Researchers found the Antarctic Ice Sheet plays a significant role in regional and global climate variability. The ice sheet's dynamic behavior over the past 8,000 years has cascading effects on the entire climate system.
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.
Feldspar's unique surface defects enable ice crystals to grow, a discovery that sheds light on precipitation formation in clouds. The research found that microscopic edges and cracks on feldspar crystallites serve as active sites for ice nucleation.
A study found that the Greenland ice sheet nearly disappeared for extended periods in the last million years, challenging previous assumptions about its stability. The finding implies global warming could tip it into decline rapidly, causing rapid sea-level rise.
A team led by Stéphane Dorbolo found that a disk of ice becomes highly mobile due to a levitating layer of water between it and the smooth surface on which it rests and melts. By controlling the flow dynamics of the melted ice, they can direct its motion.
Two studies published in Nature offer new perspectives on the past behavior of Greenland's ice sheet, with one suggesting continuous presence for seven million years while another proposes it was nearly ice-free for at least 280,000 years. The findings highlight the complexity and dynamic nature of the ice sheet.
A study analyzing marine sediment cores reveals East Greenland's ice sheet underwent deep glacial erosion over the past 7.5 million years, responding to global climate change. This finding challenges previous theories on complete and extended deglaciation, suggesting a more complex history of ice sheet dynamics.
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.
A recent study published in The Cryosphere suggests Antarctic sea ice has barely changed in size over the past 100 years. Researchers used ship logbooks from explorers like Robert Scott and Ernest Shackleton to compare ice edge locations during the Heroic Age of Antarctic Exploration with modern satellite data.
A Martian ice deposit, Utopia Planitia, contains approximately as much water as Lake Superior, spanning over 2,050 miles in diameter. The deposit is estimated to be around 260-560 feet thick, consisting of 50-85% water ice.
The NASA IceBridge mission has concluded its eighth consecutive Antarctic deployment, carrying out a record number of research flights and providing valuable insights into changes in polar ice. The campaign's findings shed light on the impact of sea level rise on climate change.
Researchers created an environmentally friendly, inexpensive coating made from PDMS that keeps surfaces ice-free with low ice adhesion strength of 5 kPa. This innovation could replace toxic liquid de-icers used on planes and cars, providing a permanent protective solution.
Researchers linked changing sea ice to shifting beluga whale migration patterns over two decades, finding whales adapt to varying sea ice conditions. Continued reductions in sea ice may result in increased predation and shifts in behavior, impacting population viability and ecosystem structure.
International scientists are searching for the oldest ice core in Antarctica, up to 1.5 million years old, to decipher past climate processes and improve future predictions. The 'Beyond EPICA - Oldest Ice' project aims to drill a core with sufficient atmospheric gases to analyze past greenhouse gas levels.
Researchers have found that each tonne of carbon dioxide emitted contributes to the loss of 3 square metres of Arctic summer sea ice. This linear relationship reveals individual contributions to global climate change, surpassing previous estimates made by climate models.
A new analysis reveals a direct correlation between carbon dioxide emissions and Arctic sea ice loss. The study suggests that reducing carbon emissions could slow the ongoing loss of summer ice and help achieve a 1.5°Celsius global warming target.
The oldest and thickest Arctic sea ice is disappearing, weakening the 'bulwark' of ice that previously protected it. This has led to an increase in sea ice loss, especially during summer months, with multi-year ice decreasing from 20% to only 3% of total sea ice cover.
Experts from Cardiff University propose that deep ocean storage of carbon dioxide may be responsible for the planet's 100,000-year ice age cycle. By analyzing tiny fossil remains, researchers found more CO2 stored in the oceans during ice ages at regular intervals every 100,000 years.
A new study reveals that Greenland's ice sheet lost nearly 2,700 gigatons of ice from 2003-2013, 7.6% more than previously thought, due to mantle softening caused by the Iceland hotspot. This correction refines understanding of modern ice loss patterns and their evolution.
Ancient leaves reveal that carbon dioxide levels increased dramatically as the ice sheet began to deteriorate, raising questions about its stability today. The study found a rapid decline in ice extent over a short period, similar to modern times, where CO2 concentrations are rising.
