Researchers led by William Krabill are flying over Greenland to measure ice sheet and glacier thickness, using a combination of laser and radar instruments. The mission aims to update measurements from the Ice, Cloud and land Elevation Satellite (ICESat) and provide critical data on the future behavior of the Greenland ice sheet.
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.
Ice storms cause significant damage to pecan trees, particularly those less than 15 feet tall, with cleanup costs varying greatly depending on tree size and labor supervision. Researchers provide information on effective cleanup procedures and economic impact of ice storms on pecan production.
Researchers modeled West Antarctic ice sheet's past movements and found it collapsed and regrew multiple times due to ocean warming. The study uses deep sea oxygen isotope ratios to deduce Antarctic temperature changes and suggests the ice sheet may collapse if ocean temperatures warm sufficiently.
Researchers at the London Centre for Nanotechnology have discovered a novel one-dimensional ice chain structure built entirely from pentagons, challenging the long-held assumption that hexagons are the building blocks of ice. This discovery has significant implications for understanding hydrogen bonding at interfaces and may lead to ne...
The Greenland ice sheet is expected to melt, causing a 23-foot sea level rise, while Antarctica's ice sheet could add up to 190 feet. Recent studies show that the ice sheets are melting faster than snow replacement.
A study published in Geophysical Research Letters proposes that reducing global fossil fuel use by 20% in 2020 and 60% in 2050 could postpone the onset of the next ice age by up to 170,000 years. By building up ice sheets, scientists can regulate climate and extend current interglacial periods.
The study predicts a rise in sea levels around North America and southern Indian Ocean due to the collapse of the West Antarctic Ice Sheet, exceeding current estimates by as much as 25%. The ice sheet's melting will cause significant changes in global sea levels, with some regions experiencing rises of up to six meters.
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.
Scientists have discovered that parts of Antarctic bedrock are rising while others sink in response to melting ice. This finding will improve estimates of future sea level rise by providing a better view of what's happening under the ice.
Scientists have derived a simple law to predict where icebergs will calve off from parent ice sheets. The rate of spreading, width, and thickness of the ice shelf are key factors in this process, accounting for most observed variability.
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.
Studies reveal Greenland's ice sheet is thinning due to warming temperatures, while Arctic sea ice loss increases phytoplankton growth. Meanwhile, data from Mars Express spacecraft indicates a comet-like ion tail forms when solar wind sweeps ions into the Martian atmosphere.
An international team is exploring two uncharted regions of Antarctica to study the impact of climate change on global sea levels. The research aims to understand how Earth's climate changed in the past and how future climate change will affect global sea level.
Preliminary data indicate 2008 may represent the lowest volume of Arctic sea ice on record. The decline is due to rising greenhouse gases and strong natural variability.
For a four-week period in August 2008, Arctic sea ice melted faster than ever before, with an average daily decline of 32,700 square miles. The rate of decline contributes to concerns that all Arctic sea ice could be gone within the century.
Researchers estimate global sea level rise could be double or triple current predictions over the next century, with possible rises of up to a third of an inch per year. The study uses lessons learned from the demise of the last great North American ice sheet to inform its findings.
Researchers analyzed the disappearance of the Laurentide Ice Sheet to shed light on how much the Greenland Ice Sheet will contribute to sea level rise. The study found that rapid melting can happen very quickly, with rates comparable to global sea level rise evidence for this interval derived from coral records.
Research suggests that changes in atmospheric carbon dioxide levels are the primary cause of Greenland's ice formation, contrary to competing theories. The study uses computer climate and ice-sheet models to show that a decline in CO2 levels led to the long-term growth of the Greenland ice sheet.
Recent studies shed new light on the late Paleozoic ice age, revealing a dynamic icehouse regime and challenging traditional interpretations. This improved understanding can aid in preparing for rising atmospheric carbon dioxide levels and global temperature increases.
