Noble gas signatures in Greenland : tracing glacial meltwater sources

Author Posting. © American Geophysical Union, 2015. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geophysical Research Letters 42 (2015): 9311–9318, doi:10.1002/2015GL065778. This study repres...

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Published in:Geophysical Research Letters
Main Authors: Niu, Yi, Castro, M. Clara, Aciego, Sarah M., Hall, Chris M., Stevenson, Emily I., Arendt, Carli A., Das, Sarah B.
Format: Article in Journal/Newspaper
Language:English
Published: John Wiley & Sons 2015
Subjects:
Online Access:https://hdl.handle.net/1912/7798
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spelling ftwhoas:oai:darchive.mblwhoilibrary.org:1912/7798 2023-05-15T16:26:52+02:00 Noble gas signatures in Greenland : tracing glacial meltwater sources Niu, Yi Castro, M. Clara Aciego, Sarah M. Hall, Chris M. Stevenson, Emily I. Arendt, Carli A. Das, Sarah B. 2015-11-06 https://hdl.handle.net/1912/7798 en_US eng John Wiley & Sons https://doi.org/10.1002/2015GL065778 Geophysical Research Letters 42 (2015): 9311–9318 https://hdl.handle.net/1912/7798 doi:10.1002/2015GL065778 Geophysical Research Letters 42 (2015): 9311–9318 doi:10.1002/2015GL065778 Noble gases Greenland Glacial meltwater Water residence times Article 2015 ftwhoas https://doi.org/10.1002/2015GL065778 2022-05-28T22:59:30Z Author Posting. © American Geophysical Union, 2015. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geophysical Research Letters 42 (2015): 9311–9318, doi:10.1002/2015GL065778. This study represents the first comprehensive noble gas study in glacial meltwater from the Greenland Ice Sheet. It shows that most samples are in disequilibrium with surface collection conditions. A preliminary Ne and Xe analysis suggests that about half of the samples equilibrated at a temperature of ~0°C and altitudes between 1000 m and 2000 m, with a few samples pointing to lower equilibration altitudes and temperatures between 2°C and 5°C. Two samples suggest an origin as melted ice and complete lack of equilibration with surface conditions. A helium component analysis suggests that this glacial meltwater was isolated from the atmosphere prior to the 1950s, with most samples yielding residence times ≤ 420 years. Most samples represent a mixture between a dominant atmospheric component originating as precipitation and basal meltwater or groundwater, which has accumulated crustal 4He over time. University of Michigan; Packard Foundation; Department of Earth and Environmental Sciences Turner fellowship 2016-05-06 Article in Journal/Newspaper Greenland Ice Sheet Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) Greenland Geophysical Research Letters 42 21 9311 9318
institution Open Polar
collection Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server)
op_collection_id ftwhoas
language English
topic Noble gases
Greenland
Glacial meltwater
Water residence times
spellingShingle Noble gases
Greenland
Glacial meltwater
Water residence times
Niu, Yi
Castro, M. Clara
Aciego, Sarah M.
Hall, Chris M.
Stevenson, Emily I.
Arendt, Carli A.
Das, Sarah B.
Noble gas signatures in Greenland : tracing glacial meltwater sources
topic_facet Noble gases
Greenland
Glacial meltwater
Water residence times
description Author Posting. © American Geophysical Union, 2015. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geophysical Research Letters 42 (2015): 9311–9318, doi:10.1002/2015GL065778. This study represents the first comprehensive noble gas study in glacial meltwater from the Greenland Ice Sheet. It shows that most samples are in disequilibrium with surface collection conditions. A preliminary Ne and Xe analysis suggests that about half of the samples equilibrated at a temperature of ~0°C and altitudes between 1000 m and 2000 m, with a few samples pointing to lower equilibration altitudes and temperatures between 2°C and 5°C. Two samples suggest an origin as melted ice and complete lack of equilibration with surface conditions. A helium component analysis suggests that this glacial meltwater was isolated from the atmosphere prior to the 1950s, with most samples yielding residence times ≤ 420 years. Most samples represent a mixture between a dominant atmospheric component originating as precipitation and basal meltwater or groundwater, which has accumulated crustal 4He over time. University of Michigan; Packard Foundation; Department of Earth and Environmental Sciences Turner fellowship 2016-05-06
format Article in Journal/Newspaper
author Niu, Yi
Castro, M. Clara
Aciego, Sarah M.
Hall, Chris M.
Stevenson, Emily I.
Arendt, Carli A.
Das, Sarah B.
author_facet Niu, Yi
Castro, M. Clara
Aciego, Sarah M.
Hall, Chris M.
Stevenson, Emily I.
Arendt, Carli A.
Das, Sarah B.
author_sort Niu, Yi
title Noble gas signatures in Greenland : tracing glacial meltwater sources
title_short Noble gas signatures in Greenland : tracing glacial meltwater sources
title_full Noble gas signatures in Greenland : tracing glacial meltwater sources
title_fullStr Noble gas signatures in Greenland : tracing glacial meltwater sources
title_full_unstemmed Noble gas signatures in Greenland : tracing glacial meltwater sources
title_sort noble gas signatures in greenland : tracing glacial meltwater sources
publisher John Wiley & Sons
publishDate 2015
url https://hdl.handle.net/1912/7798
geographic Greenland
geographic_facet Greenland
genre Greenland
Ice Sheet
genre_facet Greenland
Ice Sheet
op_source Geophysical Research Letters 42 (2015): 9311–9318
doi:10.1002/2015GL065778
op_relation https://doi.org/10.1002/2015GL065778
Geophysical Research Letters 42 (2015): 9311–9318
https://hdl.handle.net/1912/7798
doi:10.1002/2015GL065778
op_doi https://doi.org/10.1002/2015GL065778
container_title Geophysical Research Letters
container_volume 42
container_issue 21
container_start_page 9311
op_container_end_page 9318
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