Articles tagged with Glaciers
Researchers found that melting on Greenland passed a tipping point 20 years ago, causing the smallest glaciers and ice caps to no longer regrow lost ice. The study suggests that this will raise global sea level by about 1.5 inches by 2100.
A new study reveals that the sub-antarctic island of South Georgia was covered by a massive ice cap about 20,000 years ago. The researchers used sonar mapping and gravity corers to find hundreds of distinct ridges bulldozed into the seabed, showing that the ice extended across South Georgia's vast continental shelf.
Research reveals large-scale thaw-induced slope disturbances and mobilization of primary glacial sediments, leading to cascading effects on fluvial, lacustrine, and coastal systems. The study's findings have major implications for predicting northern landscape change and downstream impacts.
Researchers found that local atmospheric conditions and ocean circulation are the main drivers of ocean temperature changes in the critical depth range, leading to increased melting. The study used a five-year record to track the interactions between ocean and atmosphere, revealing an annual cycle in heat exchange that drives melting.
Researchers confirm that the floating ice shelf is strongly coupled to the ocean below and Nares Strait, with temperatures changing with seasons and tides. Temperature data shows warming of ocean water at an average rate of 0.03 degrees Celsius per year, consistent with adjacent studies.
A new UCI study shows that Canadian glaciers are losing ice at an alarming rate, with surface melt accounting for 90% of the loss since 2005. The researchers found that the Queen Elizabeth Islands' ice cap has been melting by 900 percent annually, contributing to sea level change.
Two research papers use OMG observations to document how meltwater and ocean currents interact along Greenland's west coast, improving seafloor maps used to predict future melting and sea level rise. The study also reveals the role of meltwater in cooling warmer subsurface water and tracking its impact on glacier melt rates.
Researchers at the University of Washington used CryoSat-2 data to identify four interconnected lakes draining beneath Thwaites Glacier in eight months. The glacier sped up by about 10 percent during this time, indicating that other factors, such as ocean warming, are driving its long-term movement.
A new study has determined that the first Paleoproterozoic global glaciation and significant step change in atmospheric oxygenation occurred between 2,460 and 2,426 million years ago. The rise of atmospheric oxygen was characterized by significant oscillations before irreversible oxygenation of the atmosphere 2,250 million years ago.
Researchers at Iowa State University have received grants to improve glacier-flow models and predict the contribution of glaciers to sea level rise. The team will use lab experiments, field work, and complex computer models to better understand the physics of glacial ice movement and develop more accurate sliding laws.
Researchers have mapped large oceanic valleys beneath massive glaciers flowing into the Amundsen Sea in West Antarctica. The discovery reveals channels that enable warm water to reach the undersides of glaciers, fueling their rapid retreat.
New study reveals large oceanic features that enable warm water to reach glacier undersides, fueling rapid retreat. The findings highlight the importance of ocean heat access in controlling glacier behavior.
Researchers from the University of Cincinnati studied pink snow algae growing on volcanic terrains in the Pacific Northwest, finding it can lower albedo and increase surface melting. The study suggests atmospheric sources of ammonia and nitrate may be driving the growth and survival of these algae.
A new study uses airborne ice-penetrating radar to observe meltwater's year-round life under the Greenland ice. The research reveals extensive winter water storage beneath the ice, which affects glaciers' response to melting.
Researchers studied groundwater hydrology of proglacial valleys in the Andes, finding that 29% of stream discharge comes from groundwater. The study aimed to improve hydrological modeling of proglacial catchments throughout South America.
Researchers observed 'traffic jams' in the Rutford Ice Stream in Antarctica, where ocean tides speed up or slow down glacial movement. The study used COSMO-SkyMed radar-imaging satellites to gather near-continuous data for nearly nine months.
Scientists can now map the speed of glaciers and ice sheets globally, tracking unique patterns and identifying areas with rapid change. This near-real-time data enables researchers to understand the impact on sea level and coastal communities.
A University of Washington study found that 37 mountain glaciers worldwide show a high degree of signal-to-noise ratio in their retreat, indicating a strong response to climate change. The probability of natural variations explaining the observed retreats is extremely low, ranging from less than 0.001 percent to 11 percent.
A deadly avalanche in 2016 killed nine nomadic yak herders in western Tibet, with climate change cited as a likely cause. Researchers found that meltwater lubricated the ice, allowing it to flow quickly down the mountain.
A new study reveals that ice age vertebrate species in the eastern US responded to glacial cycles and global warming in different ways. The research found that about 75% of animals expanded their populations, while 25% contracted, suggesting additional complexity in climate change impacts.
