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m summers channels become increasingly connected redistributing meltwater from high to low elevations across the ice shelf channel location is controlled by ice shelf structure and annual extent is correlated with regional air temperature hide 12 oct 2026 temperature sensitivity of snow viscoplasticity evidence from controlled creep experiments louis védrine marius brun mathis bozon benoit laurent and pascal hagenmuller the cryosphere 20 5813 5828 https doi org 10 5194 tc 20 5813 2026 https doi org 10 5194 tc 20 5813 2026 2026 short summary short summary snow slowly compacts under its own weight and this process depends strongly on temperature but past estimates vary widely we developed a device to precisely control temperature and tested the same snow sample under different conditions we found two distinct temperature regimes and a stronger sensitivity than assumed in existing snowpack models improving how snow compaction is represented hide 12 oct 2026 boundary layer characteristics of a land terminating ice cliff turbulence measurements from the summit of kilimanjaro tanzania marie schroeder ivana stiperski michael winkler georg kaser jakob steiner jakob abermann georg wohlfahrt and rainer prinz egusphere https doi org 10 5194 egusphere 2026 5112 https doi org 10 5194 egusphere 2026 5112 2026 preprint under review for tc discussion open 0 comments short summary short summary steep ice cliffs can lose ice much faster than flat glacier surfaces yet little is known about how they interact with the air around them measurements at a 25 metre high ice cliff on kilimanjaro revealed distinct day night air flows and major differences in how heat is transported higher up heat is transported in an organised way while near the cliff base this exchange was more complex the cliff shape and its surroundings can strongly influence how heat reaches the ice and how it is lost hide 12 oct 2026 organic and inorganic proxy development for advective heat flux in a basal melt dominated glacial system petermann fjord north greenland joanna davies jennifer middleton david harning peter washam william d andrea and brendan reilly egusphere https doi org 10 5194 egusphere 2026 5321 https doi org 10 5194 egusphere 2026 5321 2026 preprint under review for tc discussion open 0 comments short summary short summary we evaluate the use of organic sea ice biomarkers and phytoplankton sterols and inorganic 10 be 230 th proxies from sediment cores in petermann fjord to investigate oceanic advection and glacial dynamics we find that that lateral advection enhanced by buoyant subglacial melt plays an important role in transporting these proxies beneath the ice shelf highlighting the potential to use a multi proxy approach to reconstruct advective heat flux patterns in basal melt dominated environments hide 12 oct 2026 increased future ice loss due to nested ice climate feedbacks if antarctic heatwaves intensify lena nicola johanna beckmann felicity s mccormack and ricarda winkelmann egusphere https doi org 10 5194 egusphere 2026 6030 https doi org 10 5194 egusphere 2026 6030 2026 preprint under review for tc discussion open 0 comments short summary short summary record breaking extreme events including heatwaves leading to surface melt and extreme snowfall have been observed in antarctica in recent years such extreme events are generally expected to become more frequent and intense with anthropogenic climate change here with a suite of numerical ice sheet simulations we explore the additional antarctic contribution to future sea level rise when including atmospheric temperature extremes of varying frequency and intensity in projections hide 09 oct 2026 antarctic sea ice response to meltwater due to antarctic ice sheet mass loss in a multi model ensemble andrew g pauling inga j smith torge martin jeff k ridley david p stevens max thomas rebecca l beadling christopher danek tore hattermann qian li john marshall morven muilwijk ariaan purich and neil c swart the cryosphere 20 5761 5783 https doi org 10 5194 tc 20 5761 2026 https doi org 10 5194 tc 20 5761 2026 2026 short summary short summary climate models typically do not include meltwater entering the southern ocean due to antarctic ice sheet mass loss previous work shows this meltwater drives sea ice growth but the varying responses have been difficult to compare across models we ran 11 climate models using the same meltwater input and found a wide range of sea ice responses depending on the background state in each model understanding this uncertainty in response is important for future projections of antarctic sea ice hide 08 oct 2026 an ensemble reconstruction of greenland ice sheet surface elevation for 1850 and 1980 ana carolina moraes luzardi sophie nowicki beata csatho jason briner mohammad salmani hui gao denis felikson josh cuzzone and kristin poinar egusphere https doi org 10 5194 egusphere 2026 5841 https doi org 10 5194 egusphere 2026 5841 2026 