Sentinel-1 InSAR Measurements of Elevation Changes over Yedoma Uplands on Sobo-Sise Island, Lena Delta

Yedoma-extremely ice-rich permafrost with massive ice wedges formed during the Late Pleistocene-is vulnerable to thawing and degradation under climate warming. Thawing of ice-rich Yedoma results in lowering of surface elevations. Quantitative knowledge about surface elevation changes helps us to und...

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Published in:Remote Sensing
Main Authors: Chen, Jie, Günther, Frank (Dr.), Grosse, Guido (Prof. Dr.), Liu, Lin, Lin, Hui
Format: Article in Journal/Newspaper
Language:English
Published: 2018
Subjects:
Ice
Online Access:https://publishup.uni-potsdam.de/opus4-ubp/frontdoor/index/index/docId/52625
https://doi.org/10.3390/rs10071152
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spelling ftubpotsdam:oai:kobv.de-opus4-uni-potsdam:52625 2023-05-15T16:37:23+02:00 Sentinel-1 InSAR Measurements of Elevation Changes over Yedoma Uplands on Sobo-Sise Island, Lena Delta Chen, Jie Günther, Frank (Dr.) Grosse, Guido (Prof. Dr.) Liu, Lin Lin, Hui 2018-07-21 https://publishup.uni-potsdam.de/opus4-ubp/frontdoor/index/index/docId/52625 https://doi.org/10.3390/rs10071152 eng eng https://publishup.uni-potsdam.de/opus4-ubp/frontdoor/index/index/docId/52625 https://doi.org/10.3390/rs10071152 https://creativecommons.org/licenses/by/4.0/ info:eu-repo/semantics/closedAccess CC-BY ddc:620 Mathematisch-Naturwissenschaftliche Fakultät article doc-type:article 2018 ftubpotsdam https://doi.org/10.3390/rs10071152 2022-08-21T22:36:52Z Yedoma-extremely ice-rich permafrost with massive ice wedges formed during the Late Pleistocene-is vulnerable to thawing and degradation under climate warming. Thawing of ice-rich Yedoma results in lowering of surface elevations. Quantitative knowledge about surface elevation changes helps us to understand the freeze-thaw processes of the active layer and the potential degradation of Yedoma deposits. In this study, we use C-band Sentinel-1 InSAR measurements to map the elevation changes over ice-rich Yedoma uplands on Sobo-Sise Island, Lena Delta with frequent revisit observations (as short as six or 12 days). We observe significant seasonal thaw subsidence during summer months and heterogeneous inter-annual elevation changes from 2016-17. We also observe interesting patterns of stronger seasonal thaw subsidence on elevated flat Yedoma uplands by comparing to the surrounding Yedoma slopes. Inter-annual analyses from 2016-17 suggest that our observed positive surface elevation changes are likely caused by the delayed progression of the thaw season in 2017, associated with mean annual air temperature fluctuations. Article in Journal/Newspaper Ice lena delta permafrost wedge* University of Potsdam: publish.UP Remote Sensing 10 7 1152
institution Open Polar
collection University of Potsdam: publish.UP
op_collection_id ftubpotsdam
language English
topic ddc:620
Mathematisch-Naturwissenschaftliche Fakultät
spellingShingle ddc:620
Mathematisch-Naturwissenschaftliche Fakultät
Chen, Jie
Günther, Frank (Dr.)
Grosse, Guido (Prof. Dr.)
Liu, Lin
Lin, Hui
Sentinel-1 InSAR Measurements of Elevation Changes over Yedoma Uplands on Sobo-Sise Island, Lena Delta
topic_facet ddc:620
Mathematisch-Naturwissenschaftliche Fakultät
description Yedoma-extremely ice-rich permafrost with massive ice wedges formed during the Late Pleistocene-is vulnerable to thawing and degradation under climate warming. Thawing of ice-rich Yedoma results in lowering of surface elevations. Quantitative knowledge about surface elevation changes helps us to understand the freeze-thaw processes of the active layer and the potential degradation of Yedoma deposits. In this study, we use C-band Sentinel-1 InSAR measurements to map the elevation changes over ice-rich Yedoma uplands on Sobo-Sise Island, Lena Delta with frequent revisit observations (as short as six or 12 days). We observe significant seasonal thaw subsidence during summer months and heterogeneous inter-annual elevation changes from 2016-17. We also observe interesting patterns of stronger seasonal thaw subsidence on elevated flat Yedoma uplands by comparing to the surrounding Yedoma slopes. Inter-annual analyses from 2016-17 suggest that our observed positive surface elevation changes are likely caused by the delayed progression of the thaw season in 2017, associated with mean annual air temperature fluctuations.
format Article in Journal/Newspaper
author Chen, Jie
Günther, Frank (Dr.)
Grosse, Guido (Prof. Dr.)
Liu, Lin
Lin, Hui
author_facet Chen, Jie
Günther, Frank (Dr.)
Grosse, Guido (Prof. Dr.)
Liu, Lin
Lin, Hui
author_sort Chen, Jie
title Sentinel-1 InSAR Measurements of Elevation Changes over Yedoma Uplands on Sobo-Sise Island, Lena Delta
title_short Sentinel-1 InSAR Measurements of Elevation Changes over Yedoma Uplands on Sobo-Sise Island, Lena Delta
title_full Sentinel-1 InSAR Measurements of Elevation Changes over Yedoma Uplands on Sobo-Sise Island, Lena Delta
title_fullStr Sentinel-1 InSAR Measurements of Elevation Changes over Yedoma Uplands on Sobo-Sise Island, Lena Delta
title_full_unstemmed Sentinel-1 InSAR Measurements of Elevation Changes over Yedoma Uplands on Sobo-Sise Island, Lena Delta
title_sort sentinel-1 insar measurements of elevation changes over yedoma uplands on sobo-sise island, lena delta
publishDate 2018
url https://publishup.uni-potsdam.de/opus4-ubp/frontdoor/index/index/docId/52625
https://doi.org/10.3390/rs10071152
genre Ice
lena delta
permafrost
wedge*
genre_facet Ice
lena delta
permafrost
wedge*
op_relation https://publishup.uni-potsdam.de/opus4-ubp/frontdoor/index/index/docId/52625
https://doi.org/10.3390/rs10071152
op_rights https://creativecommons.org/licenses/by/4.0/
info:eu-repo/semantics/closedAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.3390/rs10071152
container_title Remote Sensing
container_volume 10
container_issue 7
container_start_page 1152
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