Articles | Volume 12, issue 9
https://doi.org/10.5194/tc-12-2803-2018
https://doi.org/10.5194/tc-12-2803-2018
Research article
 | 
03 Sep 2018
Research article |  | 03 Sep 2018

Consumption of atmospheric methane by the Qinghai–Tibet Plateau alpine steppe ecosystem

Hanbo Yun, Qingbai Wu, Qianlai Zhuang, Anping Chen, Tong Yu, Zhou Lyu, Yuzhong Yang, Huijun Jin, Guojun Liu, Yang Qu, and Licheng Liu

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Latest update: 27 Mar 2024
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Short summary
Here we reported the QTP permafrost region was a CH4 sink of −0.86 ± 0.23 g CH4-C m−2 yr−1 over 2012–2016, soil temperature and soil water content were dominant factors controlling CH4 fluxes, and their correlations changed with soil depth due to cryoturbation dynamics. This region was a net CH4 sink in autumn, but a net source in spring, despite both seasons experiencing similar top soil thawing and freezing dynamics.