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Daniel Steinhage

Researcher at Alfred Wegener Institute for Polar and Marine Research

Publications -  83
Citations -  2567

Daniel Steinhage is an academic researcher from Alfred Wegener Institute for Polar and Marine Research. The author has contributed to research in topics: Ice sheet & Ice stream. The author has an hindex of 25, co-authored 71 publications receiving 1953 citations.

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Deep glacial troughs and stabilizing ridges unveiled beneath the margins of the Antarctic ice sheet

TL;DR: In this paper, a high-resolution and physically based description of Antarctica bed topography using mass conservation is presented, revealing previously unknown basal features with major implications for glacier response to climate change.
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A new bed elevation dataset for Greenland

TL;DR: In this paper, a new bed elevation dataset for Greenland derived from a combination of multiple airborne ice thickness surveys undertaken between the 1970s and 2012 is presented, with roughly 70% of this having been collected since the year 2000, when the last comprehensive compilation was undertaken.
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A global, high-resolution data set of ice sheet topography, cavity geometry, and ocean bathymetry

TL;DR: The RTopo-2 data set as discussed by the authors provides consistent maps of global ocean bathymetry, upper and lower ice surface topographies, and global surface height on a spherical grid with 30'arcsec grid spacing.
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Balance velocities and measured properties of the Antarctic ice sheet from a new compilation of gridded data for modelling

TL;DR: In this paper, a new compilation of gridded data sets for three-dimensional modeling of the Antarctic ice sheet is presented, including surface elevation, icethickness, bedrock elevation and accumulation rate as interpolated on a 281 x 281 mesh with 20 km spacing.
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Direct evidence for continuous radar reflector originating from changes in crystal-orientation fabric

TL;DR: In this paper, the origin of a strong continuous radar reflector observed with airborne radio-echo sounding (RES) at the EPICA deep-drilling site in Dronning Maud Land, Antarctica, is identified as a transition in crystal fabric orientation from a vertical girdle to an increased single-pole orientation seen along the ice core.