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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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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1766286919910555648 |