In situ measurements of freeze/thaw ground displacement in the Lena River Delta, 2013-2017, using fiberglass rods

In permafrost areas, seasonal freeze-thaw cycles of active layer result in upward and downward movements of the ground. Additionally, relatively uniform thawing of the ice-rich layer at the permafrost table can contribute to net long-term surface lowering. We use a simple method to quantify surface...

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Main Authors: Antonova, Sofia, Sudhaus, Henriette, Strozzi, Tazio, Zwieback, Simon, Kääb, Andreas, Heim, Birgit, Langer, Moritz, Bornemann, Niko, Boike, Julia
Format: Dataset
Language:English
Published: PANGAEA - Data Publisher for Earth & Environmental Science 2018
Subjects:
Ice
Online Access:https://dx.doi.org/10.1594/pangaea.894716
https://doi.pangaea.de/10.1594/PANGAEA.894716
id ftdatacite:10.1594/pangaea.894716
record_format openpolar
spelling ftdatacite:10.1594/pangaea.894716 2023-05-15T15:17:26+02:00 In situ measurements of freeze/thaw ground displacement in the Lena River Delta, 2013-2017, using fiberglass rods Antonova, Sofia Sudhaus, Henriette Strozzi, Tazio Zwieback, Simon Kääb, Andreas Heim, Birgit Langer, Moritz Bornemann, Niko Boike, Julia 2018 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.894716 https://doi.pangaea.de/10.1594/PANGAEA.894716 en eng PANGAEA - Data Publisher for Earth & Environmental Science https://store.pangaea.de/Publications/Antonova-etal_2018/Antonova_2018_LenaDelta_subsidence_2013-2017_method.pdf https://dx.doi.org/10.1594/pangaea.894717 https://dx.doi.org/10.3390/rs10040494 https://store.pangaea.de/Publications/Antonova-etal_2018/Antonova_2018_LenaDelta_subsidence_2013-2017_method.pdf Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY Event label Station label DATE/TIME DISTANCE Sampling/measurement on land Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn dataset Dataset 2018 ftdatacite https://doi.org/10.1594/pangaea.894716 https://doi.org/10.1594/pangaea.894717 https://doi.org/10.3390/rs10040494 2021-11-05T12:55:41Z In permafrost areas, seasonal freeze-thaw cycles of active layer result in upward and downward movements of the ground. Additionally, relatively uniform thawing of the ice-rich layer at the permafrost table can contribute to net long-term surface lowering. We use a simple method to quantify surface lowering (subsidence) and uplift in a yedoma area of the Lena River Delta, Siberian Arctic (Kurungnakh Island), using reference rods (metal pipes and fiberglass rods) installed deeply in permafrost. The metal pipes were 2 m long and 3 cm in diameter and were anchored at least 1 m below the typical active layer. The fiberglass rods were 2 m long and 1 cm in diameter and were anchored at least 70 m below the typical active layer. We assume, therefore, that the rods were motionless relative to the permafrost. The plexiglass plate with a size of 10 by 10 cm was fixed in its horizontal position by the rod but could move freely with the surface vertically along the rod. We repeatedly measured distance between the top of a rod and a plexiglass plate resting on the ground surface. Several distance measurements around each rod were taken at each visit and averaged. Altogether 12 metal pipes were installed at the study site in April 2013 and 19 fiberglass rods were installed in April 2014. Measurements were conducted during field campaigns from spring 2013 to summer 2017 with some gaps. We provide here the measured distances between the top of a rod and a plexiglass plate. To obtain the ground displacement, the user have to define the period of interest and calculate the displacement. : Measurements are the distances between the ground surface and the top of the fiberglass rod, in cm. To obtain the displacement, you need to subtract the measurement on a certain date from the reference measurement (e.g. from the very first one). Dataset Arctic Ice lena river permafrost DataCite Metadata Store (German National Library of Science and Technology) Arctic
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Event label
Station label
DATE/TIME
DISTANCE
Sampling/measurement on land
Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn
spellingShingle Event label
Station label
