Articles | Volume 19, issue 3
https://doi.org/10.5194/bg-19-861-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-19-861-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
10 Feb 2022
Research article |
| 10 Feb 2022
| 10 Feb 2022
Radiation, soil water content, and temperature effects on carbon cycling in an alpine swamp meadow of the northeastern Qinghai–Tibetan Plateau
Junqi Wei
State Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University, Beijing 100875, China
School of Natural Resources, Faculty of Geographical Science, Beijing Normal University, Beijing 100875, China
State Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University, Beijing 100875, China
School of Natural Resources, Faculty of Geographical Science, Beijing Normal University, Beijing 100875, China
Academy of Plateau Science and Sustainability, People's Government of Qinghai Province and Beijing Normal University, Qinghai Normal University, Xining 810008, China
Key Laboratory of Tibetan Plateau Land Surface Processes and Ecological Conservation, Ministry of Education, Qinghai Normal University, Xining 810016, China
Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China
College of Resources and Environment, University of Chinese Academy of Sciences, Yuquanlu, Beijing 100049, China
Torben Røjle Christensen
Department of Ecoscience, Arctic Research Center, Aarhus University, Roskilde 4000, Denmark
Oulanka Research Station, University of Oulu, Oulu, Finland
Zhiyun Jiang
School of Geography, South China Normal University, Guangzhou 510631, China
Yujun Ma
School of Geography and Planning, Sun Yat-sen University, Guangzhou 510275, China
Xiuchen Wu
State Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University, Beijing 100875, China
School of Natural Resources, Faculty of Geographical Science, Beijing Normal University, Beijing 100875, China
Hongyun Yao
State Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University, Beijing 100875, China
School of Natural Resources, Faculty of Geographical Science, Beijing Normal University, Beijing 100875, China
Efrén López-Blanco
Department of Environment and Minerals, Greenland Institute of Natural Resources, Nuuk 3900, Greenland
Department of Ecoscience, Arctic Research Center, Aarhus University, Roskilde 4000, Denmark
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Cited
8 citations as recorded by crossref.
- Effects of rainfall amount and frequency on carbon exchange in a wet meadow ecosystem on the Qinghai-Tibet Plateau J. Wu et al. 10.1016/j.catena.2022.106629
- From climate to crop: Unveiling the impact of agro-climate dataset on rice yield in Cotabato Province R. Delena et al. 10.1016/j.dib.2023.109754
- Ecophysiological Response of Vitis vinifera L. in an Urban Agrosystem: Preliminary Assessment of Genetic Variability E. Brunori et al. 10.3390/plants11223026
- Response of methanogenic community and their activity to temperature rise in alpine swamp meadow at different water level of the permafrost wetland on Qinghai-Tibet Plateau H. Cui et al. 10.3389/fmicb.2023.1181658
- Identifying the Driving Forces of Alpine Wetland Dynamic Changes in the Yellow River Source National Park from 2000 to 2020 T. Ma et al. 10.3390/w15142557
- Growing-season carbon budget of alpine meadow ecosystem in the Qinghai Lake Basin: a continued carbon sink through this century according to the Biome-BGC model M. Zhang et al. 10.1186/s13021-023-00244-y
- Vegetation types and flood water level are dominant factors controlling the carbon sequestration potential in Dongting Lake floodplain, China T. Wang et al. 10.1016/j.scitotenv.2024.171146
- A framework for identifying propagation from meteorological to ecological drought events Y. Wang et al. 10.1016/j.jhydrol.2023.130142
8 citations as recorded by crossref.
- Effects of rainfall amount and frequency on carbon exchange in a wet meadow ecosystem on the Qinghai-Tibet Plateau J. Wu et al. 10.1016/j.catena.2022.106629
- From climate to crop: Unveiling the impact of agro-climate dataset on rice yield in Cotabato Province R. Delena et al. 10.1016/j.dib.2023.109754
- Ecophysiological Response of Vitis vinifera L. in an Urban Agrosystem: Preliminary Assessment of Genetic Variability E. Brunori et al. 10.3390/plants11223026
- Response of methanogenic community and their activity to temperature rise in alpine swamp meadow at different water level of the permafrost wetland on Qinghai-Tibet Plateau H. Cui et al. 10.3389/fmicb.2023.1181658
- Identifying the Driving Forces of Alpine Wetland Dynamic Changes in the Yellow River Source National Park from 2000 to 2020 T. Ma et al. 10.3390/w15142557
- Growing-season carbon budget of alpine meadow ecosystem in the Qinghai Lake Basin: a continued carbon sink through this century according to the Biome-BGC model M. Zhang et al. 10.1186/s13021-023-00244-y
- Vegetation types and flood water level are dominant factors controlling the carbon sequestration potential in Dongting Lake floodplain, China T. Wang et al. 10.1016/j.scitotenv.2024.171146
- A framework for identifying propagation from meteorological to ecological drought events Y. Wang et al. 10.1016/j.jhydrol.2023.130142
Latest update: 17 Apr 2024
Short summary
Although water availability has been linked to the response of ecosystem carbon (C) sink–source to climate warming, the mechanisms by which C uptake responds to soil moisture remain unclear. We explored how soil water and other environmental drivers modulate net C uptake in an alpine swamp meadow. Results reveal that nearly saturated soil conditions during warm seasons can help to maintain lower ecosystem respiration and therefore enhance the C sequestration capacity in this alpine swamp meadow.
Although water availability has been linked to the response of ecosystem carbon (C) sink–source...
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