Articles tagged with Glaciers
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A team of researchers found that glaciers in the region advanced due to cooler temperatures created by increased cloud cover and reduced evaporation. The study provides valuable insights into how glaciers respond to climate change, enabling better forecasting of water supply changes in the coming decades.
The Pine Island Glacier in West Antarctica is losing ice four times as fast as it was a decade ago, with scientists estimating that the main section of the glacier will disappear in just 100 years. The glacier's acceleration is attributed to warming oceans and has significant implications for global sea level rise.
Scientists from British Antarctic Survey and University of Durham describe a new 3D map created from radar measurements, revealing features in the landscape beneath a vast river of ice. The study provides insight into how ice streams behave and how they might change in the future.
A study of a prehistoric Canadian Arctic glacier found it rapidly retreated in just a few hundred years, demonstrating the phenomenon's occurrence. This rapid retreat could lead to sharply rising global sea levels and threaten coastal populations if similar conditions recur today.
Researchers found evidence of a massive 4,500-year-old drought in Africa and Asia, as well as a rapid 5,200-year-old cooling event that accelerated tropical glacier growth. The findings suggest that similar changes are currently occurring globally.
Scientists capture the most comprehensive set of sonar images of Antarctica's seafloor around the Amundsen Sea embayment, providing new insights into past ice flow and potential future sea-level rise. The findings indicate that the controlling mechanisms of the Antarctic ice sheet are more complex than previously thought.
A new study reveals that glaciers in New Zealand's Southern Alps have fluctuated frequently over the past 7,000 years, with some advances and declines not seen in the Northern Hemisphere. The research uses a refined method to date young moraines, allowing for more accurate reconstructions of glacial advances worldwide.
A new study using cosmogenic dating reveals that New Zealand's largest glaciers moved out of step with their northern hemisphere counterparts for the past 7,000 years. The research provides a glacial timeline and shows regional climate variations in both hemispheres.
Microbes adapted to manipulate sulfur and iron compounds to survive in the absence of photosynthesis. The discovery provides insights into the origins of life on Earth and offers a unique laboratory for studying life in hostile environments.
Researchers at Harvard University and Dartmouth College discovered hardy microbes living in isolation beneath an Antarctic glacier. The microbes, similar to those found in modern marine environments, have adapted to survive in extreme conditions by breathing iron and using sulfur catalysts.
Scientists discovered an ancient ecosystem trapped beneath Taylor Glacier in Antarctica, which survived without light or oxygen by transforming sulfur and iron compounds for growth. This unique ecosystem has the potential to explain how life might exist on other planets and serve as a model for life under ice.
Researchers linked pre-historic seismic events on the San Andreas Fault to assess likelihood of future great ruptures. Analysis suggests several events similar to a historical earthquake occurred since A.D. 900 on the southern San Andreas fault.
Scientists are conducting airborne field campaigns in the Arctic to study Greenland and Iceland ice sheets and their sea ice and glaciers. NASA's ICESat spacecraft is also completing a seasonal survey of the world's ice sheets to gauge changes in ice thickness and mass.
Researchers found that dust blown to Antarctica from Patagonia provides vital information about glacier activity and past climates. The study suggests that the coldest periods of the last ice age correspond with the dustiest periods in Antarctica's past.
Scientists use Autosub, a robot submarine, to map the seabed and underside of Pine Island Glacier in Antarctica. The mission aims to understand why the glacier is thinning and accelerating over recent decades.
A team of Yale scientists has discovered that a significant drop in CO2 levels triggered the rapid formation of massive ice sheets in Antarctica around 34 million years ago. The findings refute previous theories and suggest that a decline in greenhouse gases played a crucial role in shaping the climate during this period.
Research papers highlight the impact of melting glaciers and ice caps on sea levels, with a minimum of 180mm of rise expected in the next 100 years. Additionally, studies show the widening of the tropical belt due to human environmental effects and an underestimation of ozone abundance in the troposphere.
A Montana State University study has found that the coldest daily temperatures recorded in Bozeman, Mont., and Coldstream, British Columbia, have occurred less often over the past several decades. Extreme warm nighttime temperatures have become more frequent at a rate of about one percent per year or 10 percent per decade.
Recent research on Mars includes studies on the planet's geology and potential habitability. A new method for classifying Quaternary glacial deposits was also proposed by GSA Today's science article.
Scientists analyzed East/Japan Sea CO2 uptake, finding a surprising drop in recent years. Simulations also suggest large raindrops favor tornado formation. Remotely sensed dune celerity revealed the world's fastest moving dunes, while Martian craters indicate hidden ice deposits.
