Spatiotemporal patterns of methane fluxes across alpine permafrost region on the Tibetan Plateau

Methane (CH<sub>4</sub>) emissions from thawing permafrost could amplify climate warming. However, long-term trajectory of net CH<sub>4</sub> balance in permafrost regions, particularly high-altitude permafrost regions, remains unknown. Based on literature synthesis and CLM5.0 model, we evaluate the contemporary and future CH<sub>4</sub> fluxes across the Tibetan alpine permafrost region from 1989-2100. Here, we find that this permafrost region functions as a marginal CH<sub>4</sub> sink during 1989-2018 (-0.01 ± 0.01 Tg CH<sub>4</sub> yr⁻¹), and future trajectories diverge, with warming and wetting under low- and medium-emission scenarios (SSP1-2.6/SSP2-4.5) driving persistent CH<sub>4</sub> emissions (0.07 Tg CH<sub>4</sub> yr⁻¹). By contrast, under higher emission scenarios (SSP3-7.0/SSP5-8.5), the region shifts to net emissions by mid-century but enhanced atmospheric CH<sub>4</sub> concentrations strengthen sink, returning it to a net sink by century's end (-0.06 ~ -0.02 Tg CH<sub>4</sub> yr⁻¹). These results demonstrate that climate change and atmospheric CH<sub>4</sub> dynamics jointly mediate the trajectory of alpine permafrost CH<sub>4</sub> balance.

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Publication Details

Journal
Nature Communications
Published
2025-08-12
DOI
https://doi.org/10.1038/s41467-025-62699-6
Citations
2
Primary Topic
Climate change and permafrost
Type
article
Field-Weighted Citation Impact
2.60

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article

Spatiotemporal patterns of methane fluxes across alpine permafrost region on the Tibetan Plateau

Shiting Yao, Dan Kou, Yuanhe Yang, Shuqi Qin et al.
2 citations
Nature Communications
Climate change and permafrost
2.60
article

Spatiotemporal patterns of methane fluxes across alpine permafrost region on the Tibetan Plateau

Shiting Yao, Dan Kou, Yuanhe Yang, Shuqi Qin, Josep Peñuelas, Jinfeng Chang, Yi Xi, Xiaofeng Xu, Philippe Ciais, Laiming Huang, Guibiao Yang, Yutong Song
article en
2 citations

Abstract

Methane (CH<sub>4</sub>) emissions from thawing permafrost could amplify climate warming. However