Thermokarst Lake to Lagoon Transitions in Eastern Siberia: Do Submerged Taliks Refreeze?

As the Arctic coast erodes, it drains thermokarst lakes, transforming them into lagoons, and, eventually, integrates them into subsea permafrost. Lagoons represent the first stage of a thermokarst lake transition to a marine setting and possibly more saline and colder upper boundary conditions. In t...

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Published in:Journal of Geophysical Research: Earth Surface
Main Authors: Angelopoulos, Michael, Overduin, Pier Paul, Westermann, Sebastian, Tronicke, Jens
Format: Article in Journal/Newspaper
Language:English
Published: 2021
Subjects:
Ice
Online Access:http://hdl.handle.net/10852/85798
http://urn.nb.no/URN:NBN:no-88451
https://doi.org/10.1029/2019JF005424
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spelling ftoslouniv:oai:www.duo.uio.no:10852/85798 2023-05-15T15:10:10+02:00 Thermokarst Lake to Lagoon Transitions in Eastern Siberia: Do Submerged Taliks Refreeze? Angelopoulos, Michael Overduin, Pier Paul Westermann, Sebastian Tronicke, Jens 2021-03-24T12:04:21Z http://hdl.handle.net/10852/85798 http://urn.nb.no/URN:NBN:no-88451 https://doi.org/10.1029/2019JF005424 EN eng http://urn.nb.no/URN:NBN:no-88451 Angelopoulos, Michael Overduin, Pier Paul Westermann, Sebastian Tronicke, Jens . Thermokarst Lake to Lagoon Transitions in Eastern Siberia: Do Submerged Taliks Refreeze?. Journal of Geophysical Research (JGR): Earth Surface. 2020, 125(10) http://hdl.handle.net/10852/85798 1900589 info:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Journal of Geophysical Research (JGR): Earth Surface&rft.volume=125&rft.spage=&rft.date=2020 Journal of Geophysical Research (JGR): Earth Surface 125 10 https://doi.org/10.1029/2019JF005424 URN:NBN:no-88451 Fulltext https://www.duo.uio.no/bitstream/handle/10852/85798/2/2019JF005424.pdf Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/ CC-BY 2169-9003 Journal article Tidsskriftartikkel Peer reviewed PublishedVersion 2021 ftoslouniv https://doi.org/10.1029/2019JF005424 2021-05-05T22:31:00Z As the Arctic coast erodes, it drains thermokarst lakes, transforming them into lagoons, and, eventually, integrates them into subsea permafrost. Lagoons represent the first stage of a thermokarst lake transition to a marine setting and possibly more saline and colder upper boundary conditions. In this research, borehole data, electrical resistivity surveying, and modeling of heat and salt diffusion were carried out at Polar Fox Lagoon on the Bykovsky Peninsula, Siberia. Polar Fox Lagoon is a seasonally isolated water body connected to Tiksi Bay through a channel, leading to hypersaline waters under the ice cover. The boreholes in the center of the lagoon revealed floating ice and a saline cryotic bed underlain by a saline cryotic talik, a thin ice‐bearing permafrost layer, and unfrozen ground. The bathymetry showed that most of the lagoon had bedfast ice in spring. In bedfast ice areas, the electrical resistivity profiles suggested that an unfrozen saline layer was underlain by a thick layer of refrozen talik. The modeling showed that thermokarst lake taliks can refreeze when submerged in saltwater with mean annual bottom water temperatures below or slightly above 0°C. This occurs, because the top‐down chemical degradation of newly formed ice‐bearing permafrost is slower than the refreezing of the talik. Hence, lagoons may precondition taliks with a layer of ice‐bearing permafrost before encroachment by the sea, and this frozen layer may act as a cap on gas migration out of the underlying talik. Article in Journal/Newspaper Arctic Ice permafrost polar fox Thermokarst Tiksi Tiksi Bay Siberia Universitet i Oslo: Digitale utgivelser ved UiO (DUO) Arctic Talik ENVELOPE(146.601,146.601,59.667,59.667) Tiksi ENVELOPE(128.867,128.867,71.633,71.633) Journal of Geophysical Research: Earth Surface 125 10
institution Open Polar
collection Universitet i Oslo: Digitale utgivelser ved UiO (DUO)
