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...

Full description

Bibliographic Details
Published in:Remote Sensing
Main Authors: Jie Chen, Frank Günther, Guido Grosse, Lin Liu, Hui Lin
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2018
Subjects:
Ice
Online Access:https://doi.org/10.3390/rs10071152
id ftmdpi:oai:mdpi.com:/2072-4292/10/7/1152/
record_format openpolar
spelling ftmdpi:oai:mdpi.com:/2072-4292/10/7/1152/ 2023-08-20T04:07:07+02:00 Sentinel-1 InSAR Measurements of Elevation Changes over Yedoma Uplands on Sobo-Sise Island, Lena Delta Jie Chen Frank Günther Guido Grosse Lin Liu Hui Lin agris 2018-07-21 application/pdf https://doi.org/10.3390/rs10071152 EN eng Multidisciplinary Digital Publishing Institute Remote Sensing in Geology, Geomorphology and Hydrology https://dx.doi.org/10.3390/rs10071152 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 10; Issue 7; Pages: 1152 Sentinel-1 InSAR Yedoma uplands Sobo-Sise Island summer heave permafrost thaw subsidence active layer Text 2018 ftmdpi https://doi.org/10.3390/rs10071152 2023-07-31T21:38:19Z 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. Text Ice lena delta permafrost wedge* MDPI Open Access Publishing Remote Sensing 10 7 1152
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic Sentinel-1 InSAR
Yedoma uplands
Sobo-Sise Island
summer heave
permafrost thaw subsidence
active layer
spellingShingle Sentinel-1 InSAR
Yedoma uplands
Sobo-Sise Island
summer heave
permafrost thaw subsidence
active layer
Jie Chen
Frank Günther
Guido Grosse
Lin Liu
Hui Lin
Sentinel-1 InSAR Measurements of Elevation Changes over Yedoma Uplands on Sobo-Sise Island, Lena Delta
topic_facet Sentinel-1 InSAR
Yedoma uplands
Sobo-Sise Island
summer heave
permafrost thaw subsidence
active layer
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 Text
author Jie Chen
Frank Günther
Guido Grosse
Lin Liu
Hui Lin
author_facet Jie Chen
Frank Günther
Guido Grosse
Lin Liu
Hui Lin
author_sort Jie Chen
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
publisher Multidisciplinary Digital Publishing Institute
publishDate 2018
url https://doi.org/10.3390/rs10071152
op_coverage agris
genre Ice
lena delta
permafrost
wedge*
genre_facet Ice
lena delta
permafrost
wedge*
op_source Remote Sensing; Volume 10; Issue 7; Pages: 1152
op_relation Remote Sensing in Geology, Geomorphology and Hydrology
https://dx.doi.org/10.3390/rs10071152
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs10071152
container_title Remote Sensing
container_volume 10
container_issue 7
container_start_page 1152
_version_ 1774718564668801024