Articles tagged with Ice Sheets
A new study found that ancient ice age valleys in the North Sea formed rapidly, within hundreds of years, and transported vast amounts of meltwater away from under the ice. This process has implications for how glaciers may respond to climate warming today.
A new study reveals that marine-based ice sheets were instrumental in accelerating the penultimate deglaciation, with the intensity and rate of melt being much higher than previously thought. This process was particularly intense, rapid, and prolonged, leading to an abrupt slowdown of marine circulation in the North Atlantic.
A new study using high-resolution satellite observations confirms theoretical predictions and computational models of sea-level changes in the region surrounding the Greenland ice sheet. The research adds confidence to projections of sea level rise across the next decades and century.
A team of scientists led by Sophie Coulson and Jerry X. Mitrovica have detected the first definitive proof of elusive sea level fingerprints. The findings validate almost a century of sea level science and help solidify confidence in models predicting future sea level rise.
Researchers have created the first charts of Antarctic ocean temperatures over the past 45 million years using molecular fossils and machine learning. The study suggests that the planet is nearing a 'tipping point' where ocean warming caused by CO2 will lead to catastrophic sea level rises.
Researchers found a remarkable record of how the East Antarctic Ice Sheet responded to changes in climate over 100,000 years, with cycles of melting and freezing driven by Southern Ocean temperatures. The study provides new insights into the sensitivity of the ice sheet to small, short-term climate fluctuations.
A new study identifies areas in Antarctica's East region that could significantly contribute to sea-level rise if they undergo basal thaw. The researchers used numerical ice sheet models to simulate temperature changes at the base of the ice sheet, revealing regions such as Enderby-Kemp and George V Land as most susceptible to thawing.
Researchers discovered hydrated glass in Antarctic rocks that indicates polar glaciation during the Late Cretaceous, around 66-100 million years ago. The findings suggest that climate conditions in Antarctica were more complex than previously thought, with evidence of ice sheets existing alongside a generally warm and humid environment.
A new study by Durham University suggests that the East Antarctic Ice Sheet can be protected from devastating effects of global warming if temperature increases are kept below 2°C. The researchers found that staying within this limit could prevent significant ice loss and contribute less than half a metre to sea level rise by 2500.
A recent study combined elevation data of the Antarctic ice sheet from two different satellites, CryoSat-2 and Sentinel-3, to obtain a more accurate map of latest elevation changes. The results showed that the average elevation of the ice sheets had decreased at a rate of 4.3 cm/year during 2016-2019.
A new study reveals that subsurface ocean warming in the subpolar North Atlantic caused Heinrich Events, which led to ice sheet instability and disruption of the Atlantic Meridional Overturning Circulation. The warming facilitated melting of polar ice sheets from below, resulting in accelerated shedding of icebergs.
Researchers developed a methodology to attribute coastal glacier retreat to human-caused climate change, revealing that even modest global warming causes most glaciers to melt or retreat. The approach simulates the behavior of real ice sheets like Greenland's, helping predict major ice loss and informing decision-making for policymakers.
A new study reveals that Arctic temperatures have jumped by two steps in the last 50 years, with the second step occurring in 1999 and missed by most climate models. The findings are significant for projecting future climate change, as they highlight the need for more accurate short-term climate projections.
Researchers found that 85% of the eastern Antarctic Peninsula's ice shelf perimeter has advanced since the early 2000s, linked to decade-scale changes in atmospheric circulation. The advance is due to more sea ice being carried to the coast by wind, which stabilises ice shelves.
The study found that even if Earth's climate stopped warming, it would be difficult to rebuild the ice shelf once it has fallen apart. The researchers suggest that the ice shelf may not recover unless the future climate cools considerably. This has significant implications for sea-level rise and the stability of polar ice sheets.
Researchers have discovered a 30-mile-long, 9-mile-wide subglacial lake in East Antarctica that may hold the key to understanding the continent's glaciation history. The sediments at the bottom of Lake Snow Eagle could provide valuable insights into climate change and the ice sheet's possible demise.
Jeanine Ash is part of a US effort to recover sediment cores from the West Antarctic Ice Sheet, which will help answer questions about sea level rise and global warming. The team aims to drill through up to 1,000 feet of ice in two places on the Ross Ice Shelf.
Researcher Douglas Kurtze's study reveals that gravitational pull can cause local sea level drops near melting ice sheets, contrary to global-mean sea level rises. The phenomenon occurs due to the weakening of gravity as the ice mass decreases.
Researchers find evidence of water pockets beneath the icy surface of Europa, which could facilitate exchange between the subsurface ocean and nutrients from neighboring celestial bodies. The discovery suggests a dynamic ice shell that supports habitability on the Jupiter moon.
