Research on Influencing Factors of Freezing and Thawing Process in the regions over 5000 m a.s.l

The freezing and thawing process is a unique feature of the alpine permafrost ecosystem, which controls the growth of microorganisms and alpine meadows, and plays a vital role in animal husbandry development, ecosystem functions and services. Meanwhile, the freezing and thawing process is also affec...

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Published in:E3S Web of Conferences
Main Authors: Man Zihao, Che Shengquan, Jiang Ruiyuan, Xie Changkun
Format: Article in Journal/Newspaper
Language:English
French
Published: EDP Sciences 2023
Subjects:
Online Access:https://doi.org/10.1051/e3sconf/202339301011
https://doaj.org/article/bf8e61018d1e48098dbb46db59877a1f
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spelling ftdoajarticles:oai:doaj.org/article:bf8e61018d1e48098dbb46db59877a1f 2023-07-02T03:33:27+02:00 Research on Influencing Factors of Freezing and Thawing Process in the regions over 5000 m a.s.l Man Zihao Che Shengquan Jiang Ruiyuan Xie Changkun 2023-01-01T00:00:00Z https://doi.org/10.1051/e3sconf/202339301011 https://doaj.org/article/bf8e61018d1e48098dbb46db59877a1f EN FR eng fre EDP Sciences https://www.e3s-conferences.org/articles/e3sconf/pdf/2023/30/e3sconf_eppct2023_01011.pdf https://doaj.org/toc/2267-1242 2267-1242 doi:10.1051/e3sconf/202339301011 https://doaj.org/article/bf8e61018d1e48098dbb46db59877a1f E3S Web of Conferences, Vol 393, p 01011 (2023) Environmental sciences GE1-350 article 2023 ftdoajarticles https://doi.org/10.1051/e3sconf/202339301011 2023-06-11T00:34:25Z The freezing and thawing process is a unique feature of the alpine permafrost ecosystem, which controls the growth of microorganisms and alpine meadows, and plays a vital role in animal husbandry development, ecosystem functions and services. Meanwhile, the freezing and thawing process is also affected by external environmental factors, and its spatial differences are very significant, especially in the regions over 5000 m a.s.l. In this study, the freezing and thawing process periods of the Cuoma Township (CM), Xiangmao Township (XM) and Xiaotanggula Mountain (XTGL) sites in the Nagqu River Basin are divided, the effects of altitude, vegetation coverage, air temperature, and organic matter content on the freezing and thawing process are analyzed, the main influencing factors are discussed. The results show that in the regions over 5000 m a.s.l, the thaw initiation period (TIP) starts in early April, the entirely thawed period (ETP) starts in end of May, the freeze initiation period (FIP) starts in end of October, and the entirely frozen period (EFP) starts in early November. Compared with the regions below 5000 m a.s.l, FIP and EFP in the regions over 5000 m a.s.l start earlier, the TIP starts later and the freezing rate is faster. Organic matter content is the main influencing factor during FIP and EFP, and air temperature is the main influencing factor during TIP and ETP. This study is helpful to clarify the changes of freezing and thawing process in the regions over 5000 m a.s.l, and also provides theoretical support for ecological protection and restoration. Article in Journal/Newspaper permafrost Directory of Open Access Journals: DOAJ Articles E3S Web of Conferences 393 01011
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
French
topic Environmental sciences
GE1-350
spellingShingle Environmental sciences
GE1-350
Man Zihao
Che Shengquan
Jiang Ruiyuan
Xie Changkun
Research on Influencing Factors of Freezing and Thawing Process in the regions over 5000 m a.s.l
topic_facet Environmental sciences
GE1-350
description The freezing and thawing process is a unique feature of the alpine permafrost ecosystem, which controls the growth of microorganisms and alpine meadows, and plays a vital role in animal husbandry development, ecosystem functions and services. Meanwhile, the freezing and thawing process is also affected by external environmental factors, and its spatial differences are very significant, especially in the regions over 5000 m a.s.l. In this study, the freezing and thawing process periods of the Cuoma Township (CM), Xiangmao Township (XM) and Xiaotanggula Mountain (XTGL) sites in the Nagqu River Basin are divided, the effects of altitude, vegetation coverage, air temperature, and organic matter content on the freezing and thawing process are analyzed, the main influencing factors are discussed. The results show that in the regions over 5000 m a.s.l, the thaw initiation period (TIP) starts in early April, the entirely thawed period (ETP) starts in end of May, the freeze initiation period (FIP) starts in end of October, and the entirely frozen period (EFP) starts in early November. Compared with the regions below 5000 m a.s.l, FIP and EFP in the regions over 5000 m a.s.l start earlier, the TIP starts later and the freezing rate is faster. Organic matter content is the main influencing factor during FIP and EFP, and air temperature is the main influencing factor during TIP and ETP. This study is helpful to clarify the changes of freezing and thawing process in the regions over 5000 m a.s.l, and also provides theoretical support for ecological protection and restoration.
format Article in Journal/Newspaper
author Man Zihao
Che Shengquan
Jiang Ruiyuan
Xie Changkun
author_facet Man Zihao
Che Shengquan
Jiang Ruiyuan
Xie Changkun
author_sort Man Zihao
title Research on Influencing Factors of Freezing and Thawing Process in the regions over 5000 m a.s.l
title_short Research on Influencing Factors of Freezing and Thawing Process in the regions over 5000 m a.s.l
title_full Research on Influencing Factors of Freezing and Thawing Process in the regions over 5000 m a.s.l
title_fullStr Research on Influencing Factors of Freezing and Thawing Process in the regions over 5000 m a.s.l
title_full_unstemmed Research on Influencing Factors of Freezing and Thawing Process in the regions over 5000 m a.s.l
title_sort research on influencing factors of freezing and thawing process in the regions over 5000 m a.s.l
publisher EDP Sciences
publishDate 2023
url https://doi.org/10.1051/e3sconf/202339301011
https://doaj.org/article/bf8e61018d1e48098dbb46db59877a1f
genre permafrost
genre_facet permafrost
op_source E3S Web of Conferences, Vol 393, p 01011 (2023)
op_relation https://www.e3s-conferences.org/articles/e3sconf/pdf/2023/30/e3sconf_eppct2023_01011.pdf
https://doaj.org/toc/2267-1242
2267-1242
doi:10.1051/e3sconf/202339301011
https://doaj.org/article/bf8e61018d1e48098dbb46db59877a1f
op_doi https://doi.org/10.1051/e3sconf/202339301011
container_title E3S Web of Conferences
container_volume 393
container_start_page 01011
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