Articles tagged with Glaciers
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A new study suggests that increased snowfall has protected Patagonia's glaciers from rising temperatures, but this effect is temporary and will cease if greenhouse gas emissions continue to rise. Curb emissions at 1.5 degrees Celsius above pre-industrial levels to protect maritime glaciers.
Geology researchers from UTEP are partnering with Bhutanese scientists to better understand and mitigate the impact of glacial floods on rural mountain villages. The project aims to use geophysical methods to identify changes in water levels and sediment transport, potentially helping vulnerable villages create early warning systems.
A computer modeling study found that glacial isostatic adjustment caused downward movements in the eastern US, while upward movements occurred in eastern Canada, contributing to relative sea-level rise. The research will help generate maps for aquifer management and inform decisions on sea-level rise impacts.
The Open Radar Code Architecture (ORCA) offers scientists a standardized way to build ice-penetrating radar systems, reducing costs and increasing efficiency. This enables glaciologists to collect and reuse data more effectively, advancing research into melting ice sheets and sea-level rise.
A research team led by Dr. Franco Marcantonio found significant lead pollution in a Tibetan glacier starting in 1974, with highest levels between 2000 and 2007. The team traced the source of pollution to Chinese gasoline emissions containing lead until its phasedown after 2007.
Researchers have confirmed that El Niño causes a drastic reduction in the snow-covered area of the Quelccaya Ice Cap in the Peruvian Andes. The study used NASA Landsat satellites to measure the ice cap's sensitivity to climate shifts, finding that it lost about 58% of its snow cover between 1985 and 2022.
The SUPERSLUG initiative aims to forecast the impact of sediment slugs on river catchments and communities. The project will use a range of sensors and numerical models to provide comprehensive predictions of where and how long-term effects might be felt, up to decades or centuries after an event.
Researchers at the Alfred Wegener Institute found that atmospheric blocking slowed the melting of Greenland's 79° N Glacier by cooling Atlantic seawater flowing into its cavern. This change had significant implications for the future of Greenland's glaciers, as warmer ocean temperatures typically accelerate ice melting.
European atmospheric blocking has slowed glacial melt at Greenland's Nioghalvfjerdsfjorden Glacier by cooling subsurface waters from 2018 to 2021. The findings highlight the importance of regional atmospheric dynamics in glacier stability, which is crucial for predicting future glacier behavior.
A Dartmouth-led study projects that Antarctica's glaciers will rapidly retreat and potentially collapse by 2200, increasing global sea levels by up to 5.5 feet by 2300. The researchers used 16 ice-sheet models to refine the projection of ice loss over the next 300 years.
A landslide in remote Greenland caused a mega-tsunami that sloshed back and forth across a fjord for nine days, generating vibrations throughout the Earth. The study used mathematical models to recreate the event and demonstrate how the sloshing of water would have continued, matching global seismic recordings.
Five boulders in northern New York and Vermont provide limits on earthquake shaking intensity. The age of the rock formations indicates how long it's been since a region experienced that level of shaking.
A new study has reconstructed virus DNA from glacial ice cores, revealing nearly 1,700 viral species with adaptations that influenced their hosts' survival in extreme conditions. The findings suggest a connection between viruses and climate change, shedding light on the impact of global temperature shifts.
A new study led by Dartmouth researchers questions the rapid polar ice collapse model used in the IPCC's sixth assessment report. The team found that the expected rate of retreat is significantly lower than predicted, making the worst-case scenario less likely, but still dire due to ongoing ice loss from Greenland and Antarctica.
A new study reveals Andean tropical glaciers are the smallest in over 11,700 years due to increasing temperatures and human-induced climate change. This region is a hot spot for understanding the cryosphere's changing state, with implications for higher-latitude glaciers.
A research team deployed an unmanned submersible to map the underside of a floating ice shelf in Antarctica, revealing high melt rates and unique patterns. The findings raise questions about current models for predicting sea level rise.
The UT Austin expedition aims to investigate how sediments control glacial melt and the future of the Greenland ice sheet. A robotic submersible will gather measurements of the glaciers' underwater walls and sediment-laden meltwater, while surveys and sediment cores will reveal past climate change impacts.
Researchers deployed an unmanned submarine 'Ran' under thick ice in Antarctica, revealing high-resolution maps of the glacier's underside. The findings indicate that stronger underwater currents and flowing water influence the melting process, with complex patterns and formations resembling sand dunes.
Researchers found that specific basidiomycete yeasts play a key role in stabilizing assimilated carbon, enriching organic carbon content. Glacial recession exposes new landscapes with limited contact with air, light, and nutrients, making them ideal for studying soil formation.