Researchers at Hokkaido University found that cooler summer temperatures across Greenland are triggered by changes in the El Niño climate pattern in the Pacific Ocean. This discovery will help improve future predictions of Arctic ice sheet and sea ice melting.
A new study reveals highly variable year-to-year changes in surface meltwater lakes around the East Antarctic Ice Sheet. Warmer seasons lead to deeper and larger lakes, potentially vulnerable ice shelves are at risk of break-up due to climate change.
Scientists have found argon trapped in ice cores from Greenland and Antarctica, which can be used to reconstruct past climate changes and temperature shifts. The discovery could improve our understanding of the Earth's atmosphere and climate over hundreds of thousands of years.
Researchers reconstructed the advance of Kangiata Nunaata Sermia glacier, finding it moved at a rate comparable to modern retreat. The glacier's advance coincided with Norse settlements, contradicting the common assumption that climate warming leads to glacial retreat.
Researchers predict Greenland ice sheet will lose up to 3.54 meters of sea level equivalent by 3000, under unabated warming conditions. In contrast, reduced emissions pathway may see a loss of only 0.16-0.4 meters sea-level equivalent.
A new study by MIT researchers reveals that glacier ice flow is more sensitive to stress than previously calculated, with revised estimates potentially refining predictions of sea level rise. The improved model could help glaciologists better understand the impact of Antarctic ice flow on future sea levels.
Researchers from Denmark and Sweden have dated the massive Hiawatha impact crater in Greenland to 58 million years ago, revealing it occurred a few million years after dinosaurs went extinct. The crater's age opens up a new understanding of Earth's evolution during this period.
Researchers have found that the Greenland Ice Sheet is losing mass at an unprecedented rate due to the conversion of gravitational energy from meltwater into heat. The ice sheet's basal melting rates are comparable to those measured on the surface, but without solar energy input, producing a significant source of hydropower.
Scientists have found that the West Antarctic Ice Sheet formed 35 million years ago, with warm deep water delaying its expansion to the sea. This discovery helps improve forecasts of its future stability and ice retreat.
Researchers identified that the changing weight of ice sheets caused the entire landscape to tilt, changing the course of the Missoula megafloods. This finding provides a new perspective on Washington state's Channeled Scablands, carved by massive floods at the end of the last ice age.
Scientists resolve decades-long debate on Antarctic Ice Sheet sensitivity, finding it vulnerable to small CO2 fluctuations. Research shows that large portions of the ice sheet could have disappeared under current CO2 levels.
A new study published in The Cryosphere finds that warm seawater intrusion under glaciers may cause much higher rates of melting at the glacier bottom. This could lead to projected ice sheet volume loss being 10-50% higher, or more than doubling over the next century.
Researchers found that glaciers in the Northern Hemisphere lost a total area of 390 km² per year, with 60% attributed to the Greenland Ice Sheet. Only 3% of glaciers advanced during this period. The study highlights the impact of climate change on marine-terminating glaciers.
A submersible robot will explore three of Greenland's glaciers with a remotely operated vehicle Nereid Under Ice (NUI), mapping seafloor topography and retrieving sediment cores to study moraines and their impact on glacier stability. The mission aims to improve model projections for future sea level rise.
Researchers analyzed 23,000-year-old fisher-hunter-gatherer camp remains near the Sea of Galilee, finding a diverse diet and lifestyle that defies previous expectations. The site's abundance of animal bones reveals a robust subsistence strategy that utilized varied food sources.
A new study verifies that ancient glaciers caused the erosion of rocks up to 3 miles thick during the Snowball Earth period, resolving a long-standing debate. The research uses thermochronology to estimate temperature and thermal structure, finding a widespread signal of rapid cooling consistent with massive glacier erosion.
Researchers have compiled a comprehensive directory of subglacial lakes worldwide, revealing that 20% are active and pose a hazard to human populations. The inventory provides a knowledge base for scientists to assess future changes as the climate warms.
Scientists predict that continued global warming could lead to a five-meter sea level rise by 3000 CE, making large areas uninhabitable without extensive modification. The Antarctic ice sheet's collapse, driven by West Antarctica's grounding on a bed below sea level, is the primary reason for this decay.
A new study led by Imperial College London scientists has found that the West Antarctic Ice Sheet (WAIS) was larger than previously thought during colder periods in the Miocene, contributing significantly to sea-level rise events millions of years ago. This insight will help researchers predict the future of the WAIS as the world warms.
Researchers used Rayleigh waves to produce high-resolution images of the rocks underneath the ice sheet, identifying key factors controlling ice flow. The study provides a better understanding of processes contributing to accelerated ice discharge into the ocean and sea level rise.
A research team has reconstructed the preglacial topography of North America's mid-continent, revealing how ice sheets reshaped the landscape and allowing researchers to understand rock erosion and deposition under ice. The findings also provide insights into water resources and availability in the region.
