A new Stefan equation to characterize the evolution of thermokarst lake and talik geometry

Thermokarst lake dynamics, which play an essential role in carbon release due to permafrost thaw, are affected by various geomorphological processes. In this study, we derive a three-dimensional (3D) Stefan equation to characterize talik geometry under a hypothetical thermokarst lake in the continuo...

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Published in:The Cryosphere
Main Authors: N. Ohara, B. M. Jones, A. D. Parsekian, K. M. Hinkel, K. Yamatani, M. Kanevskiy, R. C. Rangel, A. L. Breen, H. Bergstedt
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2022
Subjects:
Ice
Online Access:https://doi.org/10.5194/tc-16-1247-2022
https://doaj.org/article/76ec342707ac4821aa78d08e62f3d8fa
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spelling ftdoajarticles:oai:doaj.org/article:76ec342707ac4821aa78d08e62f3d8fa 2023-05-15T15:09:59+02:00 A new Stefan equation to characterize the evolution of thermokarst lake and talik geometry N. Ohara B. M. Jones A. D. Parsekian K. M. Hinkel K. Yamatani M. Kanevskiy R. C. Rangel A. L. Breen H. Bergstedt 2022-04-01T00:00:00Z https://doi.org/10.5194/tc-16-1247-2022 https://doaj.org/article/76ec342707ac4821aa78d08e62f3d8fa EN eng Copernicus Publications https://tc.copernicus.org/articles/16/1247/2022/tc-16-1247-2022.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-16-1247-2022 1994-0416 1994-0424 https://doaj.org/article/76ec342707ac4821aa78d08e62f3d8fa The Cryosphere, Vol 16, Pp 1247-1264 (2022) Environmental sciences GE1-350 Geology QE1-996.5 article 2022 ftdoajarticles https://doi.org/10.5194/tc-16-1247-2022 2022-12-31T08:02:41Z Thermokarst lake dynamics, which play an essential role in carbon release due to permafrost thaw, are affected by various geomorphological processes. In this study, we derive a three-dimensional (3D) Stefan equation to characterize talik geometry under a hypothetical thermokarst lake in the continuous permafrost region. Using the Euler equation in the calculus of variations, the lower bounds of the talik were determined as an extremum of the functional describing the phase boundary area with a fixed total talik volume. We demonstrate that the semi-ellipsoid geometry of the talik is optimal for minimizing the total permafrost thaw under the lake for a given annual heat supply. The model predicting ellipsoidal talik geometry was compared to talik thickness observations using transient electromagnetic (TEM) soundings in Peatball Lake on the Arctic Coastal Plain (ACP) of northern Alaska. The depth : width ratio of the elliptical sub-lake talik can characterize the energy flux anisotropy in the permafrost, although the lake bathymetry cross section may not be elliptic due to the presence of near-surface ice-rich permafrost. This theory suggests that talik development deepens lakes and results in more uniform horizontal lake expansion around the perimeter of the lakes, while wind-induced waves and currents are likely responsible for the elongation and orientation of shallow thermokarst lakes without taliks in certain regions such as the ACP of northern Alaska. Article in Journal/Newspaper Arctic Ice permafrost The Cryosphere Thermokarst Alaska Directory of Open Access Journals: DOAJ Articles Arctic Talik ENVELOPE(146.601,146.601,59.667,59.667) The Cryosphere 16 4 1247 1264
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental sciences
GE1-350
Geology
QE1-996.5
spellingShingle Environmental sciences
GE1-350
Geology
QE1-996.5
N. Ohara
B. M. Jones
A. D. Parsekian
K. M. Hinkel
K. Yamatani
M. Kanevskiy
R. C. Rangel
A. L. Breen
H. Bergstedt
A new Stefan equation to characterize the evolution of thermokarst lake and talik geometry
topic_facet Environmental sciences
GE1-350
Geology
QE1-996.5
description Thermokarst lake dynamics, which play an essential role in carbon release due to permafrost thaw, are affected by various geomorphological processes. In this study, we derive a three-dimensional (3D) Stefan equation to characterize talik geometry under a hypothetical thermokarst lake in the continuous permafrost region. Using the Euler equation in the calculus of variations, the lower bounds of the talik were determined as an extremum of the functional describing the phase boundary area with a fixed total talik volume. We demonstrate that the semi-ellipsoid geometry of the talik is optimal for minimizing the total permafrost thaw under the lake for a given annual heat supply. The model predicting ellipsoidal talik geometry was compared to talik thickness observations using transient electromagnetic (TEM) soundings in Peatball Lake on the Arctic Coastal Plain (ACP) of northern Alaska. The depth : width ratio of the elliptical sub-lake talik can characterize the energy flux anisotropy in the permafrost, although the lake bathymetry cross section may not be elliptic due to the presence of near-surface ice-rich permafrost. This theory suggests that talik development deepens lakes and results in more uniform horizontal lake expansion around the perimeter of the lakes, while wind-induced waves and currents are likely responsible for the elongation and orientation of shallow thermokarst lakes without taliks in certain regions such as the ACP of northern Alaska.
format Article in Journal/Newspaper
author N. Ohara
B. M. Jones
A. D. Parsekian
K. M. Hinkel
K. Yamatani
M. Kanevskiy
R. C. Rangel
A. L. Breen
H. Bergstedt
author_facet N. Ohara
B. M. Jones
A. D. Parsekian
K. M. Hinkel
K. Yamatani
M. Kanevskiy
R. C. Rangel
A. L. Breen
H. Bergstedt
author_sort N. Ohara
title A new Stefan equation to characterize the evolution of thermokarst lake and talik geometry
title_short A new Stefan equation to characterize the evolution of thermokarst lake and talik geometry
title_full A new Stefan equation to characterize the evolution of thermokarst lake and talik geometry
title_fullStr A new Stefan equation to characterize the evolution of thermokarst lake and talik geometry
title_full_unstemmed A new Stefan equation to characterize the evolution of thermokarst lake and talik geometry
title_sort new stefan equation to characterize the evolution of thermokarst lake and talik geometry
publisher Copernicus Publications
publishDate 2022
url https://doi.org/10.5194/tc-16-1247-2022
https://doaj.org/article/76ec342707ac4821aa78d08e62f3d8fa
long_lat ENVELOPE(146.601,146.601,59.667,59.667)
geographic Arctic
Talik
geographic_facet Arctic
Talik
genre Arctic
Ice
permafrost
The Cryosphere
Thermokarst
Alaska
genre_facet Arctic
Ice
permafrost
The Cryosphere
Thermokarst
Alaska
op_source The Cryosphere, Vol 16, Pp 1247-1264 (2022)
op_relation https://tc.copernicus.org/articles/16/1247/2022/tc-16-1247-2022.pdf
https://doaj.org/toc/1994-0416
https://doaj.org/toc/1994-0424
doi:10.5194/tc-16-1247-2022
1994-0416
1994-0424
https://doaj.org/article/76ec342707ac4821aa78d08e62f3d8fa
op_doi https://doi.org/10.5194/tc-16-1247-2022
container_title The Cryosphere
container_volume 16
container_issue 4
container_start_page 1247
op_container_end_page 1264
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