Researchers found that glacier loss on Juneau Icefield accelerated dramatically since 2010, with rates of glacier area shrinkage five times faster from 2015-2019. The study suggests that current glacier projections may be too small and underestimate future glacier melt.
In a study published in PNAS, researchers found that microscopic fungi play a key role in enhancing soil carbon storage in newly formed landscapes created by shrinking Arctic glaciers. The team discovered diverse communities of microbes thriving in the barren soils, and pioneer fungi sequester carbon in the soil.
Researchers from the Mann Research Group found strong path dependence in Plio-Pleistocene glaciations, driven by a gradual decrease in regolith and volcanic outgassing. The study suggests that carbon dioxide levels determine the onset of the Mid-Pleistocene Transition, and that it's not too late to act to prevent ice sheet collapse.
A study by MIT scientists found that microscopic defects in the ice shape how massive glaciers flow, leading to revised predictions of future sea-level rise. The researchers developed a model to estimate an icy region's sensitivity to stress, directly relating it to its likelihood of flowing.
Researchers at the University of Copenhagen have tracked the evolution of glaciers in East Antarctica using hundreds of old aerial photographs dating back to 1937. The study reveals that the ice has remained stable and grown slightly over almost a century, partly due to increasing snowfall.
Warm seawater is pumping underneath Antarctica's Thwaites Glacier, causing ice to melt intensely and leading to devastating sea level rise. Researchers predict the glacier may retreat into the deeper part of the basin within 10-20 years, accelerating glacier melt and impacting coastal communities worldwide.
New research reveals that ice shelves don't just buckle, but fracture when weighed down by meltwater lakes. This fracturing could cause vulnerable ice shelves to collapse and contribute to sea level rise.
Researchers at UTA used ultra-high energy neutrino particles to search for signatures of quantum gravity, but found no evidence of expected quantum gravitational effects. This non-observation represents a powerful statement about the still-unknown physics operating at the interface of quantum physics and general relativity.
A team of over 100 scientists from Brazil and the US ran high-resolution simulations of South America's past and future climate using a weather research and forecasting model. The goal is to better understand hydroclimatic processes and inform adaptation measures for millions affected by climate change.
A new study reveals that meandering ocean currents and the ocean floor induce upwelling velocity, transporting warm water to shallower depths, contributing to rapid melting of Antarctic ice shelves. This process poses a significant threat to coastal communities worldwide due to rising global sea levels.
Climate change causes melting of ice sheet, resulting in loss of about 5,000 meteorites per year. Researchers call for urgent action to preserve the scientific value of meteorites and reduce greenhouse gas emissions.
Research on South Georgia reveals that invasive species are colonizing newly exposed ground as glaciers retreat due to climate change. This process allows exotic plants and animals to rapidly adapt and spread across the island.
The 79° N-Glacier in Greenland has lost over 160 meters of thickness since 1998, with melt rates reaching 130 meters per year. The glacier's instability is attributed to warm ocean currents and atmospheric warming, threatening sea level rise.
Researchers at UC Irvine and NASA found that warm ocean water beneath the ice is causing accelerated melting of Petermann Glacier in northwest Greenland. The study predicts that potential sea level rise will be much worse than previously estimated, with melt rates highest near the mouth of the grounding zone cavity.
As glaciers shrink due to global warming, glacier-fed streams are becoming warmer, calmer, and clearer, allowing algae and microorganisms to thrive. This shift is leading to a 'green transition' in these ecosystems, with potential impacts on carbon and nutrient cycles.
A study published in the Journal of Geophysical Research: Oceans has provided new insights into ocean circulation patterns around glaciers, which can enhance the accuracy of climate models. The research used GPS-tracked icebergs to track hourly changes in their position as they passed through Greenland's Ilulissat Icefjord.
A young researcher from the University of Copenhagen has made a surprising discovery of high concentrations of methane in meltwater from three Canadian mountain glaciers. The findings challenge previous assumptions that methane in meltwater could only be found in oxygen-free environments under large ice masses.
Scientists have observed the fastest-known large-scale breakage along an Antarctic ice shelf, demonstrating a 6.5-mile crack that formed in about 5.5 minutes at a speed of 80 mph. This finding reveals the physics behind ice sheet collapse and provides insights into potential calving events.
A new study suggests that the Thwaites Glacier and Pine Island Glacier began experiencing significant glacial retreat in the 1940s, driven by an extreme El Niño climate pattern. This finding corroborates previous research on ice sheet dynamics and highlights the importance of external factors in controlling glacier behavior.
A team from the Alfred Wegener Institute found that warm Atlantic water is melting Greenland's 79° North Glacier, causing it to grow thinner. The study used a high-resolution ocean model to simulate the circulation below the ice tongue, revealing that higher ocean temperatures in the Atlantic are chiefly determining the melting rates.
