Articles tagged with Antarctic Ice
The Arctic melt season has extended by seven and a half days since 1979, driven by sea ice forming later in the fall, with implications for the global climate system. The changing sea ice properties also impact the ecosystem, including the health of algae, which affects the entire food web and fisheries in the sub-Arctic and Arctic.
A new study highlights the impact of coastal freshening on the giant amphipod species Paraceradocus miersi, which lose salts, gain water, and suffer gill damage in diluted waters. The research warns that continued freshening may pose a significant threat to many marine invertebrates and reshape the global ocean's communities.
A recent study published in Nature found that Antarctica's brief rebound in 2021-2023 was caused by climate variability, not a new normal. The researchers linked the extra precipitation to the tropical warm pool, a warm patch of ocean in the western Pacific and eastern Indian oceans, which made an outsized contribution to extreme weath...
A new study reveals that Antarctica's recent snowfall surge was caused by climate variability, not a long-term trend. The surge added mass to East Antarctica, but mass loss continued in West Antarctica, highlighting the need for continued monitoring and research.
The EU project SYNCHRONY aims to improve understanding of climate and ecosystem changes in the Southern Ocean and around Antarctica, and will establish an internationally coordinated observing system. The project will coordinate interdisciplinary activities, harmonise data streams, and create new data products.
A study found that the spring SAM underwent a marked structural shift around 1998, strengthening its delayed influence on Antarctic summer sea ice. This shift led to enhanced ice-loss processes, including increased air-sea heat exchange and ocean warming in the Weddell Sea.
Researchers found that about 40% of West Antarctica's ice may be lost already, while East Antarctica could lose more with 2-3°C warming. The study highlights the need to monitor and mitigate greenhouse gas emissions to prevent destabilization of Antarctic ice basins.
Scientists at the University of East Anglia used an autonomous underwater vehicle to survey beneath the Dotson Ice Shelf, finding that the shape of the seabed is more important than current speed in influencing warm water circulation. This leads to melting at the underside of the ice shelf, contributing to sea level rise.
A team of researchers, including URI climate scientist Ambarish Karmalkar, used interactive modeling to predict the impact of Antarctic ice sheet meltwater discharge on climate and sea levels. Their findings show that while cold Antarctic meltwater will slow human-induced warming, it also causes uneven sea level rise and significant cl...
A new study reveals that Antarctic sea ice plays a critical role in predicting global warming, with a greater extent of sea ice leading to more significant warming. The research found that ocean heat uptake and thermal sea level rise will be higher than previously estimated by 2100, with implications for policy and science.
A 30-year study reveals East Antarctica's interior is warming at a rate of 0.45-0.72°C per decade, faster than global average, driven by changes in the Southern Indian Ocean. This warming process may underestimate future Antarctic ice loss predictions.
Researchers at the University of Copenhagen analyzed old aerial photos to better understand mechanisms behind Antarctic ice shelf collapse. The study reveals that rising sea temperatures are a primary driver of collapse, contradicting previous assumptions.
Research reveals common patterns between ice shelf, sea ice, and ocean swell conditions prior to three large-scale iceberg calving events. Long periods of sea ice loss surrounding the ice shelves were found in the months leading up to the events.
Research on record-low years of Antarctic sea ice reveals warming of the Southern Ocean, increased ice-shelf calving, and stronger phytoplankton blooms. Low sea-ice area negatively affects krill and fish populations, ultimately impacting their predators and humans operating in Antarctica.
Researchers find watercourse meeting sub-ice-shelf ocean cavity up close, with temperature and salinity analysis revealing it's a calm body of water primarily fed by sea. The study also reveals that the watercourse fluctuates greatly over time, with flood events occurring approximately every ten years.
Researchers at the University of Leeds have found that one glacier in Antarctica is rapidly losing ice to its neighboring glacier due to changes in flow direction. This 'ice piracy' effect has been observed over less than 18 years, contrary to previous estimates of hundreds or thousands of years.