Researchers found evidence of increased greenhouse gases in ancient ice core records, suggesting that human influence on climate started with large-scale agriculture and deforestation. The study challenges the traditional view that the Industrial Revolution marked the beginning of human-induced climate change.
Researchers monitoring Greenland's glaciers report a nearly three-fold increase in ice loss this summer compared to the previous record year. The total ice loss since 2000 is 10 times the size of Manhattan Island.
The USGS discusses prehistoric climate changes providing clues to future shifts and large deposits of gas hydrates on Alaska's North Slope. Holiday lights reveal the mineral composition behind their glow.
Research focuses on solar magnetic flux, which is linked to cosmic ray boosts. The study also investigates iceberg scrapes causing glacial quakes in Greenland. Additionally, scientists examine the renewed growth of atmospheric methane, which plays a significant role in ozone layer chemistry.
A rare mineral called nahcolite has been found to form only under high atmospheric CO2 levels, suggesting a possible benchmark for future climate change. The discovery is rooted in the Eocene Epoch, when CO2 levels were three times higher than current levels, and may signal an impending 'hothouse' climate by the end of the century.
Researchers using ground-penetrating radar on NASA's Mars Reconnaissance Orbiter have discovered vast Martian glaciers of water ice under protective blankets of rocky debris. The concealed glaciers extend for tens of miles and are up to one-half mile thick, making them the largest reservoir of water ice on Mars outside the polar caps.
Researchers found no radioactive signals in recent ice core samples from the Naimona'nyi glacier, suggesting that it has not accumulated new ice since 1944 and posing a threat to water supplies for half a billion people in Asia. The absence of these signals makes it challenging to date the ice cores and extract climate history.
Research reveals how intense glacial erosion changes the St. Elias mountain range's internal structure, responding to plate tectonics and climate change. The study provides new insights into the impact of glaciers on mountain formation and evolution.
A new NASA technique uses satellite data to measure changes in the mass of mountain glaciers in the Gulf of Alaska with unprecedented precision. The annual ice mass lost from glaciers has been found to be 84 gigatons annually, contributing nearly half as much freshwater melt as Greenland.
A genetic study found that Townsend's warblers have inherited mitochondrial DNA from hermit warblers, indicating interbreeding in the past. The DNA analysis suggests that natural selection drove hermits out of their range, leaving behind genetic fingerprints.
Researchers have developed a numerical model to recreate the Rhône Glacier's state in 1874 and predict its future evolution. The model predicts a significant increase in equilibrium line altitude due to climate change, leading to a 50% loss of volume by 2060 and complete disappearance by 2100.
New research suggests that glacial dams formed at the mouths of tributaries helped prevent the Tsangpo River from carving into the Tibetan Plateau. These dams, made of moraines and debris, flattened the river's slope and reduced its ability to cut into the surrounding terrain.
Most Alaskan glaciers are retreating and thinning, especially at lower elevations, while some are advancing, according to a comprehensive USGS study. The report uses satellite images and aerial photographs to document glacier behavior and distribution.
A team of researchers attributes the sudden thinning of Jakobshavn Isbræ, one of Greenland's largest glaciers, to subsurface ocean warming and atmospheric changes. The study suggests that ocean temperatures may play a more significant role in glacier flow than previously thought.
A recent study published in Geophysical Research Letters shows that small coastal glaciers in Greenland are responsible for the majority of the island's recent ice loss. Researchers found that these smaller glaciers account for three times more ice loss than their larger counterparts.
A CU-Boulder team discovered how microbial life becomes established and flourishes in extreme environments, with three species of cyanobacteria colonizing soil within the first year. The diversity of bacteria increased significantly over four years, snatching gaseous forms of carbon and nitrogen from the atmosphere.
A new University of Colorado at Boulder study concludes that global sea rise of more than 6 feet is physically impossible by 2100. The team estimates a total sea level rise of roughly 3 to 6 feet, which is still potentially devastating for low-lying coastal areas.
Researchers monitoring daily satellite images of Greenland's glaciers have discovered break-ups at two of the largest glaciers, including Petermann and Jakobshavn. The expected disintegration of the Northern hemisphere's longest floating glacier will continue within the next year.
Dan Shain's expeditions aim to study the reproductive behavior of giant earthworms and ice worms, shedding light on their unique adaptations. His research seeks to understand complex processes like cocoon secretion and movement patterns over geological time.
University of Cincinnati geology researcher Tom Lowell discusses the latest research on the Younger Dryas event, a significant climate change event that occurred around 12,900 years ago. Lowell's team has found evidence of discrepancies in dating techniques used to study the event, which could have implications for understanding global...
