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1
Analytic Solutions to Reflection-Transmission Problem of Interface in Anisotropic Ice Sheet
Published 2020-01-01“…The rheology and evolution of the polar ice sheet are deeply influenced by the anisotropy of ice crystals. …”
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2
A topographically controlled tipping point for complete Greenland ice sheet melt
Published 2025-01-01“…<i>no SMB–elevation feedback</i>) in this relatively confined region, the ice sheet retreat is halted and nearly complete GrIS melt is prevented even though the initial SMB forcing is past the threshold. …”
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3
Sustainability of regional Antarctic ice sheets under late Eocene seasonal atmospheric conditions
Published 2025-01-01“…These phases signal a shift from the warm middle to late Eocene greenhouse climate to cooler conditions, with global surface air temperatures decreasing by 3–5 °C and the emergence of the first continent-wide Antarctic ice sheet (AIS). While ice sheet modelling suggests that ice sheet growth can be triggered by declining <span class="inline-formula"><i>p</i></span>CO<span class="inline-formula"><sub>2</sub></span>, it remains unclear how this transition was initiated, particularly the first growth phase that appears to be related to oceanic and atmospheric cooling rather than ice sheet growth. …”
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4
The impacts of reduced ice sheets, vegetation, and elevated CO2 on future Arctic climates
Published 2024-12-01“…This study investigates the climatic response of the Arctic to key factors that could shape future climate scenarios: significantly reduced ice sheets, changes in vegetation, and elevated CO2 levels. …”
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5
East Antarctic Ice Sheet variability in the central Transantarctic Mountains since the mid Miocene
Published 2025-01-01“…<p>The response of the East Antarctic Ice Sheet to warmer-than-present climate conditions has direct implications for projections of future sea level, ocean circulation, and global radiative forcing. …”
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6
Diverse behaviors of marine ice sheets in response to temporal variability of the atmospheric and basal conditions
Published 2024-01-01Subjects: Get full text
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7
ISMIP6-based Antarctic projections to 2100: simulations with the BISICLES ice sheet model
Published 2025-02-01“…Ice sheet models are the primary tool for projecting future sea level contribution from continental ice sheets. …”
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Recent and future variability of the ice-sheet catchment of Sermeq Kujalleq (Jakobshavn Isbræ), Greenland
Published 2024-01-01“…Knowledge of ice-sheet catchments is critical for mass-balance assessments, especially glacier-scale input–output budgets. …”
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Graph convolutional network as a fast statistical emulator for numerical ice sheet modeling
Published 2025-01-01“…The Ice-sheet and Sea-level System Model (ISSM) provides numerical solutions for ice sheet dynamics using finite element and fine mesh adaption. …”
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10
Exploring grid sensitivity in an ice sheet model: A case study of the Amery Ice Shelf
Published 2024-12-01Subjects: “…Ice sheet model…”
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11
Signal characteristics of surface seismic explosive sources near the West Antarctic Ice Sheet divide
Published 2024-01-01“…Seismic imaging in 3-D holds great potential for improving our understanding of ice sheet structure and dynamics. Conducting 3-D imaging in remote areas is simplified by using lightweight and logistically straightforward sources. …”
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12
Expansion of supraglacial lake area, volume and extent on the Greenland ice sheet from 1985 to 2023
Published 2025-01-01Subjects: “…Greenland ice sheet…”
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13
Calculations of extreme sea level rise scenarios are strongly dependent on ice sheet model resolution
Published 2025-01-01“…Abstract The West Antarctic Ice Sheet (WAIS) is losing ice and its annual contribution to sea level is increasing. …”
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14
Present-day mass loss rates are a precursor for West Antarctic Ice Sheet collapse
Published 2025-01-01“…<p>Observations of recent mass loss rates of the West Antarctic Ice Sheet (WAIS) raise concerns about its stability since a collapse would increase global sea levels by several meters. …”
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15
Retreat of the Greenland Ice Sheet leads to divergent patterns of reconfiguration at its freshwater and tidewater margins
Published 2024-01-01“…Greenland's marine- and land-terminating glaciers are retreating inland due to climate warming, reconfiguring the way the ice sheet interacts with its proglacial environment. …”
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16
Nonlinear Hydroelastic Waves beneath a Floating Ice Sheet in a Fluid of Finite Depth
Published 2013-01-01“…The nonlinear hydroelastic waves propagating beneath an infinite ice sheet floating on an inviscid fluid of finite depth are investigated analytically. …”
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17
Geodetic Evidence of the Interannual Fluctuations and Long-Term Trends Over the Antarctic Ice Sheet Mass Change
Published 2025-01-01“…The spatiotemporal characteristics of the Antarctic ice sheet (AIS), as constrained by geodetic observations, provide us with a deeper understanding of the current evolution of ice mass balance. …”
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18
Evidence of active subglacial lakes under a slowly moving coastal region of the Antarctic Ice Sheet
Published 2025-01-01“…<p>Active subglacial lakes beneath the Antarctic Ice Sheet provide insights into the dynamic subglacial environment, with implications for ice-sheet dynamics and mass balance. …”
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19
Surface energy balance closure over melting snow and ice from in situ measurements on the Greenland ice sheet
Published 2024-01-01“…This study quantifies the SEB closure by comparing the energy available for surface melt, determined from continuous measurements of radiative fluxes and turbulent heat fluxes, to the surface ablation measured on the Greenland ice sheet between 2003 and 2023. We find that the measured daily energy available for surface melt exceeds the observed surface melt by on average 18 ± 30 W m−2 for snow and 12 ± 54 W m−2 for ice conditions (mean ± SD), which corresponds to 46 and 10% of the average energy available for surface melt, respectively. …”
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Global Mean and Relative Sea-Level Changes Over the Past 66 Myr: Implications for Early Eocene Ice Sheets
Published 2024-12-01“…Continental-scale ice sheets waxed and waned beginning ca. 34 Ma (>50 m BSL changes), with near complete collapse during the Miocene Climate Optimum (17–14.8 Ma). …”
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