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 rst stage of a thermokarst lake transition to amarine setting and possibly more saline and colder upper boundary conditions. In this...

Full description

Bibliographic Details
Published in:Journal of Geophysical Research: Earth Surface
Main Authors: Angelopoulos, M., Overduin, P., Westermann, S., Tronicke, J., Strauss, J., Schirrmeister, L., Biskaborn, B.K., Liebner, S., Maksimov, G., Grigoriev, M.N., Grosse, G.
Format: Article in Journal/Newspaper
Language:unknown
Published: Zenodo 2020
Subjects:
Ice
Online Access:https://doi.org/10.1029/2019JF005424
id ftzenodo:oai:zenodo.org:4270447
record_format openpolar
spelling ftzenodo:oai:zenodo.org:4270447 2024-09-15T18:11:23+00:00 Thermokarst lake to lagoon transitions in eastern Siberia: Do submerged taliks refreeze? Angelopoulos, M. Overduin, P. Westermann, S. Tronicke, J. Strauss, J. Schirrmeister, L. Biskaborn, B.K. Liebner, S. Maksimov, G. Grigoriev, M.N. Grosse, G. 2020-07-20 https://doi.org/10.1029/2019JF005424 unknown Zenodo https://zenodo.org/communities/nunataryuk https://doi.org/10.1029/2019JF005424 oai:zenodo.org:4270447 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode info:eu-repo/semantics/article 2020 ftzenodo https://doi.org/10.1029/2019JF005424 2024-07-26T00:27:51Z As the Arctic coast erodes, it drains thermokarst lakes, transforming them into lagoons, and, eventually,integrates them into subsea permafrost. Lagoons represent the rst stage of a thermokarst lake transition to amarine 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 atPolar Fox Lagoon on the Bykovsky Peninsula, Siberia. Polar Fox Lagoon is a seasonally isolated waterbody connected to Tiksi Bay through a channel, leading to hypersaline waters under the ice cover.The boreholes in the center of the lagoon revealed oating ice and a saline cryotic bed underlain by asaline cryotic talik, a thin icebearing permafrost layer, and unfrozen ground. The bathymetry showedthat most of the lagoon had bedfast ice in spring. In bedfast ice areas, the electrical resistivity profilessuggested that an unfrozen saline layer was underlain by a thick layer of refrozen talik. The modelingshowed that thermokarst lake taliks can refreeze when submerged in saltwater with mean annual bottomwater temperatures below or slightly above 0°C. This occurs, because the top-down chemical degradationof newly formed icebearing permafrost is slower than the refreezing of the talik. Hence, lagoons mayprecondition taliks with a layer of ice-bearing permafrost before encroachment by the sea, and this frozenlayer may act as a cap on gas migration out of the underlying talik. Article in Journal/Newspaper Ice permafrost polar fox Thermokarst Tiksi Tiksi Bay Siberia Zenodo Journal of Geophysical Research: Earth Surface 125 10
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
description As the Arctic coast erodes, it drains thermokarst lakes, transforming them into lagoons, and, eventually,integrates them into subsea permafrost. Lagoons represent the rst stage of a thermokarst lake transition to amarine 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 atPolar Fox Lagoon on the Bykovsky Peninsula, Siberia. Polar Fox Lagoon is a seasonally isolated waterbody connected to Tiksi Bay through a channel, leading to hypersaline waters under the ice cover.The boreholes in the center of the lagoon revealed oating ice and a saline cryotic bed underlain by asaline cryotic talik, a thin icebearing permafrost layer, and unfrozen ground. The bathymetry showedthat most of the lagoon had bedfast ice in spring. In bedfast ice areas, the electrical resistivity profilessuggested that an unfrozen saline layer was underlain by a thick layer of refrozen talik. The modelingshowed that thermokarst lake taliks can refreeze when submerged in saltwater with mean annual bottomwater temperatures below or slightly above 0°C. This occurs, because the top-down chemical degradationof newly formed icebearing permafrost is slower than the refreezing of the talik. Hence, lagoons mayprecondition taliks with a layer of ice-bearing permafrost before encroachment by the sea, and this frozenlayer may act as a cap on gas migration out of the underlying talik.
format Article in Journal/Newspaper
author Angelopoulos, M.
Overduin, P.
Westermann, S.
Tronicke, J.
Strauss, J.
Schirrmeister, L.
Biskaborn, B.K.
Liebner, S.
Maksimov, G.
Grigoriev, M.N.
Grosse, G.
spellingShingle Angelopoulos, M.
Overduin, P.
Westermann, S.
Tronicke, J.
Strauss, J.
Schirrmeister, L.
Biskaborn, B.K.
Liebner, S.
Maksimov, G.
Grigoriev, M.N.
Grosse, G.
Thermokarst lake to lagoon transitions in eastern Siberia: Do submerged taliks refreeze?
author_facet Angelopoulos, M.
Overduin, P.
Westermann, S.
Tronicke, J.
Strauss, J.
Schirrmeister, L.
Biskaborn, B.K.
Liebner, S.
Maksimov, G.
Grigoriev, M.N.
Grosse, G.
author_sort Angelopoulos, M.
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?
publisher Zenodo
publishDate 2020
url https://doi.org/10.1029/2019JF005424
genre Ice
permafrost
polar fox
Thermokarst
Tiksi
Tiksi Bay
Siberia
genre_facet Ice
permafrost
polar fox
Thermokarst
Tiksi
Tiksi Bay
Siberia
op_relation https://zenodo.org/communities/nunataryuk
https://doi.org/10.1029/2019JF005424
oai:zenodo.org:4270447
op_rights info:eu-repo/semantics/openAccess
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.1029/2019JF005424
container_title Journal of Geophysical Research: Earth Surface
container_volume 125
container_issue 10
_version_ 1810448969185099776