Researchers at Ohio State University discovered a crack that formed deep beneath the Pine Island Glacier, leading to its breaking apart in 2015. The rift's origin suggests that warming ocean waters are melting the center of the West Antarctic Ice Sheet, potentially causing accelerated ice loss and sea-level rise.
Research reveals that the grounding line of Pine Island Glacier retreated from a prominent seafloor ridge by 1945, with final ungrounding occurring in 1970. The team's findings suggest that ice-sheet retreat continued even when climate forcing weakened.
Researchers found that a cavity formed beneath the glacier prior to the mid-1940s, allowing warm sea water to flow under it and cause retreat. The study provides direct evidence of the timing of glacier retreat before satellite measurements were available.
A new species of quillwort (Isoetes mississippiensis) discovered in Mississippi, USA, is the largest representative of its genus, with two known populations at risk of extinction. Further study reveals its genetic makeup and potential role in biodiversity and conservation science.
A new study found that 10-50% of iceberg melting occurs in Greenland's fjords, outweighing the amount of freshwater coming from the island's glaciers. This discovery could help scientists better understand how Greenland melts and its impact on ocean circulation and climate.
The Alps are steadily uplifting at a rate of 1-2 millimeters per year, with the majority of this movement attributed to the loss of the Last Glacial Maximum (LGM) ice cap. Researchers have found that 90% of today's uplift is due to the thawing of ice, rather than tectonic activity or erosion.
Research on Greenland's glaciers reveals that cryoconite granules, formed by cold-loving microbes and mineral particles, accelerate melting. The study found a correlation between fine mineral particle concentrations and cryoconite granule presence.
Two studies by UCI and NASA found the fastest rates of glacier retreat in West Antarctica, offering insights into ice melting and its impact on global sea level rise. The researchers used satellite data to measure changes in glacier grounding lines, revealing significant ice loss at the bottom of glaciers.
Two new studies by UCI and NASA researchers found the fastest rates of glacier retreat ever observed in West Antarctica, shedding light on the interaction between ocean conditions and bedrock beneath glaciers. The studies provide crucial data for predicting future Antarctica ice loss and global sea level rise.
Glacial lakes in Bolivia are increasing in size, posing a threat to communities and infrastructure downstream. The study found that glacier recession could lead to glacial lake outburst floods, which have already occurred in the region, causing devastating effects on villages and farmland.
Operation IceBridge is studying the effect of summer melt on Greenland's largest and fastest-melting glacier, Helheim Glacier. The team is observing changes in ice elevation between spring and late summer to understand the cumulative response to melting.
A new technique pioneered by scientists at Plymouth University can unravel historic changes to Antarctic sea ice, as well as demonstrate past alterations to glaciers and ice shelves. The method builds on an existing technique that identified changes to Arctic sea ice, allowing for the recovery and analysis of IP25 lipids from sediments.
A recent study by ETH Zurich researchers found that opposing mountain ranges will experience different water balance changes due to climate change. The Juncal region in Chile is expected to become even drier, while the upper Langtang valley in Nepal may see increased water discharge due to glacier melt and increased rainfall.
A new study has found that ocean warming is the primary cause of glacier retreat on the western Antarctic Peninsula, with 90% of glaciers retreating since records began. This finding will improve predictions of ice loss and sea-level rise, as the Peninsula contributes significantly to global sea levels.
Researchers used a new mapping technique called Fodar to settle the debate on the highest peak in the US Arctic. The study found Mt Isto to be the tallest at 2735m, surpassing previously disputed peaks Mt Chamberlin and Mt Hubley.
A recent study reveals that red pigmented snow algae blooms in the Arctic significantly reduce albedo, leading to a runaway effect of accelerated melting. The findings suggest a universal model for algal-albedo interaction and quantify additional melting caused by algal blooms, shedding new light on climate change impacts.
Scientists have calculated the fate of Greenland's melting freshwater, finding that more than half of it is transported southward by the Labrador Current. The study suggests that the melting-induced impact on ocean salinity is smaller than expected and may lead to a weakening of the Gulf Stream system.
A team of scientists has developed an apparatus to measure the behavior of ice under various external forces. The device can be used to study both terrestrial glaciers and icy satellite bodies, providing insights into potential life-supporting oceans beneath the ice.
A new study predicts that Totten Glacier in Antarctica may cross a critical threshold within the next century, triggering an irreversible period of rapid retreat and contributing up to 2.9m to global sea-level rise. The glacier's instability is linked to its geology, which will become unstable if it retreats another 100-150km.
Researchers have found direct evidence of past changes in the Totten Glacier's glacial history, revealing unstable zones prone to rapid collapse. This study sheds light on the region's vulnerabilities and warns of potential catastrophic consequences for sea level rise.
