Greenland Ice Mapping Project: Ice Flow Velocity Variation at sub-monthly to decadal time scales

We describe several new ice velocity maps produced by the Greenland Ice Mapping Project (GIMP) using Landsat 8 and Copernicus Sentinel 1A/B data. We then focus on several sites where we analyse these data in conjunction with earlier data from this project, which extend back to the year 2000. At Jako...

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Published in:The Cryosphere
Main Authors: Joughin, Ian, Smith, Ben E., Howat, Ian
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6469699/
https://doi.org/10.5194/tc-12-2211-2018
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spelling ftpubmed:oai:pubmedcentral.nih.gov:6469699 2023-05-15T16:27:21+02:00 Greenland Ice Mapping Project: Ice Flow Velocity Variation at sub-monthly to decadal time scales Joughin, Ian Smith, Ben E. Howat, Ian 2018-07-11 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6469699/ https://doi.org/10.5194/tc-12-2211-2018 en eng http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6469699/ http://dx.doi.org/10.5194/tc-12-2211-2018 Article Text 2018 ftpubmed https://doi.org/10.5194/tc-12-2211-2018 2019-04-21T00:39:43Z We describe several new ice velocity maps produced by the Greenland Ice Mapping Project (GIMP) using Landsat 8 and Copernicus Sentinel 1A/B data. We then focus on several sites where we analyse these data in conjunction with earlier data from this project, which extend back to the year 2000. At Jakobshavn Isbrae and Koge Bugt, we find good agreement when comparing results from different sensors. In a change from recent behaviour, Jakobshavn Isbrae began slowing substantially in 2017, with a mid-summer peak that was even slower than some previous winter minimums. Over the last decade, we identify two major slowdown events at Koge Bugt that coincide with short-term advances of the terminus. We also examined populations of glaciers in northwest and southwest Greenland to produce a record of speedup since 2000. Collectively these glaciers continue to speed up, but there are regional differences in the timing of periods of peak speedup. In addition, we computed trends in winter flow speed for much of the southwest margin of the ice sheet and find little in the way of statistically significant change over the period covered by our data. Finally, although consistency of the data generally is good through time and across sensors, our analysis indicates substantial differences can arise in regions with high strain rates (e.g., shear margins) where sensor resolution can become a factor. For applications such as constraining model inversions, users should factor in the impact that the data’s resolution has on their results. Text Greenland Ice Sheet Jakobshavn PubMed Central (PMC) Greenland The Cryosphere 12 7 2211 2227
institution Open Polar
collection PubMed Central (PMC)
op_collection_id ftpubmed
language English
topic Article
spellingShingle Article
Joughin, Ian
Smith, Ben E.
Howat, Ian
Greenland Ice Mapping Project: Ice Flow Velocity Variation at sub-monthly to decadal time scales
topic_facet Article
description We describe several new ice velocity maps produced by the Greenland Ice Mapping Project (GIMP) using Landsat 8 and Copernicus Sentinel 1A/B data. We then focus on several sites where we analyse these data in conjunction with earlier data from this project, which extend back to the year 2000. At Jakobshavn Isbrae and Koge Bugt, we find good agreement when comparing results from different sensors. In a change from recent behaviour, Jakobshavn Isbrae began slowing substantially in 2017, with a mid-summer peak that was even slower than some previous winter minimums. Over the last decade, we identify two major slowdown events at Koge Bugt that coincide with short-term advances of the terminus. We also examined populations of glaciers in northwest and southwest Greenland to produce a record of speedup since 2000. Collectively these glaciers continue to speed up, but there are regional differences in the timing of periods of peak speedup. In addition, we computed trends in winter flow speed for much of the southwest margin of the ice sheet and find little in the way of statistically significant change over the period covered by our data. Finally, although consistency of the data generally is good through time and across sensors, our analysis indicates substantial differences can arise in regions with high strain rates (e.g., shear margins) where sensor resolution can become a factor. For applications such as constraining model inversions, users should factor in the impact that the data’s resolution has on their results.
format Text
author Joughin, Ian
Smith, Ben E.
Howat, Ian
author_facet Joughin, Ian
Smith, Ben E.
Howat, Ian
author_sort Joughin, Ian
title Greenland Ice Mapping Project: Ice Flow Velocity Variation at sub-monthly to decadal time scales
title_short Greenland Ice Mapping Project: Ice Flow Velocity Variation at sub-monthly to decadal time scales
title_full Greenland Ice Mapping Project: Ice Flow Velocity Variation at sub-monthly to decadal time scales
title_fullStr Greenland Ice Mapping Project: Ice Flow Velocity Variation at sub-monthly to decadal time scales
title_full_unstemmed Greenland Ice Mapping Project: Ice Flow Velocity Variation at sub-monthly to decadal time scales
title_sort greenland ice mapping project: ice flow velocity variation at sub-monthly to decadal time scales
publishDate 2018
url http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6469699/
https://doi.org/10.5194/tc-12-2211-2018
geographic Greenland
geographic_facet Greenland
genre Greenland
Ice Sheet
Jakobshavn
genre_facet Greenland
Ice Sheet
Jakobshavn
op_relation http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6469699/
http://dx.doi.org/10.5194/tc-12-2211-2018
op_doi https://doi.org/10.5194/tc-12-2211-2018
container_title The Cryosphere
container_volume 12
container_issue 7
container_start_page 2211
op_container_end_page 2227
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