USGS scientists in Glacier National Park use the commonly accepted guideline of 0.1 square kilometers (about 25 acres) as the minimum size of a glacier. Below this size, ice is generally stagnant and does not have enough mass to move. Learn more: Status of Glaciers in Glacier National Park
While there is no global standard for what size a body of ice must be to be considered a glacier, USGS scientists in Glacier National Park use the commonly accepted guideline of 0.1 square kilometers (about 25 acres) as the minimum size of a glacier. Below this size, ice is generally stagnant and does not have enough mass to move. Learn more: Status of Glaciers in Glacier National Park
- Multimedia
North America sites for Geologic Records of High Sea LevelsNorth America sites for Geologic Records of High Sea Levels
North America sites for Geologic Records of High Sea Levels
The distribution of water on, in, and above the Earth
The distribution of water on, in, and above the Earth
The distribution of water on, in, and above the Earth
The World's Water - Distribution of Earth's Water
The World's Water - Distribution of Earth's Water
PubTalk 9/2015 — Coral Reefs, Climate Change, and Atoll SustainabilityPubTalk 9/2015 — Coral Reefs, Climate Change, and Atoll Sustainability
PubTalk 9/2015 — Coral Reefs, Climate Change, and Atoll Sustainability
Will Micronesians become the U.S.'s first climate change refugees?
by Curt Storlazzi, USGS Research Geologist and Oceanographer
Will Micronesians become the U.S.'s first climate change refugees?
by Curt Storlazzi, USGS Research Geologist and Oceanographer
Cape Cod Sea Level Rise
U. S. Geological Survey Scientists Carol Johnson, Eric White and Tim McCobb prepare to deploy geophysical equipment in a coastal embayment April 9, 2015 in Falmouth, Massachusetts.
U. S. Geological Survey Scientists Carol Johnson, Eric White and Tim McCobb prepare to deploy geophysical equipment in a coastal embayment April 9, 2015 in Falmouth, Massachusetts.
Iceberg on Lake Superior
An iceberg floating in Lake Superior, June 2014. Photographed from the R/V Kiyi.
An iceberg floating in Lake Superior, June 2014. Photographed from the R/V Kiyi.
Wave-driven flooding and overwash on Roi-Namur Atoll
Wave-driven flooding and overwash on Roi-Namur Atoll
Wave-driven flooding and overwash on Roi-Namur Atoll
Wave-driven flooding and overwash on Roi-Namur Atoll, Republic of the Marshall Islands
Wave-driven flooding and overwash on Roi-Namur Atoll, Republic of the Marshall Islands
Wave-driven flooding and overwash on Roi-Namur Atoll
Wave-driven flooding and overwash on Roi-Namur Atoll
Wave-driven flooding and overwash on Roi-Namur Atoll
Wave-driven flooding and overwash on Roi-Namur Atoll, Republic of the Marshall Islands
Wave-driven flooding and overwash on Roi-Namur Atoll, Republic of the Marshall Islands
Impacts of Melting Glaciers on Gulf of AlaskaImpacts of Melting Glaciers on Gulf of Alaska
Impacts of Melting Glaciers on Gulf of Alaska
For questions about this project, please contact the speaker, John Crusius at jcrusius@usgs.gov, (206) 543-6978. The northern Gulf of Alaska (GoA) maintains a productive ecosystem, with commercially important fisheries.
By
For questions about this project, please contact the speaker, John Crusius at jcrusius@usgs.gov, (206) 543-6978. The northern Gulf of Alaska (GoA) maintains a productive ecosystem, with commercially important fisheries.
By
The Cold Facts About Melting Glaciers
Most glaciers in Washington and Alaska are dramatically shrinking in response to a warming climate.
Most glaciers in Washington and Alaska are dramatically shrinking in response to a warming climate.
- Publications
Glacier 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,
Authors
Caitlyn Florentine
Land subsidence and relative sea-level rise in the southern Chesapeake Bay region
The southern Chesapeake Bay region is experiencing land subsidence and rising water levels due to global sea-level rise; land subsidence and rising water levels combine to cause relative sea-level rise. Land subsidence has been observed since the 1940s in the southern Chesapeake Bay region at rates of 1.1 to 4.8 millimeters per year (mm/yr), and subsidence continues today.This land subsidence he
Authors
Jack Eggleston, Jason Pope
Assessing hazards along our Nation's coasts
Coastal areas are essential to the economic, cultural, and environmental health of the Nation, yet by nature coastal areas are constantly changing due to a variety of events and processes. Extreme storms can cause dramatic changes to our shorelines in a matter of hours, while sea-level rise can profoundly alter coastal environments over decades. These changes can have a devastating impact on coast
Authors
Hilary F. Stockdon, Cheryl J. Hapke, E. Robert Thieler, Nathaniel G. Plant
U.S. Geological Survey Climate and Land Use Change Science Strategy—A Framework for Understanding and Responding to Global Change
Executive SummaryThe U.S. Geological Survey (USGS), a nonregulatory Federal science agency with national scope and responsibilities, is uniquely positioned to serve the Nation’s needs in understanding and responding to global change, including changes in climate, water availability, sea level, land use and land cover, ecosystems, and global biogeochemical cycles. Global change is among the most ch
Authors
Virginia R. Burkett, David A. Kirtland, Ione L. Taylor, Jayne Belnap, Thomas M. Cronin, Michael D. Dettinger, Eldrich L. Frazier, John W. Haines, Thomas R. Loveland, Paul C.D. Milly, Robin O'Malley, Robert S. Thompson, Alec G. Maule, Gerard McMahon, Robert G. Striegl
The United States National Climate Assessment - Alaska Technical Regional Report
