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Belowground soil analysis from the Tibetan Plateau
This dataset has no description
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High-space-coverage lake level change data sets on the Tibetan Plateau from 2...
The Qinghai Tibet region, known as the Roof of the World and the Water Tower of Asia, has the largest number of lakes in the world, and because of its high altitude and the near... -
High-space-coverage lake level change data sets on the Tibetan Plateau from 2...
The Qinghai Tibet region, known as the Roof of the World and the Water Tower of Asia, has the largest number of lakes in the world, and because of its high altitude and the near... -
Methane fluxes in the foreland soil of Longxiazailongba Glacier on the Tibeta...
Glacier foreland soil was always considered as methane sink. However, there is still a lack of methane dynamics in the foreland soil of mountain glaciers , which are flooded by... -
Concentrations of alkenones in Hala Hu sediment core H7
Concentrations of alkenones were analysed in core H7 from Hala Hu, China by means of an Agilent 7890A gas chromatography (GC) instrument, equipped with a mass selective detector... -
Concentrations of alkenones in Hala Hu sediment core H11
Concentrations of alkenones were analysed in core H11 from Hala Hu, China by means of an Agilent 7890A gas chromatography (GC) instrument, equipped with a mass selective... -
Concentrations of monoanhydrous sugars (firemarkers) in Hala Hu sediment core...
Concentrations of monoanhydrous sugars (firemarkers) were analysed in core H11 from Hala Hu, China. The lake is located on the northern margin of the Tibetan Plateau (97.24 -... -
Concentrations of biomarkers (aliphatic fraction) in Hala Hu sediment core H11
Concentrations of aquatic (mid-chain n-alkenes, C20-HBIs) and terrestrial (long-chain n-alkanes) biomarker groups were analysed in core H11 from Hala Hu, China. The compounds... -
Concentrations of biomarkers (aliphatic fraction) in Hala Hu sediment core H7
Concentrations of aquatic (mid-chain n-alkenes, C20-HBIs) and terrestrial (long-chain n-alkanes) biomarker groups were analysed in core H7 from Hala Hu, China. The compounds... -
δD values of biomarkers in Hala Hu sediment core H11
Hydrogen isotope composition of aquatic (mid-chain n-alkenes, C20-HBIs, C37-alkenones) and terrestrial (long-chain n-alkanes) biomarker groups were analysed in core H11 from... -
A data compilation for soil conditions from the Tibetan Plateau
This dataset has no description
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Enzyme activity from the Tibetan Plateau
This dataset has no description
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Water vapor δD retrieved by the IASI remote-sensing instrument, Southeastern ...
This dataset has no description
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Daily precipitation δD simulated by the LMDZ general circulation model, South...
This dataset has no description
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Ice-Nucleating Particle Concentrations and Sources in Rainwater over the Thir...
The ice-nucleating particles (INPs) modulate the microphysics and radiative properties of clouds. However, less is known concerning their abundance and sources in the most... -
Daily precipitation δD records at 4 sites in Mount Yulong and Mount Meili reg...
Daily precipitation samples were collected at 4 sites in Mount Yulong and Mount Meili regions of Southeastern Tibetan Plateau and analyzed for isotopic composition. We share... -
Palynological data from cores SG-1 and SG-1b from the Qaidam Basin (Tibetan P...
To reconstruct the timing and underlying forcing of major shifts in the composition of terrestrial ecosystems in arid Central Asia during the late Cenozoic (past ~7 Ma), we... -
Rockglacier inventory of the Western Nyainqêntanglha Range, Tibetan Plateau
The western Nyainqêntanglha Range on the Tibetan Plateau reaches an elevation of 7162 m and is characterized by an extensive periglacial environment. Here, we present the first... -
Source apportionment analysis from the Tibetan Plateau
This data gives the contributions of different sources (Marine and salt-lake, dust, biomass burning and long-range transport anthropogenic pollutants) to chemical components... -
Residence time of different land covers in Tibetan Plateau
This data shows the calculated percentage of residence time when air masses passed over different land covers (vegetation,agriculture,bare area, water/ice and urban area),...
