The glacier has reached the midpoint of its projected retreat, with a shrinking length of 9 miles since 1980. The glacier's rapid retreat is attributed to complex physical processes and warming trends, resulting in an annual discharge of nearly 2 cubic miles of ice into the Prince William Sound.
The Mosaic map reveals subtle changes in terrain that indicate the direction ice is flowing now and where it has gone in the past. The digital elevation model complements this view with elevation measurements over more of the continent than ever surveyed before, yielding new information about how topography drives ice flow.
A Scripps-led study finds that climate warming will shrink key water supplies around the world, affecting millions. Glacier-dependent regions like China, India, and parts of South America are particularly vulnerable to vanishing glaciers, which will lead to costly disruptions in water supply and resource management systems.
Scientists studying the Helheim glacier in Greenland found it has sped up from 70 feet per day to nearly 110 feet per day, thinning by over 130 feet since 2001. This accelerated melting could have dramatic implications for climate models and increase sea level rise.
Researchers warn that the breakdown of major ice sheets in Greenland and Antarctica could significantly speed up sea level rise, potentially doubling current projections. The study suggests that these mechanisms should be carefully considered in future climate models to ensure accurate sea level rise predictions.
New research reveals that Mars' mid-latitude glaciers are similar to those on Earth, with features such as lineated valley fill and debris arcs. The findings suggest that Mars is experiencing ongoing climate shifts, allowing ice to leave the poles and accumulate at lower latitudes.
A University of Colorado study found that freeze-dried microbial mats in an Antarctic streambed revived quickly after water was reintroduced, demonstrating the persistence and adaptability of life in extreme environments. The research, led by Professor Diane McKnight, sheds light on the resilience of microorganisms in polar ecosystems.
Researchers found that small glaciers in Northern California are remaining stable due to higher precipitation rates. This anomaly highlights the need for further study on glacier behavior and provides insight into climate variability over thousands of years.
New research models long-term climate cycles like El Nino, finds molten rock makes big earthquakes bigger, and sheds light on Yellowstone's volcanic activity. A computer simulation produced El Nino-like climate cycles, while another study found that melted rock accelerates plate movement during earthquakes.
The Antarctic Peninsula glaciers have been in widespread retreat over the past 50 years, with most glaciers shrinking rapidly. However, 32 glaciers are showing minor advance. The study suggests that warming is the key cause of this change.
A new study found that 87% of the 244 marine glaciers have retreated over the last 50 years, with the trend moving southward from the warmer northern tip of the peninsula. The glacier retreat is linked to atmospheric temperature increases, and may affect sea level rise if ice shelves continue to break up.
A study by Woods Hole Oceanographic Institution researchers finds that variations in the Earth's axis tilt control the timing of glaciations, acting as a planetary pacemaker. The researchers developed a simple model to analyze the effects of changes in tilt on climate belts and seasons.
Scientists analyze Mars Express images to find evidence of ancient glaciers, including flow features and glacial moraines. The study suggests a significant climate change on Mars within the last million years, which could be caused by a shift in the polar axis.
Recent Martian glaciers and volcanoes suggest ice-rich movement and climate change, with evidence of a major eruption over 350,000 years ago. This new research challenges the traditional view of Mars' geological history and provides fresh insights into the planet's dynamic evolution.
Researchers have found that Canada's Arctic ice caps and glaciers are thinning at lower elevations due to increased melting. The study suggests that these changes contribute significantly to global sea level rise, with an estimated 0.065 millimeters per year added to sea levels during the 1995-2000 period.
Research suggests Arctic sea ice is shrinking, contradicting current climate models. Mountain glaciers are also losing mass due to temperature changes, raising concerns about sea level rise.
Researchers measured ancient moraine crests to determine past movement on the Karakorum fault, revealing a significant right-lateral motion. The study's findings provide crucial insights into the Asian continent's movement and the collision of India and Asia.
A catastrophic flood from ancient Glacial Lake Iroquois may have triggered the Intra-Allerod Cold Period and the Younger Dryas cold climate event. The team analyzed sediment cores, walrus fossils, and pollen to precisely date the discharge of freshwater into the North Atlantic.
Research at Ohio State University suggests that global climate changed dramatically 5,200 years ago, with severe impacts on emerging cultures. The team found evidence of sudden and severe climate shifts in ice cores, tree rings, and plant pollen records from around the world.
Researchers found plant samples dating back at least 50,000 years, suggesting the ice cap's current size may not have changed in that time. The discovery implies a possible decrease in global climate change over the past 50,000 years.
