Antarctic Climate and Ice ChangeAntarctic Climate and Ice ChangeCoverage from The Conversation, Phys, and others
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Antarctic ice change reflects interacting atmospheric, oceanic, and ice-sheet processes.
Warm air and ocean water can suppress sea-ice formation, while deeper ocean water reaching glacier undersides can accelerate melting and ice flow; snowfall may temporarily offset losses in some regions. West Antarctica and Thwaites Glacier are central to long-term projections because the timing and pace of future ice loss remain difficult to determine. Antarctic ice loss also affects sea levels unevenly around the world, making regional consequences distinct from the global average.
It adds distinct Thwaites observations from glacier-related seismic events and shows why the timing and scale of ice loss remain uncertain.
ScienceDaily / Thanh-Son Pham
Key Issues
01
Persistently low Antarctic sea ice
Antarctic sea ice remains exceptionally low: the 2026 winter peak was the third-smallest in the 48-year satellite record, after sharp declines and 2023 record lows. Ocean heat and wind-driven changes are proposed contributors, but the observations do not yet establish a structural shift or settle attribution.
Drawn from 4 articles
02
Ocean heat threatens glacier stability
Warm deep water is moving toward Antarctica and threatens ice-shelf stability; research also attributes part of Pine Island Glacier’s retreat to human-driven warming. Observations of Thwaites indicate glacier movement and possible ocean-related destabilization, while the consequences for future ice loss remain uncertain.
Drawn from 5 articles
03
Uncertain pace and scale of ice loss
The persistence and causes of low Antarctic sea ice remain unresolved, and the effects of short-term ocean changes on Thwaites are not fully understood. Sparse observations and uncertain glacier behavior limit confidence in projections of the timing and scale of future ice loss and sea-level impacts.
Drawn from 3 articles
Key Numbers
12.5 trillion tons
ice melted from Greenland and Antarctic glaciers
since 1979
“About 12.5 trillion tons of ice from glaciers in Greenland and Antarctica have melted since 1979”
KSL.com and 1 other article
five-sixths
share of ice melt attributed to warmer ocean water rather than hotter air
Greenland and Antarctica
“About five-sixths of the melt did not come from hotter air, but from warmer ocean water eroding the ice sheets from below and along their sides as glaciers flow into the oceans.”
Mercury News and 1 other article
3.1 centimeters
global sea-level rise attributed to melted ice
about · since 1979
“The melted ice produced nearly 3 quadrillion gallons of water and contributed about 1.2 inches, or 3.1 centimeters, to global sea-level rise since 1979.”
NBC News and 1 other article
2018 to 2020
most active seismic-event period
coincided with accelerated movement of Thwaites's ice tongue
“The most active period, from 2018 to 2020, coincided with accelerated movement of the glacier’s ice tongue toward the sea, a speed-up independently confirmed by satellite observations.”
ScienceDaily
245 of 362 events
events located near Thwaites Glacier's marine end
among all detected glacier-related seismic events
“About two-thirds of the detected events—245 of 362—were located near the marine end of Thwaites.”
ScienceDaily
Looking Back
306 Day Timeline
Articles published over time. Hover any bar for the period and its article count.
Nov 28 '25
Jan 16 '26
Mar 6 '26
May 1 '26
Jun 19 '26
Aug 7 '26
Sep 25 '26
The Story So Far
No material change
No material change is established since the prior state; there are no new-member articles to identify a new development.
Previously
The topic centers on unusually low Antarctic sea ice, particularly a large winter deficit in the Bellingshausen Sea off the West Antarctic Peninsula, alongside evidence of broader changes in the Southern Ocean. Scientists are investigating how warm ocean water, winds, and atmospheric circulation affect sea-ice formation, and whether reduced coastal ice leaves ice shelves and glaciers such as Thwaites and Pine Island more exposed. Potential consequences for glacier loss, sea level, and ecosystems are significant, but their timing and scale remain uncertain.
