The impacts of soil freeze/thaw dynamics on soil water transfer and spring phenology in the Tibetan Plateau

Climate warming has induced significant changes in permafrost and seasonally frozen ground (SFG) in the Tibetan Plateau, which have complex influences on local environments. A better understanding of the impacts of soil freeze/thaw (F/T) dynamics on soil water transfer and vegetation growth is impor...

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Published in:Arctic, Antarctic, and Alpine Research
Main Authors: Huiru Jiang, Wenjiang Zhang, Yonghong Yi, Kun Yang, Guicai Li, Gengxu Wang
Format: Article in Journal/Newspaper
Language:English
Published: Taylor & Francis Group 2018
Subjects:
Online Access:https://doi.org/10.1080/15230430.2018.1439155
https://doaj.org/article/72e91fb214704310a4bd6d13f54ebdfa
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spelling ftdoajarticles:oai:doaj.org/article:72e91fb214704310a4bd6d13f54ebdfa 2023-05-15T14:14:29+02:00 The impacts of soil freeze/thaw dynamics on soil water transfer and spring phenology in the Tibetan Plateau Huiru Jiang Wenjiang Zhang Yonghong Yi Kun Yang Guicai Li Gengxu Wang 2018-01-01T00:00:00Z https://doi.org/10.1080/15230430.2018.1439155 https://doaj.org/article/72e91fb214704310a4bd6d13f54ebdfa EN eng Taylor & Francis Group http://dx.doi.org/10.1080/15230430.2018.1439155 https://doaj.org/toc/1523-0430 https://doaj.org/toc/1938-4246 1523-0430 1938-4246 doi:10.1080/15230430.2018.1439155 https://doaj.org/article/72e91fb214704310a4bd6d13f54ebdfa Arctic, Antarctic, and Alpine Research, Vol 50, Iss 1 (2018) freeze/thaw permafrost soil moisture tibetan plateau vegetation spring onset Environmental sciences GE1-350 Ecology QH540-549.5 article 2018 ftdoajarticles https://doi.org/10.1080/15230430.2018.1439155 2022-12-31T09:47:16Z Climate warming has induced significant changes in permafrost and seasonally frozen ground (SFG) in the Tibetan Plateau, which have complex influences on local environments. A better understanding of the impacts of soil freeze/thaw (F/T) dynamics on soil water transfer and vegetation growth is important to explore related eco-hydrological influences. We investigated soil F/T dynamics and their impacts with in-situ and satellite-based observations. Our results showed the contrasting F/T dynamics between SFG and permafrost areas. In permafrost areas, soil froze downward from the ground surface and upward from the active layer bottom with a distinct freezing zero-curtain, and minimum soil moisture occurred in the intermediate layer, but the thawing process was unidirectional. However, the vertical F/T directions were contrary in SFG areas, where soil moisture generally increased with depth and the thawing zero-curtain was distinct. The spring onset showed a positive correlation with thaw onset in permafrost areas, but such a correlation was variable in SFG areas likely depending on soil-moisture level. Our results implied that the different soil-moisture patterns and the varying vegetation response might be related to the spatially contrasting F/T dynamics, which may have different impacts on soil water transfer, and further affect the zero-curtain and vegetation phenology. Article in Journal/Newspaper Antarctic and Alpine Research Arctic permafrost Directory of Open Access Journals: DOAJ Articles Arctic, Antarctic, and Alpine Research 50 1 e1439155
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic freeze/thaw
permafrost
soil moisture
tibetan plateau
vegetation spring onset
Environmental sciences
GE1-350
Ecology
QH540-549.5
spellingShingle freeze/thaw
permafrost
soil moisture
tibetan plateau
vegetation spring onset
Environmental sciences
GE1-350
Ecology
QH540-549.5
Huiru Jiang
Wenjiang Zhang
Yonghong Yi
Kun Yang
Guicai Li
Gengxu Wang
The impacts of soil freeze/thaw dynamics on soil water transfer and spring phenology in the Tibetan Plateau
topic_facet freeze/thaw
permafrost
soil moisture
tibetan plateau
vegetation spring onset
Environmental sciences
GE1-350
Ecology
QH540-549.5
description Climate warming has induced significant changes in permafrost and seasonally frozen ground (SFG) in the Tibetan Plateau, which have complex influences on local environments. A better understanding of the impacts of soil freeze/thaw (F/T) dynamics on soil water transfer and vegetation growth is important to explore related eco-hydrological influences. We investigated soil F/T dynamics and their impacts with in-situ and satellite-based observations. Our results showed the contrasting F/T dynamics between SFG and permafrost areas. In permafrost areas, soil froze downward from the ground surface and upward from the active layer bottom with a distinct freezing zero-curtain, and minimum soil moisture occurred in the intermediate layer, but the thawing process was unidirectional. However, the vertical F/T directions were contrary in SFG areas, where soil moisture generally increased with depth and the thawing zero-curtain was distinct. The spring onset showed a positive correlation with thaw onset in permafrost areas, but such a correlation was variable in SFG areas likely depending on soil-moisture level. Our results implied that the different soil-moisture patterns and the varying vegetation response might be related to the spatially contrasting F/T dynamics, which may have different impacts on soil water transfer, and further affect the zero-curtain and vegetation phenology.
format Article in Journal/Newspaper
author Huiru Jiang
Wenjiang Zhang
Yonghong Yi
Kun Yang
Guicai Li
Gengxu Wang
author_facet Huiru Jiang
Wenjiang Zhang
Yonghong Yi
Kun Yang
Guicai Li
Gengxu Wang
author_sort Huiru Jiang
title The impacts of soil freeze/thaw dynamics on soil water transfer and spring phenology in the Tibetan Plateau
title_short The impacts of soil freeze/thaw dynamics on soil water transfer and spring phenology in the Tibetan Plateau
title_full The impacts of soil freeze/thaw dynamics on soil water transfer and spring phenology in the Tibetan Plateau
title_fullStr The impacts of soil freeze/thaw dynamics on soil water transfer and spring phenology in the Tibetan Plateau
title_full_unstemmed The impacts of soil freeze/thaw dynamics on soil water transfer and spring phenology in the Tibetan Plateau
title_sort impacts of soil freeze/thaw dynamics on soil water transfer and spring phenology in the tibetan plateau
publisher Taylor & Francis Group
publishDate 2018
url https://doi.org/10.1080/15230430.2018.1439155
https://doaj.org/article/72e91fb214704310a4bd6d13f54ebdfa
genre Antarctic and Alpine Research
Arctic
permafrost
genre_facet Antarctic and Alpine Research
Arctic
permafrost
op_source Arctic, Antarctic, and Alpine Research, Vol 50, Iss 1 (2018)
op_relation http://dx.doi.org/10.1080/15230430.2018.1439155
https://doaj.org/toc/1523-0430
https://doaj.org/toc/1938-4246
1523-0430
1938-4246
doi:10.1080/15230430.2018.1439155
https://doaj.org/article/72e91fb214704310a4bd6d13f54ebdfa
op_doi https://doi.org/10.1080/15230430.2018.1439155
container_title Arctic, Antarctic, and Alpine Research
container_volume 50
container_issue 1
container_start_page e1439155
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