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DOI | 10.5194/essd-12-2705-2020 |
A long-term (2005-2019) eddy covariance data set of CO2 and H2O fluxes from the Tibetan alpine steppe | |
Nieberding, Felix; Wille, Christian; Fratini, Gerardo; Asmussen, Magnus O.; Wang, Yuyang; Ma, Yaoming; Sachs, Torsten | |
通讯作者 | Nieberding, F (通讯作者) |
发表日期 | 2020 |
ISSN | 1866-3508 |
EISSN | 1866-3516 |
起始页码 | 2505 |
结束页码 | 2524 |
卷号 | 12期号:4 |
英文摘要 | The Tibetan alpine steppe ecosystem covers an area of roughly 800 000 km(2) and contains up to 3.3% soil organic carbon in the uppermost 30 cm, summing up to 1.93 Pg C for the Tibet Autonomous Region only (472 037 km(2)). With temperatures rising 2 to 3 times faster than the global average, these carbon stocks are at risk of loss due to enhanced soil respiration. The remote location and the harsh environmental conditions on the Tibetan Plateau (TP) make it challenging to derive accurate data on the ecosystem-atmosphere exchange of carbon dioxide (CO2) and water vapor (H2O). Here, we provide the first multiyear data set of CO2 and H2O fluxes from the central Tibetan alpine steppe ecosystem, measured in situ using the eddy covariance technique. The calculated fluxes were rigorously quality checked and carefully corrected for a drift in concentration measurements. The gas analyzer self-heating effect during cold conditions was evaluated using the standard correction procedure and newly revised formulations (Burba et al., 2008; Frank and Massman, 2020). A wind field analysis was conducted to identify influences of adjacent buildings on the turbulence regime and to exclude the disturbed fluxes from subsequent computations. The presented CO2 fluxes were additionally gap filled using a standardized approach. The very low net carbon uptake across the 15-year data set highlights the special vulnerability of the Tibetan alpine steppe ecosystem to become a source of CO2 due to global warming. The data are freely available at https://doi.org/10.5281/zenodo.3733202 (Nieberding et al., 2020a) and https://doi.org/10.11888/Meteoro.tpdc.270333 (Nieberding et al., 2020b) and may help us to better understand the role of the Tibetan alpine steppe in the global carbon-climate feedback. |
关键词 | NET ECOSYSTEM EXCHANGECARBON-DIOXIDEMEADOWWATERTEMPERATUREQUALITYENERGYPATHUNCERTAINTYCONSEQUENCES |
语种 | 英语 |
WOS研究方向 | Geology ; Meteorology & Atmospheric Sciences |
WOS类目 | Geosciences, Multidisciplinary ; Meteorology & Atmospheric Sciences |
WOS记录号 | WOS:000592253900001 |
来源期刊 | EARTH SYSTEM SCIENCE DATA |
来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/260013 |
推荐引用方式 GB/T 7714 | Nieberding, Felix,Wille, Christian,Fratini, Gerardo,et al. A long-term (2005-2019) eddy covariance data set of CO2 and H2O fluxes from the Tibetan alpine steppe[J]. 中国科学院青藏高原研究所,2020,12(4). |
APA | Nieberding, Felix.,Wille, Christian.,Fratini, Gerardo.,Asmussen, Magnus O..,Wang, Yuyang.,...&Sachs, Torsten.(2020).A long-term (2005-2019) eddy covariance data set of CO2 and H2O fluxes from the Tibetan alpine steppe.EARTH SYSTEM SCIENCE DATA,12(4). |
MLA | Nieberding, Felix,et al."A long-term (2005-2019) eddy covariance data set of CO2 and H2O fluxes from the Tibetan alpine steppe".EARTH SYSTEM SCIENCE DATA 12.4(2020). |
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