Roughness anisotropy calculated at flightline intersections of the 2018 and 2022 NEGIS surveys, Northeast Greenland Ice Stream, downstream of the EastGRIP ice core site

Fuente: PANGAEA
Enregistré dans:
Détails bibliographiques
Auteurs principaux: Carter, Charlotte, Franke, Steven, Jansen, Daniela, Eisen, Olaf
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 2025
Sujets:
Accès en ligne:
Tags: Ajouter un tag
Pas de tags, Soyez le premier à ajouter un tag!
_version_ 1867171345523015680
author Carter, Charlotte
Franke, Steven
Jansen, Daniela
Eisen, Olaf
author_facet Carter, Charlotte
Franke, Steven
Jansen, Daniela
Eisen, Olaf
collection Datos científicos de ciencias marinas y ambientales
contents The Northeast Greenland Ice Stream (NEGIS) is an elongated feature extending ~600 km into the interior of the Greenland Ice Sheet. Here, we investigate detailed subglacial topography along the length of the NEGIS to ascertain the characteristics of the ice stream bed. Spatial topographic roughness describes the standard deviation of vertical change in bed elevation over a given horizontal distance (Root Mean Square height, or RMSh). RMSh values were derived from ice thickness data from AWI's P5-233_NEGIS_2022 and P6-211_EGRIP_NOR_2018 flight campaigns, where the majority of profiles were oriented parallel or perpendicular to ice flow direction. A moving window size of 960 m (64 data points) was used to calculate RMSh, and values are omitted where gaps in the ice thickness data were present. Roughness anisotropy was also calculated at the intersection of two flightlines, as the ratio between along- and across-flow roughness.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_984361
institution PANGAEA
language en
publishDate 2025
publisher PANGAEA
record_format pangaea
spellingShingle Roughness anisotropy calculated at flightline intersections of the 2018 and 2022 NEGIS surveys, Northeast Greenland Ice Stream, downstream of the EastGRIP ice core site
Carter, Charlotte
Franke, Steven
Jansen, Daniela
Eisen, Olaf
AC; Aircraft; Arctic; AWI UWB; Bed elevation; East Greenland Ice-core Project; EGRIP; EGRIP-NOR; EGRIP-NOR-18; LATITUDE; Line ID; LONGITUDE; MULT; Multiple investigations; 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; P6-211_EGRIP_NOR_2018; Point ID; POLAR 5; POLAR 6; radio echo sounding; Root mean square height; Roughness; Roughness anisotropy
The Northeast Greenland Ice Stream (NEGIS) is an elongated feature extending ~600 km into the interior of the Greenland Ice Sheet. Here, we investigate detailed subglacial topography along the length of the NEGIS to ascertain the characteristics of the ice stream bed. Spatial topographic roughness describes the standard deviation of vertical change in bed elevation over a given horizontal distance (Root Mean Square height, or RMSh). RMSh values were derived from ice thickness data from AWI's P5-233_NEGIS_2022 and P6-211_EGRIP_NOR_2018 flight campaigns, where the majority of profiles were oriented parallel or perpendicular to ice flow direction. A moving window size of 960 m (64 data points) was used to calculate RMSh, and values are omitted where gaps in the ice thickness data were present. Roughness anisotropy was also calculated at the intersection of two flightlines, as the ratio between along- and across-flow roughness.
title Roughness anisotropy calculated at flightline intersections of the 2018 and 2022 NEGIS surveys, Northeast Greenland Ice Stream, downstream of the EastGRIP ice core site
topic AC; Aircraft; Arctic; AWI UWB; Bed elevation; East Greenland Ice-core Project; EGRIP; EGRIP-NOR; EGRIP-NOR-18; LATITUDE; Line ID; LONGITUDE; MULT; Multiple investigations; 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; P6-211_EGRIP_NOR_2018; Point ID; POLAR 5; POLAR 6; radio echo sounding; Root mean square height; Roughness; Roughness anisotropy
url https://doi.org/10.1594/PANGAEA.984361