A study of a Greenland ice core has shown that two temperature spikes prior to the last ice age were tied to fundamental shifts in atmospheric circulation. The research found abrupt warming events that occurred suddenly, challenging modern societies' ability to adapt, and provided insights into the sequence of climate change
Researchers analyzed Greenland ice cores to understand sudden climate changes at the end of the last ice age. The results show that climatic shifts occurred rapidly over just a few years, with dramatic changes in temperature and atmospheric circulation.
A new study by NCAR researchers warns that rapid sea ice loss in the Arctic could lead to accelerated land warming and permafrost thaw, posing significant risks to sensitive ecosystems and human infrastructure. The study finds that a period of abrupt sea-ice loss could initiate significant emissions of greenhouse gases from Arctic soils.
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.
Scientists have discovered ice core data showing low CO2 levels and methane fluctuations that match temperature curves. The findings provide insight into climate history and help develop models for future climate changes.
Arctic sea ice is expected to decline further, with a 59% chance of breaking the annual minimum record for the third time in five years. This is due to the preponderance of younger, thinner ice and warming temperatures, which could have negative effects on wildlife and open up shipping lanes.
A new study by NCAR and CSU finds that unusually sunny weather contributed to last summer's record loss of Arctic sea ice. The research suggests that warmth from the Sun will increasingly affect Arctic sea ice loss in the summer.
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 found that surface meltwater can penetrate thick ice and accelerate ice flow, with a significant impact on fast-moving outlet glaciers. The study suggests a new plumbing system for the ice sheet, where meltwater can lubricate the base and reduce friction.
Scientists warn of potential sea-level rise as Antarctic ice shelf collapses. The Wilkins Ice Shelf's disintegration is linked to rapid climate change, with the remaining ice supported by a narrow strip between two islands.
Despite a colder-than-average winter, Arctic sea ice remains vulnerable due to long-term warming climate trends. The area of perennial sea ice, which lasts for several years, has declined significantly from 50-60% in the mid-1980s to less than 30% this year.
Scientists developed a new model to estimate sea ice thickness, using historical observations and environmental data analysis. The study shows that average ice thickness and total ice volume fluctuated together during the early period, peaking in the late 1980s before declining until the mid-1990s.
A NASA study reveals that warming air temperatures are causing the surface of Greenland's massive ice sheet to melt, leading to loss of ice throughout the mass beneath. The team found a strong connection between melting on the surface and ice loss below 6,500 feet in elevation.
The Baffin Island ice caps have shrunk by more than 50 percent in the last half century due to warming. The study found that these ice caps will be gone in 50 years or less if no additional warming occurs.
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.
A recent study by the University of Sheffield reveals that Greenland's ice sheet has experienced its most extreme melting in 50 years, primarily triggered by regional climate changes. The research highlights a striking correlation between Greenland's ice melt and global temperature variations.
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.
A new study indicates older Arctic sea ice is being replaced by younger, thinner ice, making the region more susceptible to rapid melt. The researchers used satellite data to reconstruct past Arctic sea ice conditions and found that 58% of remaining perennial ice is thin and only 2-3 years old.
Scientists found a potential reason for Greenland's ice melting: a thin spot in the Earth's crust enabling underground magma to heat the ice. The researchers believe this hotspot could be lubricating the base of the ice sheet, causing it to slide more rapidly out to sea.
The Arctic sea ice extent may have fallen by 50% since the 1950s, with September sea ice plummeting to the lowest levels on record. The researchers also noted that the date of the lowest sea ice extent has shifted to later in the year.
The Arctic sea ice extent on Sept. 16 stood at 1.59 million square miles, lower than the long-term minimum average from 1979 to 2000 by about 1 million square miles. The minimum also breaks previous records set in 2005.
Rising sea-surface temperatures in the Barents Sea have led to a decline in winter ice cover over the past 26 years. The study found that warming ocean temperatures, driven by increasing greenhouse gases, are the primary cause of this trend. In contrast, Arctic pack ice is expected to continue its rapid decline due to atmospheric effects.
