Erosion rates of the Sobo-Sise yedoma permafrost cliff in the Lena River Delta derived from remote sensing imagery
Permafrost thaw and ice wedge degradation lead to drastic landscape changes in the permafrost region. With this data set we investigated the cliff retreat of the Sobo-Sise Cliff (SSC), a high ice-bearing yedoma cliff in the Lena River Delta. The 1,660 m long cliff SSC extends from 72°32'34 N /...
Main Authors: | , , , , , , , , , , , |
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Format: | Other/Unknown Material |
Language: | English |
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PANGAEA
2020
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.918507 https://doi.org/10.1594/PANGAEA.918507 |
id |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.918507 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
AWI_Envi AWI_Perma CACOON Carbon in Permafrost / Kohlenstoff im Permafrost Changing Arctic Carbon cycle in the cOastal Ocean Near-shore cliff erosion digital shoreline analysis system erosion rates KoPF Lena Delta NUNATARYUK Permafrost thaw and the changing Arctic coast science for socioeconomic adaptation Permafrost Permafrost Research PETA-CARB Polar Terrestrial Environmental Systems @ AWI Rapid Permafrost Thaw in a Warming Arctic and Impacts on the Soil Organic Carbon Pool remote sensing river delta Time series |
spellingShingle |
AWI_Envi AWI_Perma CACOON Carbon in Permafrost / Kohlenstoff im Permafrost Changing Arctic Carbon cycle in the cOastal Ocean Near-shore cliff erosion digital shoreline analysis system erosion rates KoPF Lena Delta NUNATARYUK Permafrost thaw and the changing Arctic coast science for socioeconomic adaptation Permafrost Permafrost Research PETA-CARB Polar Terrestrial Environmental Systems @ AWI Rapid Permafrost Thaw in a Warming Arctic and Impacts on the Soil Organic Carbon Pool remote sensing river delta Time series Nitze, Ingmar Fuchs, Matthias Strauss, Jens Günther, Frank Wetterich, Sebastian Kizyakov, Alexander Fritz, Michael Opel, Thomas Grigoriev, Mikhail N Maksimov, Georgii T Laboor, Sebastian Grosse, Guido Erosion rates of the Sobo-Sise yedoma permafrost cliff in the Lena River Delta derived from remote sensing imagery |
topic_facet |
AWI_Envi AWI_Perma CACOON Carbon in Permafrost / Kohlenstoff im Permafrost Changing Arctic Carbon cycle in the cOastal Ocean Near-shore cliff erosion digital shoreline analysis system erosion rates KoPF Lena Delta NUNATARYUK Permafrost thaw and the changing Arctic coast science for socioeconomic adaptation Permafrost Permafrost Research PETA-CARB Polar Terrestrial Environmental Systems @ AWI Rapid Permafrost Thaw in a Warming Arctic and Impacts on the Soil Organic Carbon Pool remote sensing river delta Time series |
description |
Permafrost thaw and ice wedge degradation lead to drastic landscape changes in the permafrost region. With this data set we investigated the cliff retreat of the Sobo-Sise Cliff (SSC), a high ice-bearing yedoma cliff in the Lena River Delta. The 1,660 m long cliff SSC extends from 72°32'34 N / 128°15'59 E to 72°32'06 N / 128°18'21 E and is located on the Sardakhskaya channel, which is one of the main Lena river branches in the Lena River Delta. Erosion rates for the SSC were determined based on satellite images from different sensors (Corona, Hexagon, Landsat, Planet cube-sat) for the period 1965-2018. Cliff front lines were manually digitized and erosion rates were calculated with the Digital Shoreline Analysis System (DSAS) tool (Himmelstoos et al. 2018). The study Fuchs et al. (2020) (doi:10.3389/feart.2020.00336) shows that the up to 27.7 m high SSC erodes in average 15.7 m yr-1 (2015-2018). During the entire observed time period from 1965-2018, the SSC retreated in average 484 m (ranging from 322 - 680 m). This data set compilation consist of three GIS shapefiles with a corresponding metadata file and a