The Alaskan landscape is changing, both in terms of effects of human activities as a consequence of increased population, social and economic development and their effects on the local and broad landscape; and those effects that accompany naturally occurring hazards such as volcanic eruptions, earthquakes, and tsunamis. Some of the most prevalent changes, however, are those resulting from a changi
Authors
Carl J. Markon, Sarah F. Trainor, F. Stuart Chapin
State of the Earth’s cryosphere at the beginning of the 21st century : glaciers, global snow cover, floating ice, and permafrost and periglacial environments: Chapter A in Satellite image atlas of glaciers of the world
This chapter is the tenth in a series of 11 book-length chapters, collectively referred to as “this volume,” in the series U.S. Geological Survey Professional Paper 1386, Satellite Image Atlas of Glaciers of the World. In the other 10 chapters, each of which concerns a specific glacierized region of Earth, the authors used remotely sensed images, primarily from the Landsat 1, 2, and 3 series of sp
Authors
Richard S. Williams, Jane G. Ferrigno
USGS science for the Nation's changing coasts; shoreline change assessment
The coastline of the United States features some of the most popular tourist and recreational destinations in the world and is the site of intense residential, commercial, and industrial development. The coastal zone also has extensive and pristine natural areas, with diverse ecosystems providing essential habitat and resources that support wildlife, fish, and human use. Coastal erosion is a wides
Authors
E. Robert Thieler, Cheryl J. Hapke
Coastal change along the shore of northeastern South Carolina— The South Carolina Coastal Erosion Study
The U.S. Geological Survey, in cooperation with the South Carolina Sea Grant Consortium, conducted a 7-year, multidisciplinary study of coastal erosion in northeastern South Carolina. Shoreline behavior along the coast of Long Bay is dictated by waves, tidal currents, and sediment supply that act within the overall constraints of the regional geologic setting. Beaches are thin ribbons of sand that
Authors
W. C. Schwab, P. T. Gayes, R.A. Morton, N. W. Driscoll, W. E. Baldwin, W. A. Barnhardt, J. F. Denny, M.S. Harris, M.P. Katuna, T.R. Putney, G. Voulgaris, J.C. Warner, E.E. Wright
Fifty-year record of glacier change reveals shifting climate in the Pacific Northwest and Alaska, USA
Fifty years of U.S. Geological Survey (USGS) research on glacier change shows recent dramatic shrinkage of glaciers in three climatic regions of the United States. These long periods of record provide clues to the climate shifts that may be driving glacier change. The USGS Benchmark Glacier Program began in 1957 as a result of research efforts during the International Geophysical Year (Meier a
Authors
A strategy for monitoring glaciers
Glaciers are important features in the hydrologic cycle and affect the volume, variability, and water quality of runoff. Assessing and predicting the effect of glaciers on water resources require a monitoring program to provide basic data for this understanding. The monitoring program of the U.S. Geological Survey employs a nested approach whereby an intensively studied glacier is surrounded by le
Authors
Andrew G. Fountain, Robert M. Krimmel, Dennis C. Trabant
Sea level change: lessons from the geologic record
Rising sea level is potentially one of the most serious impacts of climatic change. Even a small sea level rise would have serious economic consequences because it would cause extensive damage to the world's coastal regions. Sea level can rise in the future because the ocean surface can expand due to warming and because polar ice sheets and mountain glaciers can melt, increasing the ocean
Authors
Glaciers: A water resource
Most Americans have never seen a glacier, and most would say that glaciers are rare features found only in inaccessible, isolated wilderness mountains. Are they really so rare? Or are they really potentially important sources of water supply?
Authors
Mark Meier, Austin Post
- News
New US Geological Survey-led Research Helps California Coastal Managers Prioritize Planning and Mitigation Efforts Due to Rising Seas and Storms
New U.S. Geological Survey-led coastal modeling research presents state, federal, and commercial entities with varying storm and sea level-rise...
Glaciers Rapidly Shrinking and Disappearing: 50 Years of Glacier Change in Montana
Glaciers Rapidly Shrinking and Disappearing: 50 Years of Glacier Change in Montana
The warming climate has dramatically reduced the size of 39 glaciers in Montana since 1966, some by as much as 85 percent, according to data released...
Rising Sea Levels, Coastal Development’s Effect on Gulf Coast Wetlands
Rising Sea Levels, Coastal Development’s Effect on Gulf Coast Wetlands
As coastal development along the Gulf Coastcontinuesto expand, tidal saline wetlands could have difficulty adjusting to rising sea levels.
Sea Level Rise and Storm Wave Flooding Threaten Seabirds
Sea Level Rise and Storm Wave Flooding Threaten Seabirds
Islands used by tropical seabirds are highly vulnerable to sea level rise according to a new study released today.
Study Shows Sea Level Rise to Threaten West Coast Tidal Wetlands Over the Next 100 Years
Study Shows Sea Level Rise to Threaten West Coast Tidal Wetlands Over the Next 100 Years
The U.S. Geological Survey and Oregon State University released a report this week examining Pacific Northwest tidal wetland vulnerability to sea...
From Icefield to Ocean - What Glacier Change Might Mean for the Future of Alaska
From Icefield to Ocean - What Glacier Change Might Mean for the Future of Alaska
Frozen bodies of ice cover nearly 10 percent of the state of Alaska, but the influence of glaciers on the environment, tourism, fisheries, hydropower...
