Helheim Glacier ice velocity variability responds to runoff and terminus position change at different timescales

Factors driving ice flow variability in Greenland vary by timescale. At seasonal scale, Helheim Glacier ice velocity responds most strongly to meltwater runoff. Glacier terminus position drives velocity variability at longer time scales.

Bibliographic Details
Published in:Nature Communications
Main Authors: Lizz Ultee, Denis Felikson, Brent Minchew, Leigh A. Stearns, Bryan Riel
Format: Article in Journal/Newspaper
Language:English
Published: Nature Portfolio 2022
Subjects:
Science
Q
Greenland
glacier
Online Access:https://doi.org/10.1038/s41467-022-33292-y
https://doaj.org/article/cce91817534b435b90e5e8d6b0619d31
id ftdoajarticles:oai:doaj.org/article:cce91817534b435b90e5e8d6b0619d31
record_format openpolar
spelling ftdoajarticles:oai:doaj.org/article:cce91817534b435b90e5e8d6b0619d31 2023-05-15T16:20:52+02:00 Helheim Glacier ice velocity variability responds to runoff and terminus position change at different timescales Lizz Ultee Denis Felikson Brent Minchew Leigh A. Stearns Bryan Riel 2022-10-01T00:00:00Z https://doi.org/10.1038/s41467-022-33292-y https://doaj.org/article/cce91817534b435b90e5e8d6b0619d31 EN eng Nature Portfolio https://doi.org/10.1038/s41467-022-33292-y https://doaj.org/toc/2041-1723 doi:10.1038/s41467-022-33292-y 2041-1723 https://doaj.org/article/cce91817534b435b90e5e8d6b0619d31 Nature Communications, Vol 13, Iss 1, Pp 1-10 (2022) Science Q article 2022 ftdoajarticles https://doi.org/10.1038/s41467-022-33292-y 2022-12-30T20:31:26Z Factors driving ice flow variability in Greenland vary by timescale. At seasonal scale, Helheim Glacier ice velocity responds most strongly to meltwater runoff. Glacier terminus position drives velocity variability at longer time scales. Article in Journal/Newspaper glacier Greenland Directory of Open Access Journals: DOAJ Articles Greenland Nature Communications 13 1
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Science
Q
spellingShingle Science
Q
Lizz Ultee
Denis Felikson
Brent Minchew
Leigh A. Stearns
Bryan Riel
Helheim Glacier ice velocity variability responds to runoff and terminus position change at different timescales
topic_facet Science
Q
description Factors driving ice flow variability in Greenland vary by timescale. At seasonal scale, Helheim Glacier ice velocity responds most strongly to meltwater runoff. Glacier terminus position drives velocity variability at longer time scales.
format Article in Journal/Newspaper
author Lizz Ultee
Denis Felikson
Brent Minchew
Leigh A. Stearns
Bryan Riel
author_facet Lizz Ultee
Denis Felikson
Brent Minchew
Leigh A. Stearns
Bryan Riel
author_sort Lizz Ultee
title Helheim Glacier ice velocity variability responds to runoff and terminus position change at different timescales
title_short Helheim Glacier ice velocity variability responds to runoff and terminus position change at different timescales
title_full Helheim Glacier ice velocity variability responds to runoff and terminus position change at different timescales
title_fullStr Helheim Glacier ice velocity variability responds to runoff and terminus position change at different timescales
title_full_unstemmed Helheim Glacier ice velocity variability responds to runoff and terminus position change at different timescales
title_sort helheim glacier ice velocity variability responds to runoff and terminus position change at different timescales
publisher Nature Portfolio
publishDate 2022
url https://doi.org/10.1038/s41467-022-33292-y
https://doaj.org/article/cce91817534b435b90e5e8d6b0619d31
geographic Greenland
geographic_facet Greenland
genre glacier
Greenland
genre_facet glacier
Greenland
op_source Nature Communications, Vol 13, Iss 1, Pp 1-10 (2022)
op_relation https://doi.org/10.1038/s41467-022-33292-y
https://doaj.org/toc/2041-1723
doi:10.1038/s41467-022-33292-y
2041-1723
https://doaj.org/article/cce91817534b435b90e5e8d6b0619d31
op_doi https://doi.org/10.1038/s41467-022-33292-y
container_title Nature Communications
container_volume 13
container_issue 1
_version_ 1766008889204015104

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