Articles tagged with Glaciers
A new study has found that six massive glaciers in West Antarctica are losing ice at an unprecedented rate, causing global sea levels to rise. The amount of ice draining from these glaciers increased by 77 percent between 1973 and 2013, with Pine Island Glacier accelerating by 75 percent over the same period.
Glacial chronologies during MIS 3 differ throughout the Tibetan Plateau, with advances on both slopes of the Nyainqentanglha being synchronous but not synchronized with Northern Hemisphere ice sheet. The study suggests a possible linkage between these events and North Atlantic cooling.
Researchers use years of data to understand how glaciers changed over time as climate has changed, providing insights into future glacier melting. The study's findings have significant implications for understanding global environmental change and planning protection efforts.
Researchers found that the northeast Greenland ice sheet is no longer stable and contributing to global sea level rise. The ice stream's retreat accelerated by 20 kilometers over the last decade, suggesting a positive feedback mechanism that could increase future sea level rise.
Scientists found that Northeast Greenland Ice Stream started losing mass in 2003 due to localized temperature increase, contradicting previous predictions. The study suggests this region is sensitive to climate changes and could contribute significantly to global sea-level rise.
Recent AGU publications explore the surface dynamics of Titan's second-largest lake, Ligeia Mare. Researchers found that the lake's surface is flat, suggesting no waves or wind in the region. Additionally, new research on U-shaped glacial valleys suggests a tectonic stress feedback loop played a crucial role in their formation.
New research using NASA data shows that only a small number of Greenland's largest glaciers are responsible for the majority of ice discharge into the ocean. The study used satellite observations and ice thickness measurements to calculate ice flow rates, providing a clearer picture of how glacier dynamics affect the Greenland Ice Sheet.
This article covers various geology topics including Mars exploration, environmental lead poisoning, earthquake hazards, the Indus Civilization collapse due to aridification event, end-Cretaceous mass extinction analysis using clumped isotope paleothermometry, and geological events such as the Tibetan Plateau's reorganization.
A Dartmouth-led study finds that temperature, not snowfall, is driving the fluctuating size of Peru's Quelccaya Ice Cap, a symbol for global climate change. The research uses field mapping and ice core analysis to determine that temperature was the primary driver of glacial expansion and retreat.
A study of Pine Island Glacier reveals it experienced rapid thinning 8,000 years ago at an average rate comparable to modern-day melting rates. This indicates that modern-day melting could last several more decades or even centuries.
Scientists found that Pine Island Glacier thinned rapidly 8000 years ago, similar to its current rate of thinning. This suggests the glacier may continue to lose mass for decades to come due to ocean-driven melting.
Articles explore geological processes such as erosion, deposition, and sedimentation, shedding light on catastrophic outburst floods and sediment routing systems. New findings from the Eocene Escanilla Formation and the Ohanapecosh Formation provide insights into facies architecture and sediment grain size variation.
The Greenland Ice Sheet is experiencing rapid ice loss, driven by ocean warming and increased surface melting. This phenomenon can lead to fresh water input into the North Atlantic Ocean, potentially disrupting global climate circulation patterns.
Jakobshavn Isbrå reaches unprecedented summer speeds of over 46m per day, exceeding 4 times the speed of the 1990s. The glacier's increasing speed contributes to sea-level rise as it adds more ice to the ocean.
Scientists reveal that Tibetan glaciers are losing mass, with a clear loss of around 16 gigatons per year. However, some glaciers in the central and north-western part of the plateau have grown in mass, contradicting previous data.
A new study suggests that El Nino events are tied to the rapid melting of Antarctica's Pine Island Glacier. The glacier's ice shelf has been thinned nearly continuously since observations began in the 1970s. Under certain conditions, a thick layer of warm water surrounding the continent can flood the glacier margin and accelerate melt.
A new study reveals that Pine Island Glacier is highly sensitive to climatic and oceanic changes, with fluctuations in ocean heat causing significant melting. The glacier's response to climate variability has been underestimated, suggesting a more complex interplay between geological, oceanographic, and climatic processes.
Scientists have discovered new evidence that the Italian Alps are warming at an unprecedented rate. A team of glaciologists drilling ice cores found a 2,600-year-old larch tree leaf that suggests the glacier was once below-freezing but now has layers at the melting point throughout the year.
Researchers study fossil estuaries, a 'natural wind tunnel' experiment on the Chinese Loess Plateau, frictional melting of rocks in water, glacial moraines in Colorado, and topographic data from Venus. These studies explore ecosystem stability, aeolian sediments, fault frictional properties, and volcanic lightning.