Researchers report Antarctic wave-driven sea-ice flooding and algal darkening can accelerate summer thinning, suggesting a missing feedback process for climate models.
A scientific study reports Antarctic sea ice declines since 2015 through Southern Ocean stratification loss, enabling deep ocean heat to melt sea ice and disrupt ecosystems.
Science study attributes East Antarctica ice-sheet formation to CO2 decline plus mantle-driven uplift that enabled year-round snow and glacier expansion, unlike the Arctic.
Esperanza Base in Antarctica recorded a June record 15.4C on June 6, while Marambio and San Martin reported higher-than-before winter temperatures linked to ongoing regional warming.
Shin Sugiyama and colleagues directly measured meltwater-driven basal lubrication at Langhovde Glacier in East Antarctica, increasing sliding after intense melt and January 2022 rainfall.
Nature Communications reports Antarctic climate-model projections of tenfold surface melt increases and expanding melt area by 2100 under high emissions, with implications for sea-level rise in New Zealand.
University of Southampton researchers report wind-driven upwelling and mixing in the Southern Ocean lowered Antarctic sea ice since about 2013, intensifying through 2023.
Stanford University researchers report that Antarctic sea ice decline around 2016 stems from precipitation-driven heat trapping followed by wind-driven upwelling of subsurface ocean heat.
Scientists estimate greenhouse-gas warming contributed about 4 km of Pine Island Glacier retreat since 1940 using climate models, machine learning, satellite data, and sediment records in West Antarctica.
Researchers from the University of Southampton and partner institutions reported that mantle-driven uplift in East Antarctica enabled major glaciation around 34 million years ago.
Ted Scambos linked unusually low west Antarctic Peninsula sea ice in June to warm air and deep ocean heat, warning of accelerated Thwaites Glacier melt.
Ted Scambos discusses unusual Antarctic west-coast sea-ice loss in June and explains subsurface ocean warming as the primary long-term threat to West Antarctic ice and sea level.
Ted Scambos explains that unusual June sea-ice loss on West Antarctica reflects warm winds and ocean heating, with Thwaites Glacier a key uncertainty for future sea-level rise.
Ted Scambos discusses unusually missing sea ice near the Antarctic Peninsula in June, linking wind and warm ocean water to ongoing glacier-melt risk and long-term sea-level rise.
Ted Scambos discusses June sea-ice deficits near Antarctica's west coast, linking warm air and deep ocean heat to accelerating West Antarctic glacier melt and sea-level rise risk.
Ted Scambos described unusual low midwinter sea ice on West Antarctica and deep-ocean warming that accelerates Thwaites Glacier, increasing sea-level rise risk.
Ted Scambos and Antarctic researchers reported a June France-sized west Antarctic Peninsula sea ice deficit driven by warm winds and ocean water, with longer-term glacier melt risk.
Ted Scambos explains unusually low Antarctic sea ice in June and how warm ocean water could accelerate West Antarctica glacier loss and nonuniform sea-level rise.
Ted Scambos discusses unusual June Antarctic sea-ice loss driven by warm winds and ocean water, with Thwaites Glacier identified as a major sea-level-rise uncertainty.
Scientists at King's College London and the British Antarctic Survey attribute Pine Island Glacier retreat during the 20th century to human-driven greenhouse gas emissions and ocean warming.
Esperanza base measurements in Antarctica on 6 June recorded a 15.4C winter peak, exceeding a 1998 record and reinforcing concerns about rapid climate-driven glacier risk.
Researchers at IBS Center for Climate Physics, Pusan National University, report Antarctic ice-sheet sensitivity increased after the Mid-Pleistocene Transition about one million years ago, using paleoclimate simulations and an ice-sheet model.
Researchers using transect and Argo float observations find deep ocean heat has shifted toward Antarctica in recent decades, increasing risk to Antarctic ice sheets and future sea-level rise.