A new study compares tropical mountain ice cores to climate model simulations, revealing discrepancies in Earth's average temperature trends. Researchers found that ice core data and computer models match for polar regions like Greenland and Antarctica, but not for tropical mountains.
A recent study revealed a record-breaking increase in Antarctic Ice Sheet mass between 2021 and 2023, with significant mass gain observed in four key glaciers. This shift counters decades of mass loss, driven by anomalous precipitation accumulation.
Research finds that strengthened westerly winds enhance clockwise oceanic circulations, transporting warm seawater and causing accelerated ice sheet melting in East Antarctica. This study's findings improve future sea level rise projections.
Researchers studied Aurora Subglacial Basin's subglacial hydrology, finding dynamic rivers that change over time. This new insight may alter predictions of rising sea levels and the role of subglacial water in ice dynamics.
Researchers at Stanford University used machine learning to analyze high-resolution remote-sensing data of ice movements in Antarctica, gaining new insights into the fundamental physics governing the large-scale movements of the Antarctic ice sheet. The study reveals that most of the ice shelf is anisotropic, with different physical pr...
Researchers from Utrecht University studied icebergs' routes during rapid ice cap deterioration and found evidence of ancient material from Antarctica near South Orkney Island. The study suggests that Antarctica had an ice cap in the late Eocene, and large icebergs could survive in warm ocean conditions.
Global glacier melt accelerated over the last decade, with a 36% increase in meltwater compared to the previous decade. This poses significant risks to drinking water supplies, particularly in South America and Asia due to rising sea levels and increased flooding after the melt season.
Researchers generated a dataset of water flow beneath the entire Antarctic Ice Sheet, improving projections of sea level rise. The model predicts higher degrees of glacier melt and mass loss by the end of the century.
Researchers analyzed over 30 years of data to discover key influences on fast ice thickness in McMurdo Sound. They found that storm events, air temperature, and winter wind speed cause annual fluctuations in thickness.
Researchers found no increase in large iceberg sizes over the last half century, contradicting climate change expectations. Instead, frequent small calving events have dominated ice shelf loss, suggesting 'death by a thousand cuts',
Scientists reveal that the Antarctic ice sheet is more unstable than previously thought, with periods of sudden melting linked to changes in Earth's orbit. The study provides a glimpse into the potential behavior of Antarctica without the Greenland Ice Sheet, highlighting the urgent need for climate action.
Researchers at the University of Washington used a global climate model to simulate how ocean and air temperatures affect sea ice in the Southern Ocean. They found that warm Southern Ocean conditions and patterns in winds can explain 70% of the record-low winter sea ice extent in 2023, with similar predictions made for 2024.
A team of scientists, including Binghamton University's Molly Patterson, is drilling into the Ross Ice Shelf to retrieve geological records and gain insights into the ice sheet's response to global warming. The project aims to provide crucial data for adapting to sea-level rise and mitigating greenhouse gas emissions.
Researchers estimate a total ice mass loss of 3213 Gt, equivalent to 8.9 mm global sea level rise, from 1996 to 2021. The Antarctic Ice Sheet's mass loss accelerated since 2006, with an increase in annual losses.
A Kobe University research team analyzes the political repercussions of a proposed underwater curtain to protect Antarctic ice sheets from melting. The team highlights concerns around authority, sovereignty, and security, emphasizing the need for international cooperation to avoid conflict.
Scientists from the University of East Anglia have discovered a 50-metre-thick 'intrusion' of warm water under the Ross Ice Shelf, which has increased heat transport into the cavity by 45% over the last four decades. This finding suggests that climate change will likely lead to further melting and ice loss.
The Antarctic Peninsula has experienced a dramatic increase in vegetation cover over the last four decades, with satellite data showing an acceleration of 30% in recent years. This 'greening' trend is attributed to climate change and has significant implications for the region's ecosystem and environmental future.
