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Carbon dioxide exchange between the atmosphere and an alpine meadow ecosystem on the Qinghai–Tibetan Plateau, China
We used the eddy covariance method to measure the M exchange between the atmosphere and an alpine meadow ecosystem (37degrees29-45'N, 101degrees12-23'E, 3250m a.s.l.) on the Qinghai-Tibetan Plateau,Expand
Energy exchange between the atmosphere and a meadow ecosystem on the Qinghai-Tibetan Plateau
To reveal the potential contribution of grassland ecosystems to climate change, we examined the energy exchange over an alpine Kobresia meadow on the northeastern Qinghai-Tibetan Plateau. The annualExpand
Effect of long-term grazing on soil organic carbon content in semiarid steppes in Inner Mongolia
To clarify the response of soil organic carbon (SOC) content to season-long grazing in the semiarid typical steppes of Inner Mongolia, we examined the aboveground biomass and SOC in both grazingExpand
Partitioning pattern of carbon flux in a Kobresia grassland on the Qinghai‐Tibetan Plateau revealed by field 13C pulse‐labeling
Characterizing the carbon turnover in terrestrial ecosystems is critical for understanding and predicting carbon dynamics in ecosystems. We used in situ 13C pulse labeling to track photosyntheticExpand
Seasonal and interannual variation in water vapor and energy exchange over a typical steppe in Inner Mongolia, China
In this study, we conducted eddy covariance (EC) measurements of water vapor exchange over a typical steppe in a semi-arid area of the Inner Mongolia Plateau, China. Measurement sites were locatedExpand
Characterizing evapotranspiration over a meadow ecosystem on the Qinghai-Tibetan Plateau
To characterize evapotranspiration (ET) over grasslands on the Qinghai-Tibetan Plateau, we examined ET and its relevant environmental variables in a Kobresia meadow from 2002 to 2004 using the eddyExpand
Short‐term variation of CO2 flux in relation to environmental controls in an alpine meadow on the Qinghai‐Tibetan Plateau
[1] The alpine meadow ecosystem on the Qinghai-Tibetan Plateau may play a significant role in the regional carbon cycle. To assess the CO2 flux and its relationship to environmental controls in theExpand
Radiation partitioning and its relation to environmental factors above a meadow ecosystem on the Qinghai‐Tibetan Plateau
Understanding the energy balance on the Qinghai-Tibetan Plateau is essential for better prediction of global climate change. To characterize the energy balance on the plateau, we examined theExpand
Effects of warming and grazing on soil N availability, species composition, and ANPP in an alpine meadow.
TLDR
It is suggested that soil N availability does not determine ANPP under simulated warming and that heavy grazing rather than warming causes degradation of the alpine meadows. Expand
Aerobic methanotroph diversity in Riganqiao peatlands on the Qinghai-Tibetan Plateau.
TLDR
The results indicate that aerobic methanotrophs are abundant in Riganqiao peatland and include previously undetected clades in this geographically isolated and distinctive environment. Expand
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