Scientists have found significant acceleration in the world's fastest glacier, Jakobshavn Isbrae, which nearly doubled its discharge of ice between 1997 and 2003. Meanwhile, Arctic sea ice has been declining at an alarming rate, with some areas experiencing 9.2% per decade decline.
A research team has found evidence of microbes living in a rock glacier for the first time, challenging previous assumptions about these environments. The discovery was made in Colorado and is similar to recent findings in Antarctica, where scientists had previously discovered life in inhospitable regions.
Scientists are using NASA's ICESat satellite to measure the height of dynamic features such as ice sheets, glaciers, forests, and clouds. The satellite's laser instruments provide unprecedented accuracy in measuring changes in elevation, including accelerated glacier movement in Antarctica and thinner ice on West Antarctic ice sheet.
Researchers found sharks can detect geomagnetic field changes, which may aid navigation. This discovery builds upon previous studies on bird navigation.
A University of Colorado at Boulder research team has discovered evidence of microbial activity in a rock glacier, a barren environment previously thought to be devoid of life. The discovery includes traces of dissolved organic material and high levels of nitrates, suggesting microbes metabolize nitrogen within the glacier.
Researchers observed a sudden speed-up of the Jakobshavn Isbrae glacier, coinciding with rapid thinning of up to 15 meters per year after 1997. The acceleration in ice flow has significant implications for sea level rise, with this one glacier contributing roughly 4% of the 20th century rate.
Researchers have made significant discoveries about the impact of human activities on the environment. A new study used satellite observations to estimate nitrogen oxide emissions from ships, which contribute approximately 23 gigagrams per year into the troposphere. Additionally, a seismic analysis technique has provided unprecedented ...
Satellite data shows Antarctic glaciers speeding up by up to five times their previous speed after the Larsen B ice shelf collapse. This acceleration is linked to climate warming and could have significant effects on sea-level rise.
Researchers found that ice shelf collapses in the Antarctic Peninsula can cause nearby glaciers to accelerate by up to eight times, leading to rapid elevations drops and increased sea level rise. The study provides clear evidence of the relationship between ice shelf breakdown and accelerated glacier flow.
A recent NASA study has found a significant correlation between the retreat of glaciers and an increase in earthquake activity in southern Alaska. As glaciers melt, they lighten the load on the Earth's crust, allowing tectonic plates to move more freely, which can lead to earthquakes.
Researchers found that eastern chipmunks in Illinois and Wisconsin descend from ancestors who survived the last North American ice age in isolated forest pockets. These chipmunks migrated south, merging with warmer east and south populations, challenging long-held assumptions about glacier-driven population migrations.
Researchers discover tiny microbes in ancient Greenland glacier that are smaller than common bacteria and can survive extreme conditions. These ultra-small cells have been found to be among the uncultured majority of microbes on Earth and hold secrets to their survival mechanisms.
Scientists have found microscopic life in ancient glacier ice, sparking interest in survival mechanisms of small cells under harsh conditions. The discovery opens up new avenues for research into growing previously unculturable organisms and understanding the limits of microbial life.
Researchers found that glaciers grind down mountains at a rate comparable to tectonic plate movement, validating the 'glacial buzz saw' hypothesis. This suggests that glacial erosion plays a significant role in shaping mountain landscapes and redistributing rock masses.
Researchers using GPS satellites have discovered a pattern of land movement across North America, with Canadian sites rising and US sites south of the Great Lakes sinking. This post-glacial rebound affects not only industries but also international water management.
A team of geologists has discovered evidence of at least three Cryogenian glaciations, with ages estimated to be around 663 million years ago. The new findings confirm a previously hypothesized 'snowball Earth' scenario and suggest significant climate changes may have led to extinctions.
Scientists from UW-Madison used a new technique to precisely date glacial deposits, revealing that the last two major glaciations were global events. The findings suggest that rapid cooling of the Earth's atmosphere synchronized climate change worldwide during each ice age.
The Jakobshavn Glacier, one of Greenland's major drainage outlets, has been found to be accelerating and retreating rapidly. Glacial scientists have discovered that the glacier is now flowing at speeds of up to 9 kilometers per year, with ice thinning rates reaching an alarming 12 meters per year.
Researchers hope that ice cores and ancient plants retrieved from glaciers in the Peruvian Andes may contain clues about a mysterious global climate change that occurred over 5,000 years ago. The cores are expected to provide a critical piece of the puzzle needed to understand climate variability in the region.
Researchers discovered a unique amphibian species, developed new methods for dating hillside erosion, and analyzed trace elements to recreate ancient environments. The team also created a new tool for analyzing basalts and found evidence of ancient volcanoes in Austria's Alps.
