In-situ snow accumulation, melt, and firn density records using ground penetrating radar and firn cores, western Greenland, 1955-2017

The stability of the Greenland Ice Sheet (GIS) is of critical interest to scientists and society at large in the context of future sea-level rise. The magnitude of GIS volumetric shrinkage in the coming decades depends on its glacial discharge and surface mass balance (SMB), with the later represent...

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Main Author: Lewis, Gabriel
Format: Dataset
Language:English
Published: NSF Arctic Data Center 2019
Subjects:
Online Access:https://dx.doi.org/10.18739/a2610vs8w
https://arcticdata.io/catalog/view/doi:10.18739/A2610VS8W
id ftdatacite:10.18739/a2610vs8w
record_format openpolar
spelling ftdatacite:10.18739/a2610vs8w 2023-05-15T16:24:11+02:00 In-situ snow accumulation, melt, and firn density records using ground penetrating radar and firn cores, western Greenland, 1955-2017 Lewis, Gabriel 2019 text/xml https://dx.doi.org/10.18739/a2610vs8w https://arcticdata.io/catalog/view/doi:10.18739/A2610VS8W en eng NSF Arctic Data Center Greenland Ice core Firn core GreenTrACS dataset Dataset 2019 ftdatacite https://doi.org/10.18739/a2610vs8w 2021-11-05T12:55:41Z The stability of the Greenland Ice Sheet (GIS) is of critical interest to scientists and society at large in the context of future sea-level rise. The magnitude of GIS volumetric shrinkage in the coming decades depends on its glacial discharge and surface mass balance (SMB), with the later representing the balance between accumulation and surface melt. Estimates of Greenland SMB increasingly utilize climate reanalyses and high-resolution regional climate models (RCMs) to determine snow accumulation, surface melt and runoff/refreeze. These models show significant and model-dependent biases along the high-gradient edges of the GIS where the highest and most variable (in space and time) rates of accumulation and surface melt are observed. Thus, the edges of the GIS are in critical need of updated validation with in-situ accumulation and melt data, as model biases lead to significant deviations in mass balance estimates. Here we propose a traverse in the Western Greenland percolation zone over two field seasons to develop continuous in-situ snow accumulation and firn density records using ground-based radar and shallow firn cores. Our research objectives include: (1) determining the spatiotemporal patterns of snow accumulation in Western Greenland over the past 20-40 years; (2) evaluating surface melt refreeze and englacial meltwater storage in the Western Greenland percolation zone over the past 20-40 years; and (3) quantifying the accumulation and surface melt biases of the most recent climate reanalysis models and their RCM counterparts. Dataset Greenland Greenland ice core ice core Ice Sheet DataCite Metadata Store (German National Library of Science and Technology) Greenland
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Greenland
Ice core
Firn core
GreenTrACS
spellingShingle Greenland
Ice core
Firn core
GreenTrACS
Lewis, Gabriel
In-situ snow accumulation, melt, and firn density records using ground penetrating radar and firn cores, western Greenland, 1955-2017
topic_facet Greenland
Ice core
Firn core
GreenTrACS
description The stability of the Greenland Ice Sheet (GIS) is of critical interest to scientists and society at large in the context of future sea-level rise. The magnitude of GIS volumetric shrinkage in the coming decades depends on its glacial discharge and surface mass balance (SMB), with the later representing the balance between accumulation and surface melt. Estimates of Greenland SMB increasingly utilize climate reanalyses and high-resolution regional climate models (RCMs) to determine snow accumulation, surface melt and runoff/refreeze. These models show significant and model-dependent biases along the high-gradient edges of the GIS where the highest and most variable (in space and time) rates of accumulation and surface melt are observed. Thus, the edges of the GIS are in critical need of updated validation with in-situ accumulation and melt data, as model biases lead to significant deviations in mass balance estimates. Here we propose a traverse in the Western Greenland percolation zone over two field seasons to develop continuous in-situ snow accumulation and firn density records using ground-based radar and shallow firn cores. Our research objectives include: (1) determining the spatiotemporal patterns of snow accumulation in Western Greenland over the past 20-40 years; (2) evaluating surface melt refreeze and englacial meltwater storage in the Western Greenland percolation zone over the past 20-40 years; and (3) quantifying the accumulation and surface melt biases of the most recent climate reanalysis models and their RCM counterparts.
format Dataset
author Lewis, Gabriel
author_facet Lewis, Gabriel
author_sort Lewis, Gabriel
title In-situ snow accumulation, melt, and firn density records using ground penetrating radar and firn cores, western Greenland, 1955-2017
title_short In-situ snow accumulation, melt, and firn density records using ground penetrating radar and firn cores, western Greenland, 1955-2017
title_full In-situ snow accumulation, melt, and firn density records using ground penetrating radar and firn cores, western Greenland, 1955-2017
title_fullStr In-situ snow accumulation, melt, and firn density records using ground penetrating radar and firn cores, western Greenland, 1955-2017
title_full_unstemmed In-situ snow accumulation, melt, and firn density records using ground penetrating radar and firn cores, western Greenland, 1955-2017
title_sort in-situ snow accumulation, melt, and firn density records using ground penetrating radar and firn cores, western greenland, 1955-2017
publisher NSF Arctic Data Center
publishDate 2019
url https://dx.doi.org/10.18739/a2610vs8w
https://arcticdata.io/catalog/view/doi:10.18739/A2610VS8W
geographic Greenland
geographic_facet Greenland
genre Greenland
Greenland ice core
ice core
Ice Sheet
genre_facet Greenland
Greenland ice core
ice core
Ice Sheet
op_doi https://doi.org/10.18739/a2610vs8w
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