about
Refined broad-scale sub-glacial morphology of Aurora Subglacial Basin, East Antarctica derived by an ice-dynamics-based interpolation schemeActive formation of 'chaos terrain' over shallow subsurface water on EuropaOcean access to a cavity beneath Totten Glacier in East AntarcticaEvidence for elevated and spatially variable geothermal flux beneath the West Antarctic Ice Sheet.A dynamic early East Antarctic Ice Sheet suggested by ice-covered fjord landscapes.Evidence for a water system transition beneath Thwaites Glacier, West Antarctica.Ice flow direction change in interior West Antarctica.Wind causes Totten Ice Shelf melt and acceleration.Initiation and long-term instability of the East Antarctic Ice Sheet.New Antarctic Gravity Anomaly Grid for Enhanced Geodetic and Geophysical Studies in Antarctica.Discovery of a hypersaline subglacial lake complex beneath Devon Ice Cap, Canadian Arctic.Seismic detection of an active subglacial magmatic complex in Marie Byrd Land, AntarcticaAntarctic regional ice loss rates from GRACEBedmap2: improved ice bed, surface and thickness datasets for AntarcticaNew boundary conditions for the West Antarctic ice sheet: Subglacial topography beneath Pine Island GlacierGreenland subglacial lakes detected by radarOcean-driven heating of Europa’s icy shell at low latitudesAerogravity evidence for major crustal thinning under the Pine Island Glacier region (West Antarctica)Accelerated Antarctic ice loss from satellite gravity measurementsSeasonal dynamics of Totten Ice Shelf controlled by sea ice buttressingA Method of Repeat Photoclinometry for Detecting Kilometer-Scale Ice Sheet Surface EvolutionTwo independent methods for mapping the grounding line of an outlet glacier – an example from the Astrolabe Glacier, Terre Adélie, AntarcticaJupiter ICY moon explorer (JUICE): Advances in the design of the radar for Icy Moons (RIME)RIME: Radar for Icy Moon ExplorationMeltwater intensive glacial retreat in polar environments and investigation of associated sediments: example from Pine Island Bay, West AntarcticaA high-resolution synthetic bed elevation grid of the Antarctic continentThe Australo-Antarctic Columbia to Gondwana transitionThe subglacial geology of Wilkes Land, East AntarcticaEvidence of a hydrological connection between the ice divide and ice sheet margin in the Aurora Subglacial Basin, East AntarcticaAn extensive subglacial lake and canyon system in Princess Elizabeth Land, East AntarcticaWhere to find 1.5 million yr old ice for the IPICS "Oldest-Ice" ice coreIdentifying flowlines and limitations of flux analyses in the interior of Thwaites Glacier, AntarcticaWeak bed control of the eastern shear margin of Thwaites Glacier, West AntarcticaNew Magnetic Anomaly Map of the AntarcticSeasonal dynamics of Totten Ice Shelf controlled by sea ice buttressingAccumulation patterns around Dome C, East Antarctica, in the last 73 kyrHigh-resolution boundary conditions of an old ice target near Dome C, AntarcticaStable accumulation patterns around Dome C, East Antarctica, over the last glacial cycleComparison of measurements from different radio-echo sounding systems and synchronization with the ice core at Dome C, AntarcticaCharacterizing near-surface firn using the scattered signal component of the glacier surface return from airborne radio-echo sounding
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description
Senior Research Scientist, Institute for Geophysics, University of Texas at Austin
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wetenschapper
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Donald D. Blankenship
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Donald D. Blankenship
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Donald D. Blankenship
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Donald D. Blankenship
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Donald D. Blankenship
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Donald D. Blankenship
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Donald D. Blankenship
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Donald D. Blankenship
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D D Blankenship
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D. D. Blankenship
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Donald Blankenship
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Donald D Blankenship
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Donald D. Blankenship
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Donald D. Blankenship
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Donald D. Blankenship
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Donald D. Blankenship
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P1960
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P496
0000-0003-0205-4830