A team of scientists simulated over 200,000 hypothetical Earth-like worlds to understand the types of environments astronomers can expect to find on real exoplanets. They found that in 90% of cases with liquid water on the surface, there are no ice sheets, but rather permanent ice belts along the equator.
A new data-model study suggests that the Antarctic Ice Sheet's tipping point was reached within a decade, leading to centuries of ice mass loss and potential irreversible ice retreat. The research team analyzed sediment cores and computer models to identify evidence of post-glacial tipping points in the past.
Researchers found that before the weakening of the Atlantic Meridional Overturning Circulation, ice sheets in the Northern Hemisphere began to stick to their bedrock more effectively, causing glaciers to grow thicker and disrupt global heat conveyor belts. This led to stronger ice ages and the observed climate pattern shift.
Researchers have identified large semi-stationary eddies off the Wilkes Land coast as causing warm water to flow towards the Antarctic continental shelf, contributing to melting of the Totten Ice Shelf. This finding has significant implications for predicting global sea-level rise.
A new study has found that Greenland's ice sheet is experiencing increased frequency and intensity of extreme ice melting events, leading to a 21% rise in meltwater runoff over the past four decades. This raises global flood risk and disrupts marine ecosystems.
New research from the University of Arizona suggests that a slowdown in the Atlantic Meridional Overturning Circulation (AMOC) will intensify extreme cold weather in the US. The study found that without the AMOC, extremely cold winter weather would become more frequent and severe.
A team of researchers, led by Scott T. Salesky, will conduct field work in Antarctica to study the impact of katabatic winds on snow transport and ice sheet growth. The study aims to advance understanding of katabatic flows and their effects on regional and global atmospheric and oceanic circulations.
Researchers found that changes to the ice sheet immediately impact the groundwater underlying the island, affecting Arctic hydrology and ocean circulation patterns. The discovery sheds new light on the importance of groundwater in responding to climate change.
Research suggests that climate-caused disruptions to the jet stream's position and intensity could lead to severe weather-related consequences. The study's findings imply that continued warming could cause significant deviations from the norm, rendering the jet stream drastically different within a matter of decades.
Research reveals that Greenland's coastal ice caps experienced growth rather than shrinkage during past periods of warming. This study provides a new perspective on climate change, highlighting the complex relationship between climate conditions and ice cap changes across different regions of the Arctic.
Researchers deployed 100 short-period seismometers to measure ice flow velocity in East Antarctica, tracking movement of up to 1m over a one-month period. The study found that seismic stations on ice sheets showed shifting longitude distributions, while those on bedrock maintained consistent coordinates.
Scientists have imaged fine-scale landforms within ancient glacial channels in the North Sea, revealing how water moved through the channels and even how ice stagnated and melted away. The findings provide clues to how ice sheets react to a warming climate and offer insights into future changes in ice sheet behavior.
A Princeton University-led research team discovered that water blisters on the surface of Greenland's high-elevation ice sheet can estimate transmissivity, a property characterizing the efficiency of water networks between ice and bedrock. The study found that transmissivity can increase by two orders of magnitude during the summer mel...
Researchers observed a 'warming bias' in the Earth's ancient history, with more warming events and greater temperature shifts than cooling events. The study suggests that a multiplier effect may kick back in as ice sheets disappear, leading to further amplification of human-induced global warming.
A decline in atmospheric CO2 played a major role in driving Earth's climate from a warm greenhouse into a cold icehouse world around 34 million years ago. Land temperatures cooled by about 3C alongside ocean temperatures, and only climate models with declining CO2 could reproduce this cooling.
Scientists at Stanford University have developed a technique using solar radio signals to measure the depth of ice sheets and glaciers, which could lead to large-scale insight into melting ice sheets and sea-level rise. The passive radar system uses naturally occurring radio waves from the sun to detect changes in ice thickness.
Scientists use NASA's Ice, Cloud and land Elevation Satellite 2 to map subglacial lakes under the West Antarctic ice sheet. The study reveals two new lakes and provides critical insight into freshwater exchange, which may alter ocean circulation and ecosystems.
Scientists discovered that changes in Earth's orbit allowed for ice-free regions to develop on 'Snowball Earth', enabling periodic survival of animal life. The research found evidence of iron-rich sedimentary rocks forming in the icy ocean near colossal ice sheets, providing a sanctuary for complex multicellular life.
A new study suggests that ice sheet thickness and the rate of calved icebergs limit the collapse of marine-terminating glaciers. Understanding this process is crucial for forecasting potential future sea level rise.
Simulations show domino effects at up to 2°C global warming, increasing risk of irreversible climate change. Rapidly reducing greenhouse gas emissions is indispensable to limit risks of crossing tipping points.