Scientists recorded and identified the sizzling sound of glacier ice as it melts, a phenomenon caused by trapped air bubbles escaping from the disappearing ice. This discovery could help researchers better monitor polar environments and track changes in glacier melt rates using underwater hydrophone recordings.
A new technique using Arctic fossil records reveals that Greenland's ice sheet was smaller between 3,000-5,000 years ago, with warmest land and ocean conditions during this period. This finding suggests the ice sheet may respond to ocean temperatures, providing a clue to future climate change.
Scientists have gained new insight into how glacier movement is affected by melting ice in summer, enabling more accurate predictions of sea level rise. The study found that fast summer ice flow caused by significant melting is cancelled out by slower motion the following winter.
A Dartmouth-led team has developed a more accurate method to date boulders deposited by tropical glaciers, yielding older ages and changing previous research on climate's impact. The new production rate suggests glaciers expanded during cooler and drier times in the tropics.
Narrow stripes of dirt and rock beneath massive Antarctic glaciers create friction zones that slow the flow of ice toward the sea. The process is strongly affected by how water infiltrates the space between the ice sheet and the bedrock, researchers found.
Biologists at the University of South Carolina have discovered a rare shark species, Sphyrna gilberti, which has a distinct genetic signature and is found only in the Santee and Pee Dee river systems. The discovery highlights the fragility of shark diversity and underscores the importance of studying evolutionary history.
Research reveals selective glacial erosion in Norway's passive margin, links gold to pyrite in carbon-rich sediments, and analyzes seawater Sr/Ca ratios. These findings advance our understanding of Earth's geological history and plate tectonics.
Researchers measured undersea current of warm water driven by fresh water from the melting glacier. The measurements will be used with physical and computer models to predict future changes in the ice shelf and glacial melt rates.
A team led by NASA's Robert Bindschadler measures the rate at which warm ocean water melts Antarctica's Pine Island Glacier ice shelf from underneath. The study reveals melt rates of up to 2.36 inches per day, with implications for sea level rise and glacier stability.
Scientists have measured ice-shelf melting rates and processes beneath Pine Island Glacier, revealing a critical need to understand channelized melting under massive glaciers. The findings could lead to the break-up of the ice shelf and contribute to global sea-level rise.
Researchers found that ocean warming is melting the Pine Island Glacier's floating ice shelf, causing rapid movement of glaciers in Antarctica. This process can lead to increased sea level rise as more ice is added to the mass of Antarctic glaciers.
Researchers found that coal soot reduced Alpine glacier ice by shrinking them, despite cooler temperatures. European glaciers retreated an average of nearly 1 kilometer between 1860 and 1930 due to industrialization, contradicting previous natural climate shift assumptions.
Scientists have uncovered strong evidence that soot from industrial Europe caused the abrupt retreat of mountain glaciers in the European Alps. The research, published in Proceedings of the National Academy of Sciences, resolves a longstanding debate about why the Alps glaciers retreated beginning in the 1860s.
New research from Durham University reveals that the East Antarctic Ice Sheet may be more susceptible to changes in air temperatures and sea-ice than previously believed. The study found rapid and synchronised periods of advance and retreat among 175 glaciers along the coastline, coinciding with cooling and warming patterns.
A study by University of Pennsylvania geologist Jane Willenbring and colleagues found that the local glacial maximum in southern Europe occurred earlier than expected, around 26,000 years ago. This discovery provides new insights into how regional climates have varied over time and could lead to more accurate global climate models.
The new articles examine ancient whale coprolites in central Italy, fault slickensides in San Francisco, and earthquake hazards in Cascadia. They also discuss the formation of silica gel during fault slip and the microstructures of superplastically deformed materials.
Researchers investigate the solid Earth's influence on sea level changes, divergent geologic histories in North America, and 'ghost glaciers' in Greenland. The study also examines the Picuris Orogeny in New Mexico and the Cryogenian Perry Canyon Formation in Utah.
Researchers discovered that soil microbial biomass and fungal activity increased as the soil aged, with correlations between microbial respiration and soil nitrogen content indicating a community-wide influence on the environment. Yellow mountain avens, which support nitrogen fixation, took 40 years to impact soil microbial biomass.
Researchers have developed a new model that simulates the calving process of icebergs, predicting areas at risk of rapid disintegration due to climate change. The model suggests that stretches of ice on Antarctica and Greenland are vulnerable to catastrophic collapse, potentially exacerbating sea level rise over the next 100 years.
Supraglacial lakes' draining mechanisms, which affect ice velocity and extent, were studied in West Greenland. The findings show that rapid draining accelerates glacial movement, while slow draining increases its pace, with implications for sea-level rise.
Researchers gathered extensive data using airborne and orbiting instruments to study the calving process of Pine Island Glacier. The analysis promises to improve understanding of how glaciers calve and shed light on future ice sheet changes.