DATE/TIME
DISTANCE
Sampling/measurement on land
Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn
Antonova, Sofia
Sudhaus, Henriette
Strozzi, Tazio
Zwieback, Simon
Kääb, Andreas
Heim, Birgit
Langer, Moritz
Bornemann, Niko
Boike, Julia
In situ measurements of freeze/thaw ground displacement in the Lena River Delta, 2013-2017, using fiberglass rods
topic_facet Event label
Station label
DATE/TIME
DISTANCE
Sampling/measurement on land
Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn
description In permafrost areas, seasonal freeze-thaw cycles of active layer result in upward and downward movements of the ground. Additionally, relatively uniform thawing of the ice-rich layer at the permafrost table can contribute to net long-term surface lowering. We use a simple method to quantify surface lowering (subsidence) and uplift in a yedoma area of the Lena River Delta, Siberian Arctic (Kurungnakh Island), using reference rods (metal pipes and fiberglass rods) installed deeply in permafrost. The metal pipes were 2 m long and 3 cm in diameter and were anchored at least 1 m below the typical active layer. The fiberglass rods were 2 m long and 1 cm in diameter and were anchored at least 70 m below the typical active layer. We assume, therefore, that the rods were motionless relative to the permafrost. The plexiglass plate with a size of 10 by 10 cm was fixed in its horizontal position by the rod but could move freely with the surface vertically along the rod. We repeatedly measured distance between the top of a rod and a plexiglass plate resting on the ground surface. Several distance measurements around each rod were taken at each visit and averaged. Altogether 12 metal pipes were installed at the study site in April 2013 and 19 fiberglass rods were installed in April 2014. Measurements were conducted during field campaigns from spring 2013 to summer 2017 with some gaps. We provide here the measured distances between the top of a rod and a plexiglass plate. To obtain the ground displacement, the user have to define the period of interest and calculate the displacement. : Measurements are the distances between the ground surface and the top of the fiberglass rod, in cm. To obtain the displacement, you need to subtract the measurement on a certain date from the reference measurement (e.g. from the very first one).
format Dataset
author Antonova, Sofia
Sudhaus, Henriette
Strozzi, Tazio
Zwieback, Simon
Kääb, Andreas
Heim, Birgit
Langer, Moritz
Bornemann, Niko
Boike, Julia
author_facet Antonova, Sofia
Sudhaus, Henriette
Strozzi, Tazio
Zwieback, Simon
Kääb, Andreas
Heim, Birgit
Langer, Moritz
Bornemann, Niko
Boike, Julia
author_sort Antonova, Sofia
title In situ measurements of freeze/thaw ground displacement in the Lena River Delta, 2013-2017, using fiberglass rods
title_short In situ measurements of freeze/thaw ground displacement in the Lena River Delta, 2013-2017, using fiberglass rods
title_full In situ measurements of freeze/thaw ground displacement in the Lena River Delta, 2013-2017, using fiberglass rods
title_fullStr In situ measurements of freeze/thaw ground displacement in the Lena River Delta, 2013-2017, using fiberglass rods
title_full_unstemmed In situ measurements of freeze/thaw ground displacement in the Lena River Delta, 2013-2017, using fiberglass rods
title_sort in situ measurements of freeze/thaw ground displacement in the lena river delta, 2013-2017, using fiberglass rods
publisher PANGAEA - Data Publisher for Earth & Environmental Science
publishDate 2018
url https://dx.doi.org/10.1594/pangaea.894716
https://doi.pangaea.de/10.1594/PANGAEA.894716
geographic Arctic
geographic_facet Arctic
genre Arctic
Ice
lena river
permafrost
genre_facet Arctic
Ice
lena river
permafrost
op_relation https://store.pangaea.de/Publications/Antonova-etal_2018/Antonova_2018_LenaDelta_subsidence_2013-2017_method.pdf
https://dx.doi.org/10.1594/pangaea.894717
https://dx.doi.org/10.3390/rs10040494
https://store.pangaea.de/Publications/Antonova-etal_2018/Antonova_2018_LenaDelta_subsidence_2013-2017_method.pdf
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/pangaea.894716
https://doi.org/10.1594/pangaea.894717
https://doi.org/10.3390/rs10040494
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