Researchers from Ohio State University discovered that Blood Falls is the last remnant of an ancient salt-water lake, formed when sea levels were higher. The lake probably existed 5 million years ago, and its remains are being slowly pushed out by the glacier.
Researchers found a clear association between ocean tides and ice stream motion in West Antarctica. The study discovered that a one-meter tide variation can cause an ice stream to halt and then accelerate rapidly.
Scientists have discovered that 'warm' glaciers can use supercooling to trap and transport silt, providing new insights into glacier dynamics. The process involves the formation of 'frazil ice,' which picks up particles from the surrounding water, creating layers of clean and dirty ice.
Researchers at Michigan State University discover that glaciers sculpt and erode landscapes through a phenomenon called glaciohydraulic supercooling, which affects the rate of erosion. This new understanding allows for better comprehension of how glaciers subdue mountains.
Researchers discovered that glacial erosion is controlled by the relationships of the ground beneath the glacier, the rubble pile, and the glacier itself. Glaciers achieve a steady state existence when the angle between their toe and sediment pile becomes too steep, causing streams to stop flowing and erosion to cease.
The study aims to analyze satellite imagery to create a new baseline of current glacier conditions for comparison with historical measurements. Researchers will focus on two regions: central Asia and southern Alaska, where glaciers have experienced unprecedented ice loss, affecting freshwater sources and regional ecosystems.
A recent UC Riverside study shows that glaciers once existed in the southernmost region of North America, as recently as 5,000-10,000 years ago. This finding has implications for understanding past climate change and testing the validity of computer models predicting future climate change.
The USGS collaborated with Alpha DVD to produce a comprehensive educational DVD about Alaska's glaciers. The DVD covers glacier characteristics, climate history, and ecosystems, providing a detailed introduction to this natural process.
Researchers collected and analyzed a record-breaking ice core in the St. Elias range, providing insights into the North Pacific Decadal Oscillation (PDO). The PDO is a 20-30 year climate cycle affecting weather across North America, with cool and warm phases centered in the North Pacific.
Researchers discovered a steady decline in the West Antarctic ice sheet over the past few thousand years, raising concerns about its future behavior. The ice sheet contains enough water to raise global sea level by 5 meters, threatening coastal regions with disastrous consequences.
A 7.9 magnitude earthquake on Alaska's Denali fault system created a 145-mile scar across the landscape, with measurable offsets of up to 22 feet. The earthquake revealed new surface ruptures, clearly developed scarps and cracks where faults pass beneath glaciers.
The study found three catastrophic droughts in Africa 8,300, 5,200, and 4,000 years ago, which coincided with the formation of cities and social structures. The ice cores also showed a significant decline in oxygen-18 isotopes, indicating another severe drought event around 5,200 years ago.
UMass geoscientists are part of a team studying the retreat of Kilimanjaro's glaciers, using continuous data from a mountaintop weather station and monitoring the glaciers. The researchers found an 80% decrease in glacier area between 1912 and the end of the 20th century.
A team of researchers led by Hongxing Liu from Texas A&M University is analyzing remotely sensed data from the Lambert ice sheet to understand its role in global climate change. The study will help determine how glaciers respond to changes in the climate and provide clues about the potential impact on sea levels.
New studies reveal close connections between North Atlantic and Pacific climates, with potential implications for predicting future climate changes. Glacier advances in Alaska and landslides triggered by asteroid impacts provide evidence of distant climate perturbations.
Researchers have calculated that Alaska glaciers contribute significantly to global sea-level rise, with most glaciers losing mass over the past four decades. The study found that Alaska's glaciers raise the level of Earth's oceans by more than one-tenth of a millimeter each year.
Researchers studied Paleocene-Eocene syncontractional sedimentation in east-central Tibet, numerical modeling of fluid flow in Utah, and syndepositional thrust-related deformation in a Central Colorado trough. The findings provide insights into the geological evolution of these regions.
Scientists warn of significant global impacts from glacier decline, with effects on agriculture, water supplies, and ecosystems. Glacier melting may lead to both serious problems and short-term increases in water availability.
Lonnie G. Thompson, a leading researcher in ice core analysis, will receive the $150,000 Heineken award for his pioneering work on climate change. His research has provided critical insights into the effects of human activity on the Earth's climate.
An ice coring team led by Ohio State University's Lonnie Thompson aims to drill through Alaska's glaciers to retrieve ancient weather records. The expedition hopes to determine if recent climate change is part of a natural cycle or caused by human activity, with potential implications for global warming.