preprint under review for tc discussion open 0 comments short summary short summary before the satellite era observations of greenland ice sheet elevation were sparse in space and time we reconstruct ice sheet wide surface elevation for 1850 and 1980 using a 127 member ensemble the reconstructions agree with observations and historical evidence reveal patterns of thinning since the preindustrial era and provide a resource for evaluating and initializing ice sheet simulations hide 08 oct 2026 glacial lake outburst flood hazard assessment in the upper indus basin ladakh himalaya using remote sensing and hydrodynamic modeling jigmet angmo egusphere https doi org 10 5194 egusphere 2026 5906 https doi org 10 5194 egusphere 2026 5906 2026 preprint under review for tc discussion open 0 comments short summary short summary this study assesses glacial lake outburst flood glof hazard for three glacier fed lakes gya raru and panikhar in the upper indus basin ladakh lake area change was mapped with sentinel 2 imagery and gis and lake volume was estimated using empirical relationships two dimensional hec ras dam break simulations for 25 100 volume release scenarios gave peak discharge flow velocity flood depth and inundation extent worst case floods could damage downstream bridges and roads hide 07 oct 2026 temperature dependence of grain size in tibetan ice core zhengqiang he and baiqing xu the cryosphere 20 5745 5759 https doi org 10 5194 tc 20 5745 2026 https doi org 10 5194 tc 20 5745 2026 2026 short summary short summary we continuously measured ice crystal sizes along two ice cores from the tibetan plateau we found that the pattern of crystal size variation with depth is similar to that in polar ice cores crystal sizes increase abruptly in refrozen ice layers while they decrease in impurity rich bands notably in specific layers crystal size is linked to δ 18 o which means the crystal sizes in mountain glacier ice cores can retain temperature signals helping us understand past climate change hide 06 oct 2026 a 2020 permafrost distribution map of the qinghai tibet plateau yuhong chen zhuotong nan wenbiao tian yi zhao shuping zhao dongkai yang guifei jing and fujun niu the cryosphere 20 5697 5723 https doi org 10 5194 tc 20 5697 2026 https doi org 10 5194 tc 20 5697 2026 2026 short summary short summary this study presents a 1 km permafrost map of the qinghai tibet plateau for 2020 generated via a frost number model and space for time substitution permafrost covers 1 038 10 km² 39 35 a 1 82 decline since 2010 while seasonally frozen ground covers 1 466 10 km² 55 57 validated against boreholes the map achieves 0 84 accuracy kappa 0 58 this map offers a critical up to date baseline for cryospheric research hide 06 oct 2026 mechanisms and patterns of snow depth and land surface temperature interactions in arid mountains coupling coordination and lagged responses across xinjiang china haixing li xiaolong bao shiqi lu yi chu jun lu mengge xiao and xuelei lei the cryosphere 20 5725 5743 https doi org 10 5194 tc 20 5725 2026 https doi org 10 5194 tc 20 5725 2026 2026 short summary short summary mountain snow is a critical water source but its warming response is complex this study developed a new method to examine this in arid xinjiang mountains using long term satellite data revealing a three level control system and that a strong snow temperature link does not guarantee a healthy system it also provides a framework for water availability prediction and climate adaptation hide 06 oct 2026 simulating jökulhlaups from an ice marginal lake within a 2d model of subglacial drainage and basal sliding adam j hepburn sammie buzzard andrew j sole stephen j livingstone felix ng mathieu morlighem elizabeth a bagshaw caroline clason lisa craw christine f dow samuel doyle jonathan hawkins matthew peacey and robert storrar the cryosphere 20 5675 5696 https doi org 10 5194 tc 20 5675 2026 https doi org 10 5194 tc 20 5675 2026 2026 short summary short summary lakes at glacier margins can drain beneath the ice in devastating floods called jökulhlaups we present the first 2d model of jökulhlaup propagation first applying it to a synthetic glacier before then assessing its ability to reproduce an observed record of lake fill drain cycles in greenland our results match a 17 year record of flood timing but underpredicts peak discharge likely because we are missing certain physical processes our results hold promise for simulating jökulhlaups hide 06 oct 2026 permafrost thaw follows spatially organized nonlinear trajectories in ice wedge terrain katherine n braun jacob may and christian g andresen egusphere https doi org 10 5194 egusphere 2026 5192 https doi org 10 5194 egusphere 2026 5192 2026 preprint under review for tc discussion open 0 comments short summary short summary we used a time series of satellite images to track the progression of permafrost thaw in arctic alaska to assess why some areas are thawing more quickly and severely than others analyzing