An Analytical Model of Active Layer Depth under Changing Ground Heat Flux
A physically based analytical model is formulated to simulate the thaw depth of active layer under changing boundary condition of soil heat flux. The energy conservation statement leads to a nonlinear integral equation of the thaw depth using an approximate temperature profile as an analytical solut...
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Authorea, Inc.
2023
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Online Access: | http://dx.doi.org/10.22541/essoar.168748466.69870560/v1 |
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crwinnower:10.22541/essoar.168748466.69870560/v1 2024-06-02T08:02:00+00:00 An Analytical Model of Active Layer Depth under Changing Ground Heat Flux ZHU, Modi Wang, Jingfeng Ivanov, Valeriy Yuryevich Sheshukov, Aleksey Y Zhou, Wenbo Zhang, Liujing Mazepa, Valeriy Sokolov, Alexandr Valdayskikh, Victor 2023 http://dx.doi.org/10.22541/essoar.168748466.69870560/v1 unknown Authorea, Inc. posted-content 2023 crwinnower https://doi.org/10.22541/essoar.168748466.69870560/v1 2024-05-07T14:19:16Z A physically based analytical model is formulated to simulate the thaw depth of active layer under changing boundary condition of soil heat flux. The energy conservation statement leads to a nonlinear integral equation of the thaw depth using an approximate temperature profile as an analytical solution of the diffusion equation describing the heat transfer in the active layer. The time-varying soil surface heat flux is estimated using non-gradient models when field observations are not available. The proposed model was validated against field observations at three Arctic forest and tundra sites. The simulated thaw depth and soil temperature profiles are in good agreement with observations hinting the potential for model application at larger spatial scales. Other/Unknown Material Arctic Tundra The Winnower Arctic |
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Open Polar |
collection |
The Winnower |
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crwinnower |
language |
unknown |
description |
A physically based analytical model is formulated to simulate the thaw depth of active layer under changing boundary condition of soil heat flux. The energy conservation statement leads to a nonlinear integral equation of the thaw depth using an approximate temperature profile as an analytical solution of the diffusion equation describing the heat transfer in the active layer. The time-varying soil surface heat flux is estimated using non-gradient models when field observations are not available. The proposed model was validated against field observations at three Arctic forest and tundra sites. The simulated thaw depth and soil temperature profiles are in good agreement with observations hinting the potential for model application at larger spatial scales. |
format |
Other/Unknown Material |
author |
ZHU, Modi Wang, Jingfeng Ivanov, Valeriy Yuryevich Sheshukov, Aleksey Y Zhou, Wenbo Zhang, Liujing Mazepa, Valeriy Sokolov, Alexandr Valdayskikh, Victor |
spellingShingle |
ZHU, Modi Wang, Jingfeng Ivanov, Valeriy Yuryevich Sheshukov, Aleksey Y Zhou, Wenbo Zhang, Liujing Mazepa, Valeriy Sokolov, Alexandr Valdayskikh, Victor An Analytical Model of Active Layer Depth under Changing Ground Heat Flux |
author_facet |
ZHU, Modi Wang, Jingfeng Ivanov, Valeriy Yuryevich Sheshukov, Aleksey Y Zhou, Wenbo Zhang, Liujing Mazepa, Valeriy Sokolov, Alexandr Valdayskikh, Victor |
author_sort |
ZHU, Modi |
title |
An Analytical Model of Active Layer Depth under Changing Ground Heat Flux |
title_short |
An Analytical Model of Active Layer Depth under Changing Ground Heat Flux |
title_full |
An Analytical Model of Active Layer Depth under Changing Ground Heat Flux |
title_fullStr |
An Analytical Model of Active Layer Depth under Changing Ground Heat Flux |
title_full_unstemmed |
An Analytical Model of Active Layer Depth under Changing Ground Heat Flux |
title_sort |
analytical model of active layer depth under changing ground heat flux |
publisher |
Authorea, Inc. |
publishDate |
2023 |
url |
http://dx.doi.org/10.22541/essoar.168748466.69870560/v1 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Tundra |
genre_facet |
Arctic Tundra |
op_doi |
https://doi.org/10.22541/essoar.168748466.69870560/v1 |
_version_ |
1800746501756944384 |