Climate warming over the past half century has led to thermal degradation of permafrost on 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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Climate warming over the past half century has led to thermal degradation of permafrost on the Qinghai–Tibet Plateau ; volume:12 ; number:2 ; year:2018 ; pages:595-608
The Cryosphere ; 12, Heft 2 (2018), 595-608
- Creator
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Ran, Youhua
Li, Xin
Cheng, Guodong
- DOI
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10.5194/tc-12-595-2018
- URN
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urn:nbn:de:101:1-2018061216073189762330
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
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15.08.2025, 7:31 AM CEST
Data provider
This object is provided by:
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Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Associated
- Ran, Youhua
- Li, Xin
- Cheng, Guodong
Other Objects (12)
Summer heat wave in 2022 led to rapid warming of permafrost in the central Qinghai-Tibet Plateau
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Effects of stratified active layers on high-altitude permafrost warming: a case study on the Qinghai–Tibet Plateau
Response of freeze-thaw processes to experimental warming in the permafrost regions of the central Qinghai-Tibet Plateau
Hydraulic and thermal dynamics at various permafrost sites on the Qinghai-Tibet Plateau
Hydraulic and thermal dynamics at various permafrost sites on the Qinghai-Tibet Plateau
Simulating the current and future northern limit of permafrost on the Qinghai–Tibet Plateau
A synthesis dataset of permafrost thermal state for the Qinghai–Tibet (Xizang) Plateau, China
Projected changes of Active layer thickness over permafrost under 1.5~5.0 °C climate warming on the Qinghai-Tibet Plateau
Climate warming has led to the degradation of permafrost stability in the past half century over the Qinghai-Tibet Plateau
Permafrost temperature baseline at 15 meters depth in the Qinghai-Tibet Plateau (2010–2019)
Distress Characteristics in Embankment-Bridge Transition Section of the Qinghai-Tibet Railway in Permafrost Regions
Summer heat wave in 2022 led to rapid warming of permafrost in the central Qinghai-Tibet Plateau
Root uptake dominates mercury accumulation in permafrost plants of Qinghai-Tibet Plateau
Effects of stratified active layers on high-altitude permafrost warming: a case study on the Qinghai–Tibet Plateau
Response of freeze-thaw processes to experimental warming in the permafrost regions of the central Qinghai-Tibet Plateau
Hydraulic and thermal dynamics at various permafrost sites on the Qinghai-Tibet Plateau
Hydraulic and thermal dynamics at various permafrost sites on the Qinghai-Tibet Plateau
Simulating the current and future northern limit of permafrost on the Qinghai–Tibet Plateau
A synthesis dataset of permafrost thermal state for the Qinghai–Tibet (Xizang) Plateau, China
Projected changes of Active layer thickness over permafrost under 1.5~5.0 °C climate warming on the Qinghai-Tibet Plateau
Climate warming has led to the degradation of permafrost stability in the past half century over the Qinghai-Tibet Plateau
Permafrost temperature baseline at 15 meters depth in the Qinghai-Tibet Plateau (2010–2019)
Distress Characteristics in Embankment-Bridge Transition Section of the Qinghai-Tibet Railway in Permafrost Regions
Summer heat wave in 2022 led to rapid warming of permafrost in the central Qinghai-Tibet Plateau
Root uptake dominates mercury accumulation in permafrost plants of Qinghai-Tibet Plateau
Effects of stratified active layers on high-altitude permafrost warming: a case study on the Qinghai–Tibet Plateau
Response of freeze-thaw processes to experimental warming in the permafrost regions of the central Qinghai-Tibet Plateau
Hydraulic and thermal dynamics at various permafrost sites on the Qinghai-Tibet Plateau
Hydraulic and thermal dynamics at various permafrost sites on the Qinghai-Tibet Plateau
Simulating the current and future northern limit of permafrost on the Qinghai–Tibet Plateau
A synthesis dataset of permafrost thermal state for the Qinghai–Tibet (Xizang) Plateau, China
Projected changes of Active layer thickness over permafrost under 1.5~5.0 °C climate warming on the Qinghai-Tibet Plateau
Climate warming has led to the degradation of permafrost stability in the past half century over the Qinghai-Tibet Plateau
Permafrost temperature baseline at 15 meters depth in the Qinghai-Tibet Plateau (2010–2019)