table of the mean annual erosion rates of the yedoma SSC for the time periods 1965-1975, 1975-2000, 2000-2005, 2005-2010, 2010-2015, and 2015-2018, as well as the absolute cliff retreat rates over the entire period 1965-2018, which are derived from remote sensing imagery analyzed with the DSAS tool. In addition, the cliff front lines for each investigated time step are provided as well as the separation between yedoma and alas deposits for each time step. Related trend data for this region, based on Landsat trend analysis are available at: doi:10.1594/PANGAEA.884136 (Nitze, 2018). |
format |
Other/Unknown Material |
author |
Nitze, Ingmar Fuchs, Matthias Strauss, Jens Günther, Frank Wetterich, Sebastian Kizyakov, Alexander Fritz, Michael Opel, Thomas Grigoriev, Mikhail N Maksimov, Georgii T Laboor, Sebastian Grosse, Guido |
author_facet |
Nitze, Ingmar Fuchs, Matthias Strauss, Jens Günther, Frank Wetterich, Sebastian Kizyakov, Alexander Fritz, Michael Opel, Thomas Grigoriev, Mikhail N Maksimov, Georgii T Laboor, Sebastian Grosse, Guido |
author_sort |
Nitze, Ingmar |
title |
Erosion rates of the Sobo-Sise yedoma permafrost cliff in the Lena River Delta derived from remote sensing imagery |
title_short |
Erosion rates of the Sobo-Sise yedoma permafrost cliff in the Lena River Delta derived from remote sensing imagery |
title_full |
Erosion rates of the Sobo-Sise yedoma permafrost cliff in the Lena River Delta derived from remote sensing imagery |
title_fullStr |
Erosion rates of the Sobo-Sise yedoma permafrost cliff in the Lena River Delta derived from remote sensing imagery |
title_full_unstemmed |
Erosion rates of the Sobo-Sise yedoma permafrost cliff in the Lena River Delta derived from remote sensing imagery |
title_sort |
erosion rates of the sobo-sise yedoma permafrost cliff in the lena river delta derived from remote sensing imagery |
publisher |
PANGAEA |
publishDate |
2020 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.918507 https://doi.org/10.1594/PANGAEA.918507 |
op_coverage |
MEDIAN LATITUDE: 72.538889 * MEDIAN LONGITUDE: 128.286111 * SOUTH-BOUND LATITUDE: 72.535000 * WEST-BOUND LONGITUDE: 128.266389 * NORTH-BOUND LATITUDE: 72.542778 * EAST-BOUND LONGITUDE: 128.305833 |
long_lat |
ENVELOPE(128.266389,128.305833,72.542778,72.535000) |
genre |
Ice lena delta lena river permafrost wedge* |
genre_facet |
Ice lena delta lena river permafrost wedge* |
op_relation |
Fuchs, Matthias; Nitze, Ingmar; Strauss, Jens; Günther, Frank; Wetterich, Sebastian; Kizyakov, Alexander; Fritz, Michael; Opel, Thomas; Grigoriev, Mikhail N; Maksimov, Georgii T; Grosse, Guido (2020): Rapid Fluvio-Thermal Erosion of a Yedoma Permafrost Cliff in the Lena River Delta. Frontiers in Earth Science, 8, 336, https://doi.org/10.3389/feart.2020.00336 Himmelstoss, Emily A; Henderson, Rachel E; Kratzmann, Meredith G; Farris, Amy S (2018): Digital Shoreline Analysis System (DSAS) Version 5.0 User Guide. US Geological Survey Open-File Report 2018-1179, 110 pp, https://doi.org/10.3133/ofr20181179 Nitze, Ingmar (2018): Trends of land surface change from Landsat time-series 1999-2014, Transect T2, Eastern Siberia [dataset]. Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, PANGAEA, https://doi.org/10.1594/PANGAEA.884136 https://doi.pangaea.de/10.1594/PANGAEA.918507 https://doi.org/10.1594/PANGAEA.918507 |
op_rights |
CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.91850710.3389/feart.2020.0033610.3133/ofr2018117910.1594/PANGAEA.884136 |
_version_ |
1810449093504270336 |
