The impacts of soil enthalpy change on land–atmosphere interactions of permafrost on the Qinghai-Tibet Plateau

The hydrothermal changes in the active layers of permafrost soils during freeze–thaw processes are crucial for understanding the interactions between the surface and the atmosphere. The soil enthalpy of the active layer in permafrost regions is a comprehensive parameter incorporating soil temperatur...

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Váldodahkkit:	Ren Li, Shenning Wang, Junjie Ma, Wenhao Liu, Tonghua Wu, Changwei Xie, Xiaodong Wu, Yongjian Ding, Lin Zhao, Guojie Hu, Jimin Yao, Xiaofan Zhu, Wu Wang, Yongliang Jiao, Yao Xiao, Jianzong Shi, Yongping Qiao
Materiálatiipa:	Artigo
Giella:	Inglês
Almmustuhtton:	Elsevier 2025-02-01
Ráidu:	Geoderma
Fáttát:	Qinghai-Tibet Plateau Active layer Soil enthalpy Freeze–thaw process Hydrothermal change
Liŋkkat:	http://www.sciencedirect.com/science/article/pii/S0016706125000217
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