Researchers discovered that brine moving up or down through floating sea ice follows universal transport properties, similar to water flow through sedimentary rocks. This finding can help improve forecasts of global warming's impact on polar icepacks and understand how polar ecosystems respond to climate change.
A CU-Boulder team forecasts a 92% probability of the September 2007 Arctic sea ice minimum extent setting a new record low. The researchers attribute this to rapid disintegration and thinning of multi-year ice, replaced by thinner first-year ice.
A CU-Boulder study finds that glaciers and ice caps are currently contributing about 60% of the world's ice to the oceans, with an accelerating rate of 3 cubic miles per year. The team estimates this could add up to 4-9.5 inches of additional sea level rise globally by 2100.
Researchers suggest that perennial water-ice deposits at Mars' South Pole are juggled between the North and South Poles every 51,000 years due to precession. Water vapour is transported from the North Pole to the South Pole, where it re-condenses and freezes, forming a thick layer.
Researchers use echo-sounding equipment to create images of the ocean floor, providing evidence that West Antarctica was involved in the growth of the Antarctic Ice Sheet. The findings suggest that more of the continent hosted an ice sheet at the start of the 'icehouse' Earth period.
Scientists have developed a breakthrough understanding of how individual water molecules come together to form ice crystals. This research provides unprecedented resolution and sheds light on the process of heterogeneous nucleation, essential for climate change models and cloud formation.
Researchers Philip Mote and Georg Kaser attribute Kilimanjaro's ice decline primarily to solar radiation and sublimation, rather than atmospheric warming. The decrease in snowfall and energy absorption by the ice also contribute to its shrinking size.
A NASA-led research team has measured critical areas of Greenland's ice sheet and glaciers, finding a significant loss of ice over the past several years. The data suggests that the island's major glaciers have sped up in thinning since the turn of the century, with documented changes of up to 100 feet per year.
Researchers found that high-altitude ice fields, like Mont Blanc and Dôme du Goûter, have remained stable in mass balance over the last 100 years. The accumulation of snow and ice has varied little since the beginning of the 20th century, indicating a lack of significant melting due to climate change.
A large area of low but increasing gravity over North America has been discovered, reflecting the lingering impact of the last ice age. The study provides an unprecedented image of the geometry of the long-vanished Laurentide ice sheet and reveals that its ghost still hangs over the continent.
Researchers found that water ice exists in variable depths and is patchy across the Martian surface. The discovery was made using data from NASA's THEMIS camera on the Mars Odyssey orbiter, which showed that areas with rocky surfaces have deeper ice deposits, while dusty areas allow ice to survive closer to the surface.
A new study finds that Arctic sea ice is retreating more quickly than computer models project, with the actual rate being 30 years ahead of schedule. The research indicates that greenhouse gases may be playing a significantly greater role in ice loss than previously thought.
Researchers at CU-Boulder's Colorado Center for Astrodynamics Research predict a 57% chance of lower sea-ice minimum than 2006, with 70% chance within lowest five years on record. Declining Arctic sea ice is linked to higher winter temperatures due to greenhouse warming.
Researchers are setting up observatories to examine changes under the Arctic ice cap, investigating water properties in the upper layers of the Arctic Ocean. The goal is to understand annual change and measure mechanisms that lead to ice melting from below.
The Arctic sea-ice extent in March 2007 was the second lowest on satellite record, at 5.7 million square miles. Researchers attribute declining sea ice to rising greenhouse gases and strong natural variability.
A team of researchers led by Jennifer Hutchings will spend two weeks studying the relationship between ice movement, stress, and sea ice mass in the Beaufort Sea. The goal is to validate current sea ice models and reduce uncertainty in predicting arctic climate change.
Experts warn of uncertainty over sea-level rise due to rapidly changing Antarctic Ice Sheet, particularly in the Amundsen Sea Embayment. Thinning ice shelves and increased melting are contributing to faster flow, potentially leading to 'runaway' thinning and several feet of sea-level rise over centuries.