Hydrothermal Dynamics of Seasonally Frozen Soil With Different Vegetation Coverage in the Tianshan Mountains

The hydrothermal relationship between vegetation and seasonal frozen soil is one of the key research contents in the fields of permafrost ecological environment, hydrology and climate change in alpine mountainous areas. Based on the monitoring data of air temperature, precipitation and soil hydrothe...

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Published in:Frontiers in Earth Science
Main Authors: Ma, Shen, Yang, Bin, Zhao, Jingyi, Tan, Changhai, Chen, Ji, Mei, Qihang, Hou, Xin
Format: Article in Journal/Newspaper
Language:unknown
Published: Frontiers Media SA 2022
Subjects:
Online Access:http://dx.doi.org/10.3389/feart.2021.806309
https://www.frontiersin.org/articles/10.3389/feart.2021.806309/full
id crfrontiers:10.3389/feart.2021.806309
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spelling crfrontiers:10.3389/feart.2021.806309 2024-06-23T07:56:09+00:00 Hydrothermal Dynamics of Seasonally Frozen Soil With Different Vegetation Coverage in the Tianshan Mountains Ma, Shen Yang, Bin Zhao, Jingyi Tan, Changhai Chen, Ji Mei, Qihang Hou, Xin 2022 http://dx.doi.org/10.3389/feart.2021.806309 https://www.frontiersin.org/articles/10.3389/feart.2021.806309/full unknown Frontiers Media SA https://creativecommons.org/licenses/by/4.0/ Frontiers in Earth Science volume 9 ISSN 2296-6463 journal-article 2022 crfrontiers https://doi.org/10.3389/feart.2021.806309 2024-06-11T04:09:20Z The hydrothermal relationship between vegetation and seasonal frozen soil is one of the key research contents in the fields of permafrost ecological environment, hydrology and climate change in alpine mountainous areas. Based on the monitoring data of air temperature, precipitation and soil hydrothermal conditions at the depth of 0–5 m from site TS-04 (with high vegetation coverage) and site TS-05 (with low vegetation coverage) in the alpine grassland of the Tianshan Mountains, this study compared and analyzed the characteristics of freezing-thawing process, temperature and moisture changes of seasonal frozen soil with different vegetation coverage. The results show that the maximum seasonal freezing depth of the two sites is almost comparable, but site TS-04 has a smaller freezing and thawing rate, and a shorter duration of freeze-thaw at all depths. TS-04 also has a smaller annual range of surface temperature and ground-air temperature difference. The analysis indicates that vegetation acts as a thermal buffer and has a good thermal insulation effect on the ground surface. Site TS-04 had high unfrozen water content in the unfrozen period and the water content increased with depth, while the unfrozen water content was low in site TS-05. In addition, the thresholds of soil water content response to rainfall events at 5 cm depth of site TS-04 and site TS-05 were 5 and 11 mm precipitation respectively, which indicated that the high vegetation coverage is conducive to rainwater infiltration, and the underlying soil of the site has a faster response to rainfall events. Article in Journal/Newspaper permafrost Frontiers (Publisher) Frontiers in Earth Science 9
institution Open Polar
collection Frontiers (Publisher)
op_collection_id crfrontiers
language unknown
description The hydrothermal relationship between vegetation and seasonal frozen soil is one of the key research contents in the fields of permafrost ecological environment, hydrology and climate change in alpine mountainous areas. Based on the monitoring data of air temperature, precipitation and soil hydrothermal conditions at the depth of 0–5 m from site TS-04 (with high vegetation coverage) and site TS-05 (with low vegetation coverage) in the alpine grassland of the Tianshan Mountains, this study compared and analyzed the characteristics of freezing-thawing process, temperature and moisture changes of seasonal frozen soil with different vegetation coverage. The results show that the maximum seasonal freezing depth of the two sites is almost comparable, but site TS-04 has a smaller freezing and thawing rate, and a shorter duration of freeze-thaw at all depths. TS-04 also has a smaller annual range of surface temperature and ground-air temperature difference. The analysis indicates that vegetation acts as a thermal buffer and has a good thermal insulation effect on the ground surface. Site TS-04 had high unfrozen water content in the unfrozen period and the water content increased with depth, while the unfrozen water content was low in site TS-05. In addition, the thresholds of soil water content response to rainfall events at 5 cm depth of site TS-04 and site TS-05 were 5 and 11 mm precipitation respectively, which indicated that the high vegetation coverage is conducive to rainwater infiltration, and the underlying soil of the site has a faster response to rainfall events.
format Article in Journal/Newspaper
author Ma, Shen
Yang, Bin
Zhao, Jingyi
Tan, Changhai
Chen, Ji
Mei, Qihang
Hou, Xin
spellingShingle Ma, Shen
Yang, Bin
Zhao, Jingyi
Tan, Changhai
Chen, Ji
Mei, Qihang
Hou, Xin
Hydrothermal Dynamics of Seasonally Frozen Soil With Different Vegetation Coverage in the Tianshan Mountains
author_facet Ma, Shen
Yang, Bin
Zhao, Jingyi
Tan, Changhai
Chen, Ji
Mei, Qihang
Hou, Xin
author_sort Ma, Shen
title Hydrothermal Dynamics of Seasonally Frozen Soil With Different Vegetation Coverage in the Tianshan Mountains
title_short Hydrothermal Dynamics of Seasonally Frozen Soil With Different Vegetation Coverage in the Tianshan Mountains
title_full Hydrothermal Dynamics of Seasonally Frozen Soil With Different Vegetation Coverage in the Tianshan Mountains
title_fullStr Hydrothermal Dynamics of Seasonally Frozen Soil With Different Vegetation Coverage in the Tianshan Mountains
title_full_unstemmed Hydrothermal Dynamics of Seasonally Frozen Soil With Different Vegetation Coverage in the Tianshan Mountains
title_sort hydrothermal dynamics of seasonally frozen soil with different vegetation coverage in the tianshan mountains
publisher Frontiers Media SA
publishDate 2022
url http://dx.doi.org/10.3389/feart.2021.806309
https://www.frontiersin.org/articles/10.3389/feart.2021.806309/full
genre permafrost
genre_facet permafrost
op_source Frontiers in Earth Science
volume 9
ISSN 2296-6463
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3389/feart.2021.806309
container_title Frontiers in Earth Science
container_volume 9
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