Researchers have developed a network of unmanned, autonomous robots called SnoMotes to collect data on ice sheets and glaciers in the Arctic. These toy-like robots can navigate treacherous terrain and capture real-time measurements of barometric pressure, temperature, and relative humidity.
A team has extracted a 150-meter ice core from the McCall Glacier, which may provide quantitative data on climate change in the region over the past two centuries. The core spans the entire depth of the glacier and offers insights into past climate conditions using clues like gas bubbles and isotopes.
Researchers discovered that an Antarctic ice stream radiates seismic waves, similar to earthquakes, due to the 'stick-slip' phenomenon. The ice stream moves about 18 inches within ten minutes, producing two bursts of seismic waves per day.
A team of Penn State scientists has discovered a novel bacterial species, Chryseobacterium greenlandensis, that has survived for over 120,000 years in the ice of a Greenland glacier. The microorganism's ability to persist in extreme conditions makes it useful for studying life in various environments on Earth and potentially elsewhere.
Scientists from the University of New Hampshire and University of Maine are heading to Denali National Park on an ice core expedition to gather climate records from glaciers in the Alaska wilderness. The mission aims to provide a comprehensive picture of regional climate variability in the Arctic, spanning 2,000 years.
Scientists at Brown University found evidence of recent glaciation on Mars, challenging the notion that the planet's active climate was confined to the distant past. The team discovered ice packs up to 2.5 kilometers thick existed along Mars' mid-latitude belt as recently as 100 million years ago.
Researchers confirm structure of Greenland Ice Sheet plumbing and find that summertime melt indeed contributes to the speed up of ice loss. However, they also conclude that summertime melt is not as critical a factor as other causes of ice loss.
Researchers found that surface meltwater is responsible for only a few percent of the movement of Greenland's outlet glaciers, despite being a major factor in their acceleration. Meltwater is instead thought to play a more significant role in calving events, which contribute to ice loss.
Researchers identify tropical wetlands as primary methane emitters during glacial times, while forest fires remained constant. The study provides essential information on natural changes in atmospheric methane concentrations prior to human impact.
Researchers collected boulders from three glaciers in the Amundsen Sea Embayment, a region experiencing rapid ice sheet changes. The study's findings provide a long-term picture of glacier behavior and help improve computer models to predict future sea-level rise.
A new study by UC Irvine and NASA scientists has found that Antarctic ice loss increased by 75% in the last 10 years due to accelerated glacier flow. The team mapped patterns of ice loss on a glacier-by-glacier basis and detected a sharp jump in Antarctica's ice loss, now nearly as great as that observed in Greenland.
Scientists have discovered evidence of a subglacial volcano beneath the West Antarctic Ice Sheet, which erupted around 2000 years ago. The discovery provides vital insights into the ice sheet's dynamics and its potential impact on sea-level rise.
A University of Colorado at Boulder study finds that meltwater clogging and speeding of Kennicott Glacier may help explain the acceleration of glaciers in Greenland. The excess water causes water pressure to increase, causing the glacier to slide more rapidly down its bedrock valley.
Research from the University of Bristol finds Antarctic ice loss is concentrated at narrow glacier outlets, driven by accelerating ice flow, and may dominate the ice sheet mass budget. The study estimates a total loss of 192 billion tonnes of ice over the past decade.
Researchers found missing radioactive signals in Tibetan ice cores, indicating the Himalayan glacier has shrunk at least since the A-bomb test half a century ago. The loss of freshwater from glaciers could impact nearly half a billion people in India.
The Greenland ice sheet is experiencing rapid acceleration of melting, with record years in 2005, 2007, and a 30% increase in western part from 1979 to 2006. The melting is driven by warming temperatures, primarily due to greenhouse gas buildup.
Researchers found that Greenland's glaciers responded similarly to the 1920s warming event, with the Kangerdlugssuaq Glacier losing nearly a mile of ice in 1932. This parallels recent changes, increasing alarm about the island's ice fields and sea level rise.
Recent high-resolution images from NASA's Mars orbiters show extensive evidence of ice-made features on the planet's surface, including glacial debris and valley deposits. The findings suggest a dynamic history of Martian climate change, with water ice playing a key role in shaping the planet's geology.
New research suggests that Antarctic plant and animal life has a striking ability to survive global climate change. The findings contradict current reconstructions of past glacial ice extent and highlight the importance of integrating biological evidence into climate models.
As glaciers melt, DNA of ancient microorganisms may return to life, potentially altering ecosystems. The duration the DNA remains intact depends on factors such as temperature and oxygen levels.