A Dartmouth study reveals that surface meltwater and subglacial discharge are driving the loss of ice mass in Greenland's coastal glaciers. The findings show that meltwater can exploit weaknesses in glaciers, fracturing and weakening them, and also increase calving and melting.
Scientists have obtained high-resolution satellite images revealing the dramatic retreat of tropical glaciers in the Pacific, particularly in West Papua New Guinea. The Carstenz Glacier has almost completely disappeared, while the East North Wall Firn has split into smaller fragments.
A collaborative team of researchers has discovered that the North Atlantic Ocean played a pivotal role in the last great climate tipping point, leading to major expansions of carbon-rich southern-sourced deep waters into the northwestern Atlantic abyss. This finding provides new insights into the process driving these events, suggestin...
Scientists reveal how Arctic microbes speed up glacier melting through cryoconite formation, altering ice surface albedo and creating a self-sustaining cycle. This microbial process is driving the expansion of biologically productive regions on glaciers, contributing to sea level rise.
Researchers have uncovered evidence of 12 massive explosive eruptions in the Cassia Hills of southern Idaho, which left behind glassy deposits and a deep volcanic basin. These eruptions were hotter and more frequent than those at Yellowstone, and provide insights into ancient volcanic activity west of the famous park.
Fiamma Straneo has been chosen by the American Geophysical Union (AGU) for the Sverdrup Lecture, a top honor in ocean sciences. Her research focuses on the role of high-latitude oceans in climate change and ice sheet dynamics.
University of Exeter researchers present world-leading studies on climate tipping points and glacial lake outburst floods, shedding light on early warning signals and their implications for global action. The research aims to provide insights into the social and policy implications of these critical thresholds.
The interaction of water and magma can dramatically increase the explosivity of a volcanic eruption, producing billowing clouds that deposit tephra as fine-grained ash within 10 km of the vent area. The study of the 2008 Okmok eruption in Alaska provides insights into water-magma interactions and their impact on eruption parameters.
Research reveals that ice-shelf loss leads to rapid dynamic ice loss, exacerbating sea-level rise. The Antarctic Peninsula has experienced significant retreat and break-up of ice shelves over the past two decades, with upstream glaciers flowing into the ocean at an accelerated rate.
Researchers from Michigan Technological University identified a geological pop-up structure known as the Menominee Crack, which formed in 2010. The crack is believed to be a unique feature resulting from the removal of overlying rock or ice, possibly due to glaciers receding over 11,000 years ago.
Research-based climate scenarios predict catastrophic consequences of rising carbon emissions, including sea-level rise and coastal submersion affecting 1.3 billion people. The long-term view underscores the urgency to curb emissions within decades.
Researchers found that the Greenland ice sheet is releasing a significant amount of phosphorus into the Arctic Ocean, with annual input equal to some of the world's largest rivers. The nutrient could stimulate growth of plankton at the base of the ocean food web, impacting birds, fish, and marine mammals higher up the chain.
Researchers used computer models and field data to accurately depict current flow conditions in Greenland's topographically complex ice sheet. The study aims to improve knowledge of subglacial topography and predict potential effects on sea levels from a melting ice sheet.
New research reveals Greenland's ice sheet is releasing 400,000 metric tons of phosphorus annually, enriching Arctic Ocean waters and potentially stimulating growth of marine food chain. The nutrient could impact birds, fish, and marine mammals higher up the food chain.
New research from the University of Gothenburg suggests that water supplies in major Asian rivers, such as the Yellow River and Yangtze, will be stable or increase in the coming decades. The study models future climate change and its impact on the region's water balance.
Scientists at Potsdam Institute for Climate Impact Research found a unique relationship between summer insolation and atmospheric CO2 that explains past eight ice ages. Moderate human interference with the planet's natural carbon balance can postpone the next glacial inception by up to 100,000 years.
Historians Ian Calder and Jan Till believe Shackleton may have had an atrial septal defect, a congenital heart condition commonly known as a 'hole in the heart'. Shackleton exhibited symptoms of breathlessness and weakness during expeditions, which experts now attribute to this condition.
A CU-Boulder study reveals an ongoing loss of ice on Niwot Ridge and the Green Lakes Valley in the Rocky Mountains, likely to progress as climate warms. The decline is associated with rising temperatures each summer and autumn, causing glaciers, rock glaciers, and permafrost to thin.
Researchers found the Greenland ice sheet's firn layer is changing rapidly with climate change, altering its ability to store meltwater. The study suggests this could lead to higher-than-predicted sea level rise contributions from the ice sheet.
Geologists have discovered a unique landform in the Wabash River Valley that was formed by erosion from melting glacier floodwaters. The finding provides insight into how floodwaters may behave as glaciers continue to melt today, with potential effects on surrounding landscapes.