High-resolution Digital Elevation Model of subglacial topography in the onset region of the Northeast Greenland Ice Stream, generated from swath radar imaging

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Hauptverfasser: Carter, Charlotte, Franke, Steven, Helm, Veit, Jansen, Daniela, Paden, John D, Eisen, Olaf
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 2025
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author Carter, Charlotte
Franke, Steven
Helm, Veit
Jansen, Daniela
Paden, John D
Eisen, Olaf
author_facet Carter, Charlotte
Franke, Steven
Helm, Veit
Jansen, Daniela
Paden, John D
Eisen, Olaf
collection Datos científicos de ciencias marinas y ambientales
contents Rapidly-flowing ice streams drain the interior of the Greenland Ice Sheet, currently accounting for half of its annual mass loss. The Northeast Greenland Ice Stream (NEGIS) is one of the longest, recognisable almost 600 km inland, extending close to the ice divide. Here, we use swath radar imaging to create a high-resolution Digital Elevation Model (DEM) of the bed under the onset zone of the NEGIS, from radio-echo sounding data collected in 2022. The DEM covers a 40 km by 60 km area centred on the drill site for the East Greenland Ice-core Project (EGRIP). It has a spatial resolution of 25 m in coordinate system WGS 84 NSIDC Sea Ice Polar Stereographic North (EPSG 3413). The acquisition system was a multichannel ultra-wideband radar mounted on AWI's POLAR 5 aircraft.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_972422
institution PANGAEA
language en
publishDate 2025
publisher PANGAEA
record_format pangaea
spellingShingle High-resolution Digital Elevation Model of subglacial topography in the onset region of the Northeast Greenland Ice Stream, generated from swath radar imaging
Carter, Charlotte
Franke, Steven
Helm, Veit
Jansen, Daniela
Paden, John D
Eisen, Olaf
AC; Aircraft; Arctic; AWI UWB; digital elevation model (DEM); East Greenland Ice-core Project; EGRIP; NEGIS-FLOW, NEGIS-ANISO, NEGIS Folds; Northeast Greenland Ice Stream (NEGIS); P5_233_NEGIS_2022_2206030202; P5_233_NEGIS_2022_2206070301; P5_233_NEGIS_2022_2206080401; P5_233_NEGIS_2022_2206090501; P5_233_NEGIS_2022_2206100601; P5_233_NEGIS_2022_2206110701; P5_233_NEGIS_2022_2206120801; P5_233_NEGIS_2022_2206130901; P5_233_NEGIS_2022_2206161001; P5-233_NEGIS_2022; POLAR 5; radio echo-sounding; subglacial topography
Rapidly-flowing ice streams drain the interior of the Greenland Ice Sheet, currently accounting for half of its annual mass loss. The Northeast Greenland Ice Stream (NEGIS) is one of the longest, recognisable almost 600 km inland, extending close to the ice divide. Here, we use swath radar imaging to create a high-resolution Digital Elevation Model (DEM) of the bed under the onset zone of the NEGIS, from radio-echo sounding data collected in 2022. The DEM covers a 40 km by 60 km area centred on the drill site for the East Greenland Ice-core Project (EGRIP). It has a spatial resolution of 25 m in coordinate system WGS 84 NSIDC Sea Ice Polar Stereographic North (EPSG 3413). The acquisition system was a multichannel ultra-wideband radar mounted on AWI's POLAR 5 aircraft.
title High-resolution Digital Elevation Model of subglacial topography in the onset region of the Northeast Greenland Ice Stream, generated from swath radar imaging
topic AC; Aircraft; Arctic; AWI UWB; digital elevation model (DEM); East Greenland Ice-core Project; EGRIP; NEGIS-FLOW, NEGIS-ANISO, NEGIS Folds; Northeast Greenland Ice Stream (NEGIS); P5_233_NEGIS_2022_2206030202; P5_233_NEGIS_2022_2206070301; P5_233_NEGIS_2022_2206080401; P5_233_NEGIS_2022_2206090501; P5_233_NEGIS_2022_2206100601; P5_233_NEGIS_2022_2206110701; P5_233_NEGIS_2022_2206120801; P5_233_NEGIS_2022_2206130901; P5_233_NEGIS_2022_2206161001; P5-233_NEGIS_2022; POLAR 5; radio echo-sounding; subglacial topography
url https://doi.org/10.1594/PANGAEA.972422