about
Ice-sheet-driven methane storage and release in the Arctic.Modeling of subglacial hydrological development following rapid supraglacial lake drainage.Postglacial response of Arctic Ocean gas hydrates to climatic amelioration.Seismic evidence for complex sedimentary control of Greenland Ice Sheet flow.Massive blow-out craters formed by hydrate-controlled methane expulsion from the Arctic seafloor.Sensitive response of the Greenland Ice Sheet to surface melt drainage over a soft bed.BedMachine v3: Complete Bed Topography and Ocean Bathymetry Mapping of Greenland From Multibeam Echo Sounding Combined With Mass Conservation.Direct measurements of meltwater runoff on the Greenland ice sheet surface.Gas hydrate dissociation off Svalbard induced by isostatic rebound rather than global warming.Dark zone of the Greenland Ice Sheet controlled by distributed biologically-active impurities.Cascading lake drainage on the Greenland Ice Sheet triggered by tensile shock and fracture.Seismic evidence of mechanically weak sediments underlying Russell Glacier, West GreenlandThin-layer effects in glaciological seismic amplitude-versus-angle (AVA) analysis: implications for characterising a subglacial till unit, Russell Glacier, West GreenlandRegulation of ice stream flow through subglacial formation of gas hydratesSeasonal evolution of subglacial drainage and acceleration in a Greenland outlet glacierWhy and How to Write a High-Impact Review Paper: Lessons From Eight Years of Editorial Board Service to Reviews of GeophysicsIce-Dammed Lake Drainage Evolution at Russell Glacier, West GreenlandSelf-regulation of ice flow varies across the ablation area in south-west GreenlandExtraordinary runoff from the Greenland ice sheet in 2012 amplified by hypsometry and depleted firn retentionBiocryomorphology: Integrating Microbial Processes with Ice Surface Hydrology, Topography, and RoughnessReconstructing the Last Glacial Maximum ice sheet in the Weddell Sea embayment, Antarctica, using numerical modelling constrained by field evidenceSubglacial topography inferred from ice surface terrain analysis reveals a large un-surveyed basin below sea level in East AntarcticaThe configuration, sensitivity and rapid retreat of the Late Weichselian Icelandic ice sheetRapid marine deglaciation: asynchronous retreat dynamics between the Irish Sea Ice Stream and terrestrial outlet glaciersThe last Welsh Ice Cap: Part 1 - Modelling its evolution, sensitivity and associated climateThe last Welsh Ice Cap: Part 2 - Dynamics of a topographically controlled icecapInfluence of seasonality on glacier mass balance, and implications for palaeoclimate reconstructionsDynamic cycles, ice streams and their impact on the extent, chronology and deglaciation of the British–Irish ice sheetAlgae Drive Enhanced Darkening of Bare Ice on the Greenland Ice SheetBenchmark experiments for higher-order and full-Stokes ice sheet models (ISMIP–HOM)A Full-Stokes 3-D Calving Model Applied to a Large Greenlandic GlacierGlacial isostatic adjustment associated with the Barents Sea ice sheet: A modelling inter-comparisonSeasonal velocities of eight major marine-terminating outlet glaciers of the Greenland ice sheet from continuous in situ GPS instrumentsGreenland ice sheet motion coupled with daily melting in late summerPalaeoglaciology of Bayan Har Shan, NE Tibetan Plateau: exposure ages reveal a missing LGM expansionIdentifying patterns of correspondence between modeled flow directions and field evidence: An automated flow direction analysisTowards a GIS assessment of numerical ice-sheet model performance using geomorphological dataA revised Little Ice Age chronology of the Franz Josef Glacier, Westland, New ZealandDeglaciation of the Eurasian ice sheet complexIce–ocean interaction and calving front morphology at two west Greenland tidewater outlet glaciers
P50
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P50
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