op_collection_id ftoslouniv
language English
description As the Arctic coast erodes, it drains thermokarst lakes, transforming them into lagoons, and, eventually, integrates them into subsea permafrost. Lagoons represent the first stage of a thermokarst lake transition to a marine setting and possibly more saline and colder upper boundary conditions. In this research, borehole data, electrical resistivity surveying, and modeling of heat and salt diffusion were carried out at Polar Fox Lagoon on the Bykovsky Peninsula, Siberia. Polar Fox Lagoon is a seasonally isolated water body connected to Tiksi Bay through a channel, leading to hypersaline waters under the ice cover. The boreholes in the center of the lagoon revealed floating ice and a saline cryotic bed underlain by a saline cryotic talik, a thin ice‐bearing permafrost layer, and unfrozen ground. The bathymetry showed that most of the lagoon had bedfast ice in spring. In bedfast ice areas, the electrical resistivity profiles suggested that an unfrozen saline layer was underlain by a thick layer of refrozen talik. The modeling showed that thermokarst lake taliks can refreeze when submerged in saltwater with mean annual bottom water temperatures below or slightly above 0°C. This occurs, because the top‐down chemical degradation of newly formed ice‐bearing permafrost is slower than the refreezing of the talik. Hence, lagoons may precondition taliks with a layer of ice‐bearing permafrost before encroachment by the sea, and this frozen layer may act as a cap on gas migration out of the underlying talik.
format Article in Journal/Newspaper
author Angelopoulos, Michael
Overduin, Pier Paul
Westermann, Sebastian
Tronicke, Jens
spellingShingle Angelopoulos, Michael
Overduin, Pier Paul
Westermann, Sebastian
Tronicke, Jens
Thermokarst Lake to Lagoon Transitions in Eastern Siberia: Do Submerged Taliks Refreeze?
author_facet Angelopoulos, Michael
Overduin, Pier Paul
Westermann, Sebastian
Tronicke, Jens
author_sort Angelopoulos, Michael
title Thermokarst Lake to Lagoon Transitions in Eastern Siberia: Do Submerged Taliks Refreeze?
title_short Thermokarst Lake to Lagoon Transitions in Eastern Siberia: Do Submerged Taliks Refreeze?
title_full Thermokarst Lake to Lagoon Transitions in Eastern Siberia: Do Submerged Taliks Refreeze?
title_fullStr Thermokarst Lake to Lagoon Transitions in Eastern Siberia: Do Submerged Taliks Refreeze?
title_full_unstemmed Thermokarst Lake to Lagoon Transitions in Eastern Siberia: Do Submerged Taliks Refreeze?
title_sort thermokarst lake to lagoon transitions in eastern siberia: do submerged taliks refreeze?
publishDate 2021
url http://hdl.handle.net/10852/85798
http://urn.nb.no/URN:NBN:no-88451
https://doi.org/10.1029/2019JF005424
long_lat ENVELOPE(146.601,146.601,59.667,59.667)
ENVELOPE(128.867,128.867,71.633,71.633)
geographic Arctic
Talik
Tiksi
geographic_facet Arctic
Talik
Tiksi
genre Arctic
Ice
permafrost
polar fox
Thermokarst
Tiksi
Tiksi Bay
Siberia
genre_facet Arctic
Ice
permafrost
polar fox
Thermokarst
Tiksi
Tiksi Bay
Siberia
op_source 2169-9003
op_relation http://urn.nb.no/URN:NBN:no-88451
Angelopoulos, Michael Overduin, Pier Paul Westermann, Sebastian Tronicke, Jens . Thermokarst Lake to Lagoon Transitions in Eastern Siberia: Do Submerged Taliks Refreeze?. Journal of Geophysical Research (JGR): Earth Surface. 2020, 125(10)
http://hdl.handle.net/10852/85798
1900589
info:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Journal of Geophysical Research (JGR): Earth Surface&rft.volume=125&rft.spage=&rft.date=2020
Journal of Geophysical Research (JGR): Earth Surface
125
10
https://doi.org/10.1029/2019JF005424
URN:NBN:no-88451
Fulltext https://www.duo.uio.no/bitstream/handle/10852/85798/2/2019JF005424.pdf
op_rights Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/
op_rightsnorm CC-BY
op_doi https://doi.org/10.1029/2019JF005424
container_title Journal of Geophysical Research: Earth Surface
container_volume 125
container_issue 10
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