thaw over time revealed that the severity and timing of thaw is linked to geomorphic landforms while the overall pattern at this site was increasing thaw over time tracking thaw at fine spatial scales showed that there is high variability with thaw persisting initiating stabilizing and changing over time hide 05 oct 2026 seasonal evolution of suncup roughness describes broadband albedo decay on alpine snow francesca carletti nora helbig nander wever loïc brouet mathias bavay benjamin walter and michael lehning the cryosphere 20 5653 5673 https doi org 10 5194 tc 20 5653 2026 https doi org 10 5194 tc 20 5653 2026 2026 short summary short summary melting alpine snowfields develop cup shaped hollows that reduce how much sunlight the snow reflects accelerating melt over three seasons in the swiss alps we monitored how these hollows form and grow with a laser scanner two processes reduce reflectivity at the same time hollows trap light through internal reflections and meltwater washes dark particles into them because they are difficult to separate surface roughness alone emerges as a proxy for overall reflectivity loss hide 05 oct 2026 wave induced erosion and notch development at the fimbul ice shelf front wenjun lu lotte wendt behnam ghadimi shovon jubair dominique mouaze marianne font rémi lambert harvey goodwin geir moholdt raed lubbad and sveinung løset egusphere https doi org 10 5194 egusphere 2026 4610 https doi org 10 5194 egusphere 2026 4610 2026 preprint under review for tc discussion open 0 comments short summary short summary ocean waves carve a notch into the waterline of antarctic ice shelf fronts the notch is hidden from satellites yet it weakens the front and helps set how fast it retreats at the fimbul ice shelf we extend a standard wave erosion formula to irregular and breaking waves and drive it with reanalysis waves for the 2024 austral summer it predicts about 110 m of erosion while satellites show about 265 m of retreat so wave erosion alone does not explain the observed front retreat hide 02 oct 2026 gravity topography modeling of the denman glacier region using a geostatistical approach mareen lösing alan aitken michael field emma mackie and lu li the cryosphere 20 5629 5652 https doi org 10 5194 tc 20 5629 2026 https doi org 10 5194 tc 20 5629 2026 2026 short summary short summary subglacial topography controls how antarctic ice flows towards the ocean and responds to climate change in the denman shackleton region deep valleys connect the ice sheet interior to the coast denman glacier occupies one of the deepest and could contribute significantly to sea level rise combining new ground based gravity measurements with airborne data and statistical modelling reveals a more complex landscape than existing maps and a potential vulnerability to unstable retreat hide 02 oct 2026 diverse c band radiometric signatures of buried supraglacial lakes on the greenland ice sheet jillian steinmetz and riley culberg egusphere https doi org 10 5194 egusphere 2026 4964 https doi org 10 5194 egusphere 2026 4964 2026 preprint under review for tc discussion open 0 comments short summary short summary many studies use dark patches in satellite radar imagery to map buried lakes on the greenland ice sheet and infer how much water they store however this method has never been validated we use airborne ice penetrating radar to directly image buried lakes then analyze their signatures in satellite data we show that satellite systems can directly sense these buried lakes but they have very diverse expressions and as a result popular detection algorithms are likely to miss many lakes hide 02 oct 2026 a visco elastic phase field model for calving in ice daniel h richards robert j arthern and oliver j marsh egusphere https doi org 10 5194 egusphere 2026 5569 https doi org 10 5194 egusphere 2026 5569 2026 preprint under review for tc discussion open 1 comment short summary short summary iceberg calving is a major source of ice loss from antarctica yet predicting when and how this happens remains difficult we develop a mathematical model that simulates how ice deforms over years but also how it suddenly fractures our model can represent cracks on the surface and base of the ice our results show the rate of ice loss depends strongly on thickness the model can reproduce different ways in which icebergs calve allowing better predictions of future ice loss and sea level rise hide 02 oct 2026 greenland fjord processes have a depth dependent influence on predicted submarine melt rates emma f cameron tom r cowton alexander t bradley and paul r holland egusphere https doi org 10 5194 egusphere 2026 5769 https doi org 10 5194 egusphere 2026 5769 2026 preprint under review for tc discussion open 0 comments short summary short summary many of greenland s glaciers end in fjords where they are melted by the ocean fjords are too small to resolve in ocean models so melt rates are often estimated from offshore temperatures we compared temperatures in 38...