Researchers used CMIP6 GCMs and ISMIP6-calibrated ice-sheet models in the 2020s to project Antarctic mass loss and sea-level contribution through 2300 across emission scenarios in Antarctica.
The Columbia Climate School reported on February 2, 2026, that University of Oldenburg researchers linked West Antarctic ice-sheet retreat to reduced Southern Ocean carbon uptake, with no heat pump relevance.
A British Antarctic Survey-led team reports that Antarctic glacier-calving internal tsunamis significantly enhance Southern Ocean mixing and ice melt, with no mention of heat-pump systems.
In East Antarctica during July to August 2024, record winter warmth up to 28°C above average was traced to altered atmospheric circulation and increased likelihood from human-caused climate change.
University of Southampton researchers link record-low Antarctic sea ice in 2023 to wind-driven transport and mixing of deep Southern Ocean heat since 2013.
Researchers using observational temperature reconstructions report marked climate change across interior Antarctica, with stronger peninsula and West Antarctica warming and CMIP6 warming overestimation.
National Snow and Ice Data Center reported record-low Arctic winter sea ice growth as scientists cited widespread March heat extremes across multiple regions.
South Korean climate scientist Min Seung-ki announced in February 2026 at POSTECH a recalibrated model projecting nearly ice-free Arctic conditions as early as the 2030s.
Researchers from PIK and NORCE warn in 2025 that about 0.25 C of deep ocean warming around Antarctica could trigger West Antarctic Ice Sheet collapse, risking roughly four meters of long-term sea-level rise.
The National Snow and Ice Data Center reported that Antarctic sea ice reached a preliminary winter peak of 17.59 million square kilometres on 14 September 2026, the third-smallest maximum in the satellite record.
Canadian and Chilean scientists completed a 14-day Antarctica expedition returning to Punta Arenas, Chile with multi-beam ocean and sediment data on accelerating glacier retreat.
Scientists warn that MISI, MICI, and SEMI could accelerate Greenland and Antarctic ice-sheet retreat, raising global sea levels and increasing coastal flooding risk this century.
An international polar science team reported that Greenland and Antarctica lost about 12.5 trillion tons of ice since 1979, raising global sea levels by roughly one inch worldwide.
An international polar science collaboration found that Greenland and Antarctica lost 12.5 trillion tons of ice since 1979, raising global sea levels by about 3.1 centimeters.
An international polar science team led by the European Space Agency found that Greenland and Antarctica lost 12.5 trillion tons of ice from 1979 to 2023, raising global sea levels by 1.2 inches.
9/16/2026 • Climate Science & Impacts • General
The Conversation / Matt King, Nancy A.N. Bertler72
Antarctic researchers are calling for a multinational ocean-and-ice survey in coming years to measure warming-driven retreat risk in East Antarctica's Wilkes Subglacial Basin.
David Holland and collaborators are measuring glaciers and surrounding waters in Greenland and Antarctica to evaluate sea-level risks and possible interventions to slow ice loss.
Satellite data show missing Bellingshausen Sea winter sea ice during June, coinciding with extreme Antarctic Peninsula warming and raising risks for ice shelves and marine ecosystems.
University of Leeds researchers report satellite evidence that freshwater meltwater lakes at Greenland glacier fronts accelerate glacier flow and may increase future sea-level rise.
Researchers detected 362 previously overlooked glacier-related seismic events in Antarctica from 2010 to 2023, including 245 near Thwaites Glacier during accelerated flow toward the ocean.
European Space Agency Sentinel-1 observations documented a 76-square-kilometer ice island calving from Petermann Glacier in northwest Greenland on August 4, 2026.
Ted Scambos links unusual June sea-ice loss on Antarctica's west coast to warm winds and ocean water, warning that deep-ocean melting of Thwaites Glacier could drive long-term sea-level rise.