A new study suggests that the Greenland ice sheet's contribution to sea-level rise will continue to increase as surface melting becomes more significant. This change is driven by the rapid retreat of outlet glaciers and strong warming-induced surface melting, which removes ice before it can reach the marine margin.
Researchers have used innovative radar analysis to accurately image the vast subglacial water system under Thwaites Glacier, a Florida-sized outlet glacier in Antarctica. The findings suggest that the dynamics of this water system may play a crucial role in predicting the fate of the glacier.
Researchers investigate strain localization, atmospheric CO2, and ultra-high pressure metamorphism, shedding light on geological phenomena. Intensified Southern Hemisphere Westerlies are found to regulate atmospheric CO2 during the last deglaciation, highlighting critical parameters for the global carbon cycle.
Two UAF scientists contributed to a global study on glacier mass losses and their impact on rising sea levels. Their findings suggest that Alaskan glaciers alone explain one-third of the current sea-level rise, making Alaska a top contributor to global sea level.
Researchers John Isbell and Erik Gulbranson study ancient climate shifts to understand modern-day drastic climate change. They find evidence of 22 individual ice sheets in Gondwana, suggesting dramatic temperature swings and atmospheric CO2 levels fluctuations.
A new study reveals that glacier melting is responsible for about one-third of the observed sea-level rise, with other factors like ice sheets and thermal expansion contributing equally. The research used satellite data from NASA's ICESat and GRACE missions to calculate glacier mass changes globally.
A new study found that the world's glaciers lost an average of roughly 260 billion metric tons of ice annually between 2003 and 2009, contributing to ocean rise of 0.03 inches or 0.7 millimeters per year. This loss exceeds previous estimates, highlighting the crucial role of smaller ice bodies in global sea level rise.
A new study using NASA satellite data found that glaciers outside of Greenland and Antarctica lost an average of 571 trillion pounds of mass every year, contributing to a 0.03-inch-per-year rise in sea levels. This is equal to about 30% of the total observed global sea level rise during the same period.
Glaciers in the Mount Everest region have shrunk by 13% in the last 50 years, with snowlines shifted upward by 180 meters. The researchers suspect human-generated greenhouse gases are causing climate change, but need to establish a firm connection.
A new study models iceberg production by Greenland glaciers, finding that fjord shape and terrain below the ice significantly affect their movement. The research suggests that climate change will lead to an average loss of 30-47Gt of ice from these glaciers over the 21st century.
IceBridge team measures sea ice, maps sub-ice bedrock, and gathers data on Greenland's glaciers, improving computer models of sea and land ice. The campaign aims to collect as much data as possible to understand the changing state of Arctic sea ice.
Researchers analyzed a new ice core from Antarctica, finding that recent glacier changes are at the 'upper bound' of normal. The study suggests that rapid thinning and warming in the region cannot be confidently attributed to human-caused global warming.
The study reveals that peripheral glaciers in Greenland are losing mass at a rate of up to 50 Gigatons per year, contributing to around 15-20% of sea-level rise. This is higher than expected and more significant than the ice sheet alone.
Recent research highlights a catastrophic acceleration in Canadian Arctic glacier melt, with projections suggesting up to 18% mass loss by the end of the century. Climate change is deemed effectively irreversible, according to model simulations.
A new study by Woods Hole Oceanographic Institution identifies glaciers as a significant source of iron to the North Atlantic Ocean. The research found high concentrations of dissolved iron in meltwater from glaciers and ice sheets, which may fuel plankton growth during spring and summer.
Research predicts 20% of Canadian Arctic glaciers will melt by end of century, causing irreparable ice loss and sea-level rise. The study's results show that climate change reinforces warming, making it highly likely that glaciers will melt at alarming rate.
A team of geoscientists from the University of Arizona led by Stuart N. Thomson discovered that East Antarctica's landscape changed dramatically when big glaciers appeared there, carving deep valleys quickly. The research used sediment cores to analyze minerals and determine the rate of erosion over time.
A new study projects that global sea-level rise will not be uniform, with certain regions experiencing higher rates of rise. The team used sophisticated computer modeling to show how ice loss from glaciers and ice sheets will impact regional sea levels, particularly in the Equatorial Pacific Ocean.
Researchers studied the origin of freshwater bodies in the New Jersey shelf and found it comes from modern rainwater, seawater, and a brine from deep sediments. They also investigated active methane formation beneath the seafloor and its potential impact on greenhouse gas emissions during ice ages.
Glaciers in the tropical Andes have been retreating at an increasing rate since the 1970s, with a 30-50% shrinkage since then. Climate change is blamed for this rapid melting, which could affect water supply to Andean populations.