Outlet glacier flow response to surface melt: based on analysis of a high-resolution satellite data set

The dynamics of the Greenland Ice Sheet are affected by surface meltwater reaching the base of the ice, altering ice contact with the bedrock. Lack of understanding of this evolution hampers the ability to predict the effects of increasing temperatures on the Greenland Ice Sheet mass balance. Here w...

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Published in:Journal of Glaciology
Main Authors: Signe H. Larsen, Andreas P. Ahlstrøm, Nanna B. Karlsson, Anders Kusk, Peter L. Langen, Christine S. Hvidberg
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2023
Subjects:
Online Access:https://doi.org/10.1017/jog.2022.124
https://doaj.org/article/562a32088b72486bbcacee8b3f9e523c
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spelling ftdoajarticles:oai:doaj.org/article:562a32088b72486bbcacee8b3f9e523c 2023-08-20T04:06:41+02:00 Outlet glacier flow response to surface melt: based on analysis of a high-resolution satellite data set Signe H. Larsen Andreas P. Ahlstrøm Nanna B. Karlsson Anders Kusk Peter L. Langen Christine S. Hvidberg 2023-08-01T00:00:00Z https://doi.org/10.1017/jog.2022.124 https://doaj.org/article/562a32088b72486bbcacee8b3f9e523c EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143022001241/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2022.124 0022-1430 1727-5652 https://doaj.org/article/562a32088b72486bbcacee8b3f9e523c Journal of Glaciology, Vol 69, Pp 1047-1055 (2023) Ice dynamics ice streams subglacial processes Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2023 ftdoajarticles https://doi.org/10.1017/jog.2022.124 2023-07-30T00:36:44Z The dynamics of the Greenland Ice Sheet are affected by surface meltwater reaching the base of the ice, altering ice contact with the bedrock. Lack of understanding of this evolution hampers the ability to predict the effects of increasing temperatures on the Greenland Ice Sheet mass balance. Here we present a unique high-resolution study of ice velocity response to surface melting based on data from a COSMO-SkyMed satellite campaign over Upernavik Isstrøm (Northwest Greenland) for two months around the end of the 2014 melt season. We show that the velocity variations, due to both short-term (days) and seasonal variations in surface melt rates, are increasing in relative strength farther from the glacier terminus. Furthermore, we observe how ice dynamic response to frontal retreat, reaching several kilometres inland, can obscure the meltwater-induced velocity change close to the terminus. Future studies should consider the flow velocity dependence on the distance to the terminus, and local geometry, to distinguish subglacial hydrologic system changes from frontal processes and local basal conditions. Article in Journal/Newspaper glacier Greenland Ice Sheet Journal of Glaciology Upernavik Directory of Open Access Journals: DOAJ Articles Greenland Upernavik Isstrøm ENVELOPE(-54.500,-54.500,72.917,72.917) Journal of Glaciology 1 9
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Ice dynamics
ice streams
subglacial processes
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle Ice dynamics
ice streams
subglacial processes
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
Signe H. Larsen
Andreas P. Ahlstrøm
Nanna B. Karlsson
Anders Kusk
Peter L. Langen
Christine S. Hvidberg
Outlet glacier flow response to surface melt: based on analysis of a high-resolution satellite data set
topic_facet Ice dynamics
ice streams
subglacial processes
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
description The dynamics of the Greenland Ice Sheet are affected by surface meltwater reaching the base of the ice, altering ice contact with the bedrock. Lack of understanding of this evolution hampers the ability to predict the effects of increasing temperatures on the Greenland Ice Sheet mass balance. Here we present a unique high-resolution study of ice velocity response to surface melting based on data from a COSMO-SkyMed satellite campaign over Upernavik Isstrøm (Northwest Greenland) for two months around the end of the 2014 melt season. We show that the velocity variations, due to both short-term (days) and seasonal variations in surface melt rates, are increasing in relative strength farther from the glacier terminus. Furthermore, we observe how ice dynamic response to frontal retreat, reaching several kilometres inland, can obscure the meltwater-induced velocity change close to the terminus. Future studies should consider the flow velocity dependence on the distance to the terminus, and local geometry, to distinguish subglacial hydrologic system changes from frontal processes and local basal conditions.
format Article in Journal/Newspaper
author Signe H. Larsen
Andreas P. Ahlstrøm
Nanna B. Karlsson
Anders Kusk
Peter L. Langen
Christine S. Hvidberg
author_facet Signe H. Larsen
Andreas P. Ahlstrøm
Nanna B. Karlsson
Anders Kusk
Peter L. Langen
Christine S. Hvidberg
author_sort Signe H. Larsen
title Outlet glacier flow response to surface melt: based on analysis of a high-resolution satellite data set
title_short Outlet glacier flow response to surface melt: based on analysis of a high-resolution satellite data set
title_full Outlet glacier flow response to surface melt: based on analysis of a high-resolution satellite data set
title_fullStr Outlet glacier flow response to surface melt: based on analysis of a high-resolution satellite data set
title_full_unstemmed Outlet glacier flow response to surface melt: based on analysis of a high-resolution satellite data set
title_sort outlet glacier flow response to surface melt: based on analysis of a high-resolution satellite data set
publisher Cambridge University Press
publishDate 2023
url https://doi.org/10.1017/jog.2022.124
https://doaj.org/article/562a32088b72486bbcacee8b3f9e523c
long_lat ENVELOPE(-54.500,-54.500,72.917,72.917)
geographic Greenland
Upernavik Isstrøm
geographic_facet Greenland
Upernavik Isstrøm
genre glacier
Greenland
Ice Sheet
Journal of Glaciology
Upernavik
genre_facet glacier
Greenland
Ice Sheet
Journal of Glaciology
Upernavik
op_source Journal of Glaciology, Vol 69, Pp 1047-1055 (2023)
op_relation https://www.cambridge.org/core/product/identifier/S0022143022001241/type/journal_article
https://doaj.org/toc/0022-1430
https://doaj.org/toc/1727-5652
doi:10.1017/jog.2022.124
0022-1430
1727-5652
https://doaj.org/article/562a32088b72486bbcacee8b3f9e523c
op_doi https://doi.org/10.1017/jog.2022.124
container_title Journal of Glaciology
container_start_page 1
op_container_end_page 9
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