spelling |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.918507 2024-09-15T18:11:30+00:00 Erosion rates of the Sobo-Sise yedoma permafrost cliff in the Lena River Delta derived from remote sensing imagery Nitze, Ingmar Fuchs, Matthias Strauss, Jens Günther, Frank Wetterich, Sebastian Kizyakov, Alexander Fritz, Michael Opel, Thomas Grigoriev, Mikhail N Maksimov, Georgii T Laboor, Sebastian Grosse, Guido MEDIAN LATITUDE: 72.538889 * MEDIAN LONGITUDE: 128.286111 * SOUTH-BOUND LATITUDE: 72.535000 * WEST-BOUND LONGITUDE: 128.266389 * NORTH-BOUND LATITUDE: 72.542778 * EAST-BOUND LONGITUDE: 128.305833 2020 application/zip, 2 datasets https://doi.pangaea.de/10.1594/PANGAEA.918507 https://doi.org/10.1594/PANGAEA.918507 en eng PANGAEA Fuchs, Matthias; Nitze, Ingmar; Strauss, Jens; Günther, Frank; Wetterich, Sebastian; Kizyakov, Alexander; Fritz, Michael; Opel, Thomas; Grigoriev, Mikhail N; Maksimov, Georgii T; Grosse, Guido (2020): Rapid Fluvio-Thermal Erosion of a Yedoma Permafrost Cliff in the Lena River Delta. Frontiers in Earth Science, 8, 336, https://doi.org/10.3389/feart.2020.00336 Himmelstoss, Emily A; Henderson, Rachel E; Kratzmann, Meredith G; Farris, Amy S (2018): Digital Shoreline Analysis System (DSAS) Version 5.0 User Guide. US Geological Survey Open-File Report 2018-1179, 110 pp, https://doi.org/10.3133/ofr20181179 Nitze, Ingmar (2018): Trends of land surface change from Landsat time-series 1999-2014, Transect T2, Eastern Siberia [dataset]. Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, PANGAEA, https://doi.org/10.1594/PANGAEA.884136 https://doi.pangaea.de/10.1594/PANGAEA.918507 https://doi.org/10.1594/PANGAEA.918507 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess AWI_Envi AWI_Perma CACOON Carbon in Permafrost / Kohlenstoff im Permafrost Changing Arctic Carbon cycle in the cOastal Ocean Near-shore cliff erosion digital shoreline analysis system erosion rates KoPF Lena Delta NUNATARYUK Permafrost thaw and the changing Arctic coast science for socioeconomic adaptation Permafrost Permafrost Research PETA-CARB Polar Terrestrial Environmental Systems @ AWI Rapid Permafrost Thaw in a Warming Arctic and Impacts on the Soil Organic Carbon Pool remote sensing river delta Time series dataset bundled publication 2020 ftpangaea https://doi.org/10.1594/PANGAEA.91850710.3389/feart.2020.0033610.3133/ofr2018117910.1594/PANGAEA.884136 2024-07-24T02:31:21Z Permafrost thaw and ice wedge degradation lead to drastic landscape changes in the permafrost region. With this data set we investigated the cliff retreat of the Sobo-Sise Cliff (SSC), a high ice-bearing yedoma cliff in the Lena River Delta. The 1,660 m long cliff SSC extends from 72°32'34 N / 128°15'59 E to 72°32'06 N / 128°18'21 E and is located on the Sardakhskaya channel, which is one of the main Lena river branches in the Lena River Delta. Erosion rates for the SSC were determined based on satellite images from different sensors (Corona, Hexagon, Landsat, Planet cube-sat) for the period 1965-2018. Cliff front lines were manually digitized and erosion rates were calculated with the Digital Shoreline Analysis System (DSAS) tool (Himmelstoos et al. 2018). The study Fuchs et al. (2020) (doi:10.3389/feart.2020.00336) shows that the up to 27.7 m high SSC erodes in average 15.7 m yr-1 (2015-2018). During the entire observed time period from 1965-2018, the SSC retreated in average 484 m (ranging from 322 - 680 m). This data set compilation consist of three GIS shapefiles with a corresponding metadata file and a table of the mean annual erosion rates of the yedoma SSC for the time periods 1965-1975, 1975-2000, 2000-2005, 2005-2010, 2010-2015, and 2015-2018, as well as the absolute cliff retreat rates over the entire period 1965-2018, which are derived from remote sensing imagery analyzed with the DSAS tool. In addition, the cliff front lines for each investigated time step are provided as well as the separation between yedoma and alas deposits for each time step. Related trend data for this region, based on Landsat trend analysis are available at: doi:10.1594/PANGAEA.884136 (Nitze, 2018). Other/Unknown Material Ice lena delta lena river permafrost wedge* PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(128.266389,128.305833,72.542778,72.535000) |