Soil respiration of alpine meadow is controlled by freeze–thaw processes of active layer in the permafrost region of the Qinghai–Tibet Plateau
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Extent
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Online-Ressource
- Language
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Englisch
- Bibliographic citation
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Soil respiration of alpine meadow is controlled by freeze–thaw processes of active layer in the permafrost region of the Qinghai–Tibet Plateau ; volume:14 ; number:9 ; year:2020 ; pages:2835-2848
The Cryosphere ; 14, Heft 9 (2020), 2835-2848
- Creator
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Wang, Junfeng
Wu, Qingbai
Yuan, Ziqiang
Kang, Hojeong
- DOI
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10.5194/tc-14-2835-2020
- URN
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urn:nbn:de:101:1-2020091005324728964490
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
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14.08.2025, 10:49 AM CEST
Data provider
This object is provided by:
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Associated
- Wang, Junfeng
- Wu, Qingbai
- Yuan, Ziqiang
- Kang, Hojeong
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Seasonal freeze‒thaw processes impact microbial communities of soil aggregates associated with soil pores on the Qinghai–Tibet Plateau
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Spatially resolved analysis of the progression of freeze‐thaw damage in concrete
Response of freeze-thaw processes to experimental warming in the permafrost regions of the central Qinghai-Tibet Plateau
Freeze-thaw processes of active layer regulate soil respiration of alpine meadow in the permafrost region of the Qinghai-Tibet Plateau
Seasonal freeze‒thaw processes impact microbial communities of soil aggregates associated with soil pores on the Qinghai–Tibet Plateau
Heterogeneity of Surface Heat Exchange of Slopes and Potential Drivers of the Initiation of Thaw Slump, Qinghai-Tibet Plateau
Research progress of freeze–thaw rock using bibliometric analysis
Retrogressive thaw slumps along the Qinghai-Tibet Engineering Corridor: a comprehensive inventory and their distribution characteristics
Material cycling of wetland soils driven by freeze-thaw effects
Freeze–Thaw Resistance of Ternary Blended Concrete Using Ferronickel Slag
100 years of lake evolution over the Qinghai–Tibet Plateau
100 years of lake evolution over the Qinghai-Tibet Plateau
Freeze–thaw Caenorhabditis elegans freeze–thaw stress response is regulated by the insulin/IGF-1 receptor daf-2
Spatially resolved analysis of the progression of freeze‐thaw damage in concrete
Response of freeze-thaw processes to experimental warming in the permafrost regions of the central Qinghai-Tibet Plateau
Freeze-thaw processes of active layer regulate soil respiration of alpine meadow in the permafrost region of the Qinghai-Tibet Plateau
Seasonal freeze‒thaw processes impact microbial communities of soil aggregates associated with soil pores on the Qinghai–Tibet Plateau
Heterogeneity of Surface Heat Exchange of Slopes and Potential Drivers of the Initiation of Thaw Slump, Qinghai-Tibet Plateau
Research progress of freeze–thaw rock using bibliometric analysis
Retrogressive thaw slumps along the Qinghai-Tibet Engineering Corridor: a comprehensive inventory and their distribution characteristics
Material cycling of wetland soils driven by freeze-thaw effects
Freeze–Thaw Resistance of Ternary Blended Concrete Using Ferronickel Slag
100 years of lake evolution over the Qinghai–Tibet Plateau
100 years of lake evolution over the Qinghai-Tibet Plateau
Freeze–thaw Caenorhabditis elegans freeze–thaw stress response is regulated by the insulin/IGF-1 receptor daf-2