Rapid basal channel growth beneath Greenland's longest floating ice shelf

This dataset contains ice surface elevation reconstructions, floating ice bottom elevation reconstructions, and Lagrangian surface elevation change estimates for the Northeast Greenland Ice Sheet outlet region, focused on Nioghalvfjerdsfjorden Glacier (N79); as well as elevation time series for sele...

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Bibliographic Details
Main Author: Narkevic, Ash
Other Authors: Csatho, Beata
Format: Article in Journal/Newspaper
Language:unknown
Published: 2023
Subjects:
Online Access:https://zenodo.org/record/7518206
https://doi.org/10.5281/zenodo.7518206
id ftzenodo:oai:zenodo.org:7518206
record_format openpolar
spelling ftzenodo:oai:zenodo.org:7518206 2023-05-15T16:21:30+02:00 Rapid basal channel growth beneath Greenland's longest floating ice shelf Narkevic, Ash Csatho, Beata 2023-01-09 https://zenodo.org/record/7518206 https://doi.org/10.5281/zenodo.7518206 unknown doi:10.5281/zenodo.7518205 https://zenodo.org/record/7518206 https://doi.org/10.5281/zenodo.7518206 oai:zenodo.org:7518206 info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/4.0/legalcode info:eu-repo/semantics/article publication-article 2023 ftzenodo https://doi.org/10.5281/zenodo.751820610.5281/zenodo.7518205 2023-03-11T00:13:26Z This dataset contains ice surface elevation reconstructions, floating ice bottom elevation reconstructions, and Lagrangian surface elevation change estimates for the Northeast Greenland Ice Sheet outlet region, focused on Nioghalvfjerdsfjorden Glacier (N79); as well as elevation time series for select locations. The surface elevation reconstructions (beginning with "dem_mosaic_") consist of mosaics of WorldView stereoimage DEMs from the ArcticDEM project that have been individually corrected using laser altimetry (ATM, ICESat, and ICESat-2). These elevations are referenced to the WGS84 datum, and include reconstruction for 2012, 2014-2017, and 2020. The ice bottom reconstructions (beginning with "dem_ice_bottom_") apply a hydrostatic assumption to the surface elevation reconstruction to infer the bed elevation. These elevations are referenced to the Eigen-6c4 geoid, and include all the years above, as well as 1978, based on DEMs from aerial photographs. The Lagrangian elevation change reconstruction (beginning with "lagrangian_elevation_change_") is derived from comparing elevation values in successive time periods, using velocity values to infer displacement over the interim and match pixels that represent the same ice parcel. Reported values correspond to the end point of this migration. The time series file ("TimeSeriesTile26_partitioned_selected.txt") contains SERAC elevation time series for 6 locations near the N79 grounding line. Article in Journal/Newspaper glacier Greenland Ice Sheet Ice Shelf Nioghalvfjerdsfjorden Zenodo Greenland Nioghalvfjerdsfjorden ENVELOPE(-21.500,-21.500,79.500,79.500)
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
description This dataset contains ice surface elevation reconstructions, floating ice bottom elevation reconstructions, and Lagrangian surface elevation change estimates for the Northeast Greenland Ice Sheet outlet region, focused on Nioghalvfjerdsfjorden Glacier (N79); as well as elevation time series for select locations. The surface elevation reconstructions (beginning with "dem_mosaic_") consist of mosaics of WorldView stereoimage DEMs from the ArcticDEM project that have been individually corrected using laser altimetry (ATM, ICESat, and ICESat-2). These elevations are referenced to the WGS84 datum, and include reconstruction for 2012, 2014-2017, and 2020. The ice bottom reconstructions (beginning with "dem_ice_bottom_") apply a hydrostatic assumption to the surface elevation reconstruction to infer the bed elevation. These elevations are referenced to the Eigen-6c4 geoid, and include all the years above, as well as 1978, based on DEMs from aerial photographs. The Lagrangian elevation change reconstruction (beginning with "lagrangian_elevation_change_") is derived from comparing elevation values in successive time periods, using velocity values to infer displacement over the interim and match pixels that represent the same ice parcel. Reported values correspond to the end point of this migration. The time series file ("TimeSeriesTile26_partitioned_selected.txt") contains SERAC elevation time series for 6 locations near the N79 grounding line.
author2 Csatho, Beata
format Article in Journal/Newspaper
author Narkevic, Ash
spellingShingle Narkevic, Ash
Rapid basal channel growth beneath Greenland's longest floating ice shelf
author_facet Narkevic, Ash
author_sort Narkevic, Ash
title Rapid basal channel growth beneath Greenland's longest floating ice shelf
title_short Rapid basal channel growth beneath Greenland's longest floating ice shelf
title_full Rapid basal channel growth beneath Greenland's longest floating ice shelf
title_fullStr Rapid basal channel growth beneath Greenland's longest floating ice shelf
title_full_unstemmed Rapid basal channel growth beneath Greenland's longest floating ice shelf
title_sort rapid basal channel growth beneath greenland's longest floating ice shelf
publishDate 2023
url https://zenodo.org/record/7518206
https://doi.org/10.5281/zenodo.7518206
long_lat ENVELOPE(-21.500,-21.500,79.500,79.500)
geographic Greenland
Nioghalvfjerdsfjorden
geographic_facet Greenland
Nioghalvfjerdsfjorden
genre glacier
Greenland
Ice Sheet
Ice Shelf
Nioghalvfjerdsfjorden
genre_facet glacier
Greenland
Ice Sheet
Ice Shelf
Nioghalvfjerdsfjorden
op_relation doi:10.5281/zenodo.7518205
https://zenodo.org/record/7518206
https://doi.org/10.5281/zenodo.7518206
oai:zenodo.org:7518206
op_rights info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.5281/zenodo.751820610.5281/zenodo.7518205
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