Ted Scambos discussed unusual midwinter sea-ice loss along Antarctica's west coast and deeper-ocean glacier melt affecting Thwaites and future sea-level rise risk in June.
Ted Scambos discusses unusually low Antarctic sea ice in June and ocean-driven glacier melting, focusing on West Antarctica and non-uniform sea-level rise risk.
UC Boulder scientist Ted Scambos discussed unusually low Antarctic sea ice and ocean-driven glacier melt risks during an interview on June conditions and long-term sea-level rise.
Ted Scambos discusses June observations of unusually low Antarctic sea ice and long-term West Antarctica sea-level rise risks linked to warmer ocean water.
Ted Scambos linked June sea-ice losses on the Antarctic Peninsula to warm winds and deep ocean heat, highlighting Thwaites Glacier as a key sea-level rise uncertainty.
Scientists report unusually missing sea ice along Antarctica's west coast in June, tied to warm South Pacific winds and ocean water, raising risks from Thwaites Glacier melt and nonuniform sea-level rise.
Ted Scambos said June observations showed unusually missing sea ice on the West Antarctic coast, linked to warm winds and ocean heat and raising sea-level rise concerns.
Ted Scambos described unusual midwinter sea-ice loss on West Antarctica in 2020s conditions, attributing it to warm winds and warm ocean water that increase snowfall but also accelerate glacier melt and future nonuniform sea-level rise risk.
Ted Scambos discusses unusual June sea-ice loss on Antarctica's west coast and deep ocean-driven glacier melt that may shape long-term, regionally varied sea-level rise risks.
Scientists documented unusually low midwinter sea ice on Antarctica's west coast in June, linking warm winds and ocean heat to accelerating glacier-melt risks and regional sea-level rise impacts.
Scientists report an unusually large midwinter sea-ice deficit near the Antarctic Peninsula and link conditions to warm South Pacific air and warm ocean water that increase glacier melting.
Ted Scambos links unusual West Antarctic Peninsula sea-ice loss to warm air and ocean conditions, warning of long-term, regionally uneven sea-level rise risk centered on Thwaites Glacier.
Ted Scambos reports unusual June sea-ice loss on Antarctica's west coast linked to warm South Pacific winds and ocean water, with Thwaites Glacier as a key sea-level rise uncertainty.
Scientists report West Antarctica winter sea ice did not refreeze after a heatwave in 2025, based on satellite observations and linked warming factors that affect sea-level rise risk.
Nearly 40 scientists on the Araon studied Thwaites Glacier in Antarctica to quantify warm-ocean melting and associated sea-level rise risk during an Antarctic expedition.
Robert Larter of the British Antarctic Survey warns that Thwaites Glacier's ice-shelf breakup could accelerate sea-level rise and coastal flooding during the coming year.
Researchers from Columbia University and partner institutions reported in January 2026 that coastal Greenland sea levels are projected to fall due to rapid land uplift and changing gravity.
A study found that 203 glaciers in the western Antarctic Peninsula contributed 0.74 centimeters to sea-level rise from 1992 to 2020 despite rising surface mass balance since 1980.
Thwaites Glacier retreat in Antarctica is measurable and driven by ocean water intrusions, while near-term collapse claims are criticized as unsupported by data and uncertainty.
A modeling study explains Antarctic sea-ice shifts as Southern Ocean heat and wind-driven upwelling that can sustain low ice conditions, with 2023 record lows consistent with the mechanism.
Arctic sea ice hit its lowest winter peak measured during record March heat across the USA, Mexico, Australia, Northern Africa, and parts of Northern Europe, while Antarctica saw a record cold March day.
University of Gothenburg researchers attribute rapid Antarctic sea-ice decline starting in late 2015 to 2015 Southern Ocean storms thinning the cold Winter Water layer.
Walt Meier reports record-low March Arctic sea ice coverage since 1979, describing reduced albedo, faster Arctic warming, and possible extreme weather impacts.