New research using satellite technology tracks the movement of albatrosses and petrels, finding that they use sea ice-affected parts of the ocean for feeding and scavenging. The study suggests that Antarctica's shrinking sea ice could force seabirds to travel further or alter their food patterns, affecting ecosystems.
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 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.
Scientists have developed a state-of-the-art computational model predicting land, ice and global sea-level interactions. The model estimates that reducing greenhouse gas emissions could slow melting Antarctic ice enough to allow Earth uplift to partially stabilize the ice sheet and prevent some future sea-level rise.
A McGill-led study finds that swift action to lower emissions could prevent some of the most destructive impacts of climate change, particularly for coastal communities. The research suggests that reducing carbon emissions could reduce Antarctica's contribution to sea-level rise by up to 40%.
A new study suggests that the rising earth in Antarctica will impact future sea level rise, depending on how much global warming is controlled. If humans lower greenhouse gas emissions, upward shifts in solid earth could reduce Antarctica's contribution to sea level rise by about 40%, bolstering best-case scenarios for global sea level...
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.
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.
A new study reveals the geological footprint of persistent bottom currents within East Antarctic submarine canyons, carrying ocean heat to the continent. The discovery highlights the key role of these canyons in the melting of glaciers, contributing to sea level rise.
Researchers used AI to map slush on Antarctic ice shelves and found that 57% of all meltwater is held in slush, with a significant impact on ice shelf stability and sea level rise. This discovery could lead to more accurate predictions of ice sheet melting and collapse.
Scientists at British Antarctic Survey have identified a new tipping point in Antarctic ice sheet melting due to ocean water intrusion. This process, currently not included in models, could lead to significant underestimates of sea level rise and accelerated ice sheet melting.
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.
A UC Irvine-led team has discovered the 'vigorous melting' of West Antarctica's Thwaites Glacier using high-resolution satellite radar data. The study found that seawater intrusion causes ice to rise and fall, potentially requiring revised global sea level rise projections. The findings raise concerns for coastal communities worldwide.
A team of researchers found that the current rate of atmospheric carbon dioxide increase is 10 times faster than at any other point in the past 50,000 years. The study provides new insight into abrupt climate change periods and potential impacts of climate change today.
Researchers have uncovered a feedback loop that may be accelerating the melting of ice shelves in West Antarctica, contributing to global sea level rise. The study suggests that as ice shelves melt, they produce more freshwater, which strengthens an underwater current carrying warm water towards the ice shelf.
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.
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.
Researchers found that the West Antarctic Ice Sheet thinned by 450 meters in just under 200 years at the end of the Last Ice Age. The study sheds light on how quickly Antarctic ice could melt if temperatures continue to soar.
Two GEOMAR researchers will receive €2 million EU funding over five years to study the Antarctic ice sheet, carbon cycles, and deep-sea biodiversity. Their projects aim to improve climate projections and solve deep-sea mysteries.
A Cornell University-led team used an underwater robot to explore the ocean conditions beneath an Antarctic ice shelf, discovering a new circulation pattern involving a jet funneling water sideways through crevasses. The findings improve modeling of ice shelf melting and freezing rates, which can impact global sea-level rise.
The West Antarctic Ice Sheet is projected to melt at an increased rate, even under ambitious climate targets. Sea levels may rise by up to five meters, impacting millions of people living near the coast. The study's findings highlight the need for continued efforts to reduce greenhouse gas emissions and adapt to sea-level rise.
Over 71 of Antarctica's 162 ice shelves have reduced in volume over the past 25 years, with a net release of 7.5 trillion tonnes of meltwater into the oceans. The western side of Antarctica experienced significant ice loss, while the eastern side remained relatively stable.
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.
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...
Researchers have discovered clues about Antarctica's ice sheet formation in Mississippi mud, suggesting a 300,000-year brake on climate cooling. The study provides new insights into the Eocene-Oligocene transition, a significant climate event that had a major impact on Earth's history.