Researchers have discovered chemical traces of sea ice in Greenland ice cores, allowing them to calculate past sea ice levels. The data suggests that the Arctic climate was 2-3 degrees warmer 8000 years ago, with less summertime sea ice than today.
A new University of Washington study finds a trend toward earlier sea ice melt in the spring and later ice growth in the fall across all 19 polar bear populations. The analysis shows that critical timing of sea ice break-up and freeze-up is changing in a direction harmful for polar bears.
A recent study reveals that the expansion of Antarctic sea ice has caused a significant freshening of the Southern Ocean. The increased freshwater flux from the sea-ice conveyor belt explains the observed salinity changes in the region.
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.
Scientists have created an interactive game, 'Ice Flows', to demonstrate the Antarctic Ice Sheet's response to climate change. The game allows players to control ice flow and observe its effects on penguins and seals.
Researchers studied West Antarctica's landscape and found the ice sheet thinned relatively quickly after a period of warming, losing 400m of thickness in 3,000 years. This caused sea levels to increase by up to two metres.
Arctic sea ice cover is still declining despite slower melt rates, scientists say. The new normal for sea ice extent is expected to remain low due to extreme weather conditions.
Researchers have discovered a 65% reduction in Antarctic sea ice around 128,000 years ago, which has significant implications for predicting the Earth's future climate. The study, published in Nature Communications, used analysis of ice cores to determine the state of Antarctic sea ice during this past warm period.
Researchers have found strong evidence of sea ice distribution in the Nordic seas over the past 90,000 years, using a marine sediment core. The study reveals that sea ice played a significant role in shaping climate change and ocean currents during this period.
A study published in PLOS ONE found that little auks target the continental shelf and its edge for foraging, regardless of sea ice presence. The birds' diet varied depending on the location, with larger prey preferred at the shelf break when ice was absent.
New study reveals Arctic algae play a crucial role in the ocean's food web, with species at great depths relying on carbon from these algae. The decline of Arctic sea ice could have significant impacts on marine life, including fish, seals and polar bears.
A new study reveals that changes in Antarctic coastal polynyas are driven by variations in surrounding ice, including ice shelves and glaciers. Sea ice production decreases during major events like ice shelf collapse and increases when off-shore first-year ice is reduced.
A new study reveals that Antarctic sea ice migration drives the strength of global ocean circulation by changing water density. The researchers found that freshwater from melting sea ice contributes 10 times more to freshwater input than land-based glaciers, making it a vital contributor to circulation.
Operation IceBridge completed its eighth spring Arctic campaign, collecting data on key portions of the Greenland Ice Sheet and Arctic sea ice. The mission focused on measuring changes in sea ice extent, thickness, and elevation, with implications for predicting melt season patterns.
A study of Antarctic coastline images reveals a 40-year record of ice loss to the ocean, with approximately 1000km2 of ice lost over the past four decades. The research team used satellite data to track changes in ice thickness and thinning rates along West Antarctica's coastline.
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.
Using radar data from NASA's Mars Reconnaissance Orbiter, a team of researchers found evidence of an accelerated accumulation rate of ice in the Martian polar cap. The volume and thickness of ice match model predictions, providing insights into Mars' climate change history.
Researchers have confirmed that Mars has undergone multiple rounds of climate change using radar measurements of its polar ice caps. The study reveals the planet's current retreat from an ice age began approximately 370,000 years ago and is still ongoing.
Scientists discover that temperature inversions and low-level atmospheric phenomena isolate the ice surface from the atmosphere, recycling water vapor and halting loss or gain of ice. This process, known as boundary-layer recycling, occurs in the center of Greenland's ice sheet and is surprisingly efficient.
Researchers discovered an insulating layer of air that forms near the surface during winter, reducing evaporation and precipitation on the ice sheet. This phenomenon explains why temperature has risen without increased precipitation on the central parts of the Greenland ice sheet.
Sea ice physicists project a possible record-low Arctic sea ice extent this summer, with thin ice unlikely to survive the melting season. The CryoSat-2 satellite data shows that arctic sea ice was unusually thin in 2015 and grew slowly during the past winter.