Researchers at Stanford have found that the Wilkes Subglacial Basin in East Antarctica could be closer to runaway melting than previously thought. The study suggests that this region, which holds enough ice to raise global sea levels by over 10 feet, may be vulnerable to irreversible melting if warming seawater gets under the ice sheet.
Researchers found that global warming made the Corbassière glacier unusable as a climate archive, destroying reliable information about past climate and air pollution. The glacier's ice core showed flattened concentration curves and lower amounts of trace substances, likely due to meltwater washing away the deposits.
By 2050, at least 34% of Alpine ice volume will be lost even if global warming stops. This is based on a new study predicting near-term ice loss due to climate inertia.
Researchers discovered traces of sunscreen agents in Arctic snow, with highest concentrations found in winter. The study suggests these contaminants are transported from lower latitudes via atmospheric circulation.
Reducing air pollution to pre-pandemic levels can protect Himalayan glaciers and prevent melting by the end of the century. Clean energy and lower-emission modes of transport would bring significant benefits for sustainable water supplies and ecosystems in Asia.
Researchers discovered that rising temperatures trigger katabatic winds in Himalayan glaciers, cooling the air and preserving surrounding ecosystems. The team used climate models to demonstrate this phenomenon across the Himalayan range, suggesting that some glaciers may have a chance to 'save' themselves by reacting to global warming.
Scientists tracking Cadman Glacier's rapid retreat highlight the importance of long-term monitoring of Antarctica's polar regions. The glacier's ice shelf thinned due to warmer ocean waters, leading to a 28% increase in ice discharge over 13 months.
A Northwestern University and University of Copenhagen study reveals that Greenland's thousands of peripheral glaciers have rapidly retreated over the past two decades. The research team combined satellite images with historical aerial photographs to document changes in over 1,000 glaciers over a century.
Researchers studied mountain goats' behavior in Glacier National Park, finding that ear flicks showed a strong correlation with the presence of snow. The lack of summer snow patches may increase their risk of local extirpation due to increased tick infestations.
The loss is attributed to warming ocean temperatures causing glaciers' floating extensions to melt. This weakening could lead to accelerated sea-level rise as the ice shelves act as frozen dams regulating ice discharge into the ocean.
New research suggests that meltwater flowing out to sea from beneath Antarctic glaciers is accelerating their retreat and contributing to global sea-level rise. The study's simulations indicate that this process could make a significant contribution to sea-level rise by 2300, potentially up to 15%.
Research reveals human occupation in Charco Verde II site from 21,000 to 15,000 years ago, defying the idea that Upper Palaeolithic humans avoided inland Iberia due to its cold climate.
Research reveals the grounding line of the Ronne Ice Shelf can shift up to 15 km with changing tides, controlling ice stability and potentially accelerating ice melt. This finding highlights the need for improved observations and modeling of tidal processes to predict Antarctica's response to climate change.
Researchers aim to access ocean waters hidden beneath ice shelves, where critical information about climate change is stored. An intelligent mothership and coordinated marine robots will communicate data from under-ice cavities, optimizing sampling and configuration.
A new inventory from Portland State University researchers reveals that some glaciers have disappeared entirely, while others have shrunk to tiny sizes. The loss of these natural regulators has significant impacts on streamflow, drought susceptibility, and sea level rise.
Researchers tracked daily volume changes with automated laser scanning to determine Glacier Loss Day (GLD), a critical indicator of glacier health. The 2022 GLD was reached earlier than usual, signaling severe climate change impacts.
Researchers have identified pathways through which warm ocean water flows into ice shelf cavities for the first time. The study found broad ocean heat intruding toward the shelf, with seawater temperatures up to 1℃ higher than freezing at depths of 50-100 meters.
A new study published in the Journal of Glaciology suggests that prior attempts to evaluate the mass of Antarctic ice shelves may have overestimated their thickness. The researchers found that on average, the Antarctic ice shelves are nearly 6% thinner than previously assumed, a difference of about 17 meters.
A multinational team of researchers studied the flow of warm water to the Totten Ice Shelf, revealing crucial details on how Circumpolar Deep Water interacts with the glacier and accelerates melting processes. The findings highlight the importance of bathymetry and regional circulation in regulating ocean heat transport towards the ice...
Recent extreme events in Antarctica and the Southern Ocean are likely to become more common and severe due to global warming. The study calls for urgent policy action to protect the continent's fragile environments, which have global implications if not preserved.
A new study by Flinders University researchers suggests that only 1% of dormant pathogens could cause major ecological harm, leading to the loss of host organisms worldwide. The simulations showed that these ancient microbes can survive, evolve, and become dominant in modern ecosystems, posing a substantial danger.