Researchers found that Greenland and Antarctica lost 12.5 trillion tonnes of ice since 1979, raising global sea levels by about 3.2 centimetres through increased glacier discharge.
An international team in 2026 is deploying sensors at Antarctica's Thwaites Glacier and Amundsen Sea to evaluate a proposed seabed curtain geoengineering structure intended to slow glacier-driven sea-level rise.
Researchers at Columbia University's Lamont-Doherty Earth Observatory report in Nature Communications that glacial isostatic adjustment will lower Greenland's local sea levels by 2100.
An international research team documented Petermann Glacier's 76.4-square-kilometer iceberg calving in northwest Greenland on August 4, 2026, while Canadian officials assessed maritime risks.
Experts report near-total winter sea-ice absence in the Bellingshausen Sea during June, coinciding with Antarctic Peninsula heat and raising ecosystem and sea-level risks.
Raymond Zhong and Chang W. Lee reported from Antarctica on an expedition aboard the South Korean icebreaker Araon studying Thwaites Glacier melt mechanisms.
South Korean researchers drilled beneath the Thwaites Glacier in January 2022 aboard Araon and found warm, turbulent subglacial water linked to future sea-level rise risk.
Erica Lucas and colleagues at the University of California, Santa Cruz project larger ice-free Antarctica land exposure by 2300 using glacial isostatic adjustment, with potential governance impacts for Argentina, Chile, and the United Kingdom.
Scientists retrieved a 23-million-year sediment record from beneath the Ross Ice Shelf, linking West Antarctica retreat to modest past warming and projecting accelerating sea-level rise from human-caused warming.
An international polar science collaboration found that Greenland and Antarctica lost about 12.5 trillion tons of ice since 1979, raising global sea levels by approximately 3.1 centimeters.
Researchers at a polar climate session examined Antarctic atmospheric processes, sea ice loss, precipitation extremes, and future ice shelf melt across Antarctica and the Southern Ocean.
Scientists from Newcastle University and the British Antarctic Survey modeled 2100 outcomes for the Antarctic Peninsula, finding higher emissions will accelerate ocean warming, ice loss, and ecosystem collapse.
Researchers mapped the East Antarctic Fan-shaped Basin Province beneath East Antarctica, linking Wilkes, Aurora, and Lake Vostok and suggesting tectonic control on ice-sheet movement.
Researchers found that climate warming and anthropogenic emissions increased mercury accumulation in Antarctic Peninsula seafloor sediments through glacier release and expanded air-sea exchange.
Scientists report rising Antarctic extreme weather, including rain at Rothera and anomalously warm conditions at Concordia, worsening research access and ecosystems.
Scientists using Fimbulisen Ice Shelf observations and modeling found underside channels can amplify melt under warmer ocean water, affecting Antarctic stability and sea-level projections.
National Snow and Ice Data Center reported record-low Arctic sea ice winter maximum on March 15 in 2020s, tying last year's satellite minimum and indicating earlier melt onset.
UNSW, ANU, and Australian Antarctic Division researchers warn in 2025 that accelerating Antarctic ice and ocean changes threaten global sea-level rise and ecosystem collapse.
Researchers in Antarctica reported June temperatures well above average at Trinity Peninsula and Collins glacier, with Thwaites glacier risks tied to warmer subsurface waters.
Geological forces in Antarctica, including geothermal heat and volcanic activity, are argued to be undermeasured drivers of glacial and sea-ice change, requiring expanded monitoring.
Scientists in Antarctica drilled two kilometers through the ice sheet to access subglacial Lake Vostok, revealing scientific opportunities and ethical concerns about future uses of deep-ice manipulation techniques.
2/2/2026 • Policy, Politics & Governance • General
University of Wisconsin-Milwaukee researchers studying Phyllophora antarctica in McMurdo Sound find sea-ice loss is associated with shifts in algae diversity and population connectivity.