A study suggests that gas hydrates in sediments slowed down an ice stream in the Barents Sea during the last ice age. The sticky spots under the ice act like hook and loop fasteners, creating friction and lubrication that can stop or slow the flow of the ice stream.
A recent study by University of Montana researcher Jesse Johnson reveals that geothermal heat enhances rapid ice flow and subglacial melting in northern Greenland. The research, published in Nature Geoscience, identifies a west-to-east zone with anomalously high heat that drives widespread melting and rapid ice flow.
Researchers found that meltwater streams on Greenland's ice sheet erode channels at a rate of up to 10 centimeters daily, similar to river erosion patterns. This discovery provides a new tool for studying melt rates and glacial response to climate change.
A study by GFZ researchers reveals that Earth's internal heat is responsible for the rapid flow of Greenland's ice, driven by a geothermal anomaly that originated from the Icelandic mantle plume. The anomaly creates a region with abundant subglacial meltwater, lubricating the base of the ice and making it flow rapidly.
A new study found that exceptionally warm weather episodes, rather than radiant energy, cause significant melting of the Greenland ice sheet. The research revealed that climate models tend to underestimate the impact of these events, which are expected to occur more frequently in the future due to climate change.
Researchers at OIST Graduate University have made a groundbreaking discovery about the behavior of protons inside ice. They found that protons exhibit locally ordered yet globally disordered patterns, which are rare in nature and occur only in ice.
Researchers predict that Antarctica's ice sheet could contribute up to 15 meters of sea-level rise by 2500 if greenhouse gas emissions continue unabated. An aggressive reduction in emissions could limit the risk of major Antarctic ice sheet retreat and associated sea-level rise.
A new ice sheet model suggests that Antarctic ice sheet melting could lead to a 50-foot rise in sea level by 2500, potentially doubling previous estimates. The researchers attribute this to ocean warming and the fracturing of floating ice shelves, which would cause them to collapse into the sea.
Scientists at NASA and the National Snow and Ice Data Center report that Arctic sea ice extent reached a record low wintertime maximum in 2016, with the lowest extent since satellite records began in 1979. The warming ocean waters are likely to contribute to continued declines in Arctic sea ice cover.
A study by Rutgers University researchers links Greenland's melting surface ice to shrinking Arctic sea ice and strong 'blocking-high' pressure systems. The findings highlight the increased threat of coastal communities as sea levels rise.
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 discover that warm ocean water is carving channels under Antarctica's ice shelves, weakening their stability. This process can lead to the disintegration of ice shelves, allowing more rapid ice flow into the ocean and increased rates of sea level rise.
Researchers study ice shelf motion and flow to better understand Antarctic ice sheet dynamics. GPS and tilt sensor measurements help modelers project future changes in ice shelf behavior, contributing to sea level rise predictions.
Researchers found that a 100,000-square-mile section of the Ross Ice Shelf broke apart within 1,500 years during a warming period after the last ice age. The study provides clues about how Antarctica's nation-sized Ross Ice Shelf might respond to a warming climate.
A new paper in Nature presents an alternative narrative to the collapse of Earth's ice sheets. Research on the Laurentide Ice Sheet reveals that ice loss occurred through frozen rivers that turned on and off, shifting from place to place. The findings provide a window into ice streams' complex behavior over long periods of time.
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.
A new study suggests that the Greenland Ice Sheet's stiff upper layer of ice formed during the Holocene era may be causing its deceleration. The analysis reveals that softer ice, resulting from higher atmospheric dust levels, is being compressed by stiffer ice below.
Researchers created a paleo-velocity map for Greenland, showing the ice sheet's flow pattern over the past 9,000 years. The study found that the ice sheet's interior is moving more slowly than during most of the Holocene period, while glaciers along the edges are rapidly thinning.
The West Antarctic ice sheet may experience catastrophic collapse due to ocean warming, leading to a 3-meter increase in global sea levels. Researchers have identified that parts of the ice sheet have existed continuously for at least 1.4 million years.