Hochschulschrift
Hydraulic and thermal dynamics at various permafrost sites on the Qinghai-Tibet Plateau
- Location
-
Deutsche Nationalbibliothek Frankfurt am Main
- Dimensions
-
30 cm
- Extent
-
XIII, 147 S.
- Language
-
Englisch
- Notes
-
Ill., graph. Darst.
Heidelberg, Univ., Diss., 2011 (Nicht für den Austausch)
- Keyword
-
Dauerfrostboden ; Hochland von Tibet ; Elektromagnetische Reflexionsmethode ; Parametrisierung
Dauerfrostboden
Qinghai
- Creator
- Table of contents
- Rights
-
Bei diesem Objekt liegt nur das Inhaltsverzeichnis digital vor. Der Zugriff darauf ist unbeschränkt möglich.
- Last update
-
11.06.2025, 1:58 PM 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.
Object type
- Hochschulschrift
Associated
Other Objects (12)
Hydraulic and thermal dynamics at various permafrost sites on the Qinghai-Tibet Plateau
Root uptake dominates mercury accumulation in permafrost plants of 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
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
Geological line selection for the Qinghai-Tibet railway engineering
Permafrost, active layer, and meteorological data (2010–2020) at the Mahan Mountain relict permafrost site of northeastern Qinghai–Tibet Plateau
Summer heat wave in 2022 led to rapid warming of permafrost in the central Qinghai-Tibet Plateau
Ecological restoration is crucial in mitigating carbon loss caused by permafrost thawing on the Qinghai-Tibet Plateau
100 years of lake evolution over the Qinghai–Tibet Plateau
Surface oxygen concentration on the Qinghai-Tibet Plateau (2017–2022)
Hydraulic and thermal dynamics at various permafrost sites on the Qinghai-Tibet Plateau
Root uptake dominates mercury accumulation in permafrost plants of 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
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
Geological line selection for the Qinghai-Tibet railway engineering
Permafrost, active layer, and meteorological data (2010–2020) at the Mahan Mountain relict permafrost site of northeastern Qinghai–Tibet Plateau
Summer heat wave in 2022 led to rapid warming of permafrost in the central Qinghai-Tibet Plateau
Ecological restoration is crucial in mitigating carbon loss caused by permafrost thawing on the Qinghai-Tibet Plateau
100 years of lake evolution over the Qinghai–Tibet Plateau
Surface oxygen concentration on the Qinghai-Tibet Plateau (2017–2022)
Hydraulic and thermal dynamics at various permafrost sites on the Qinghai-Tibet Plateau
Root uptake dominates mercury accumulation in permafrost plants of 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
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
Geological line selection for the Qinghai-Tibet railway engineering
Permafrost, active layer, and meteorological data (2010–2020) at the Mahan Mountain relict permafrost site of northeastern Qinghai–Tibet Plateau
Summer heat wave in 2022 led to rapid warming of permafrost in the central Qinghai-Tibet Plateau
Ecological restoration is crucial in mitigating carbon loss caused by permafrost thawing on the Qinghai-Tibet Plateau
100 years of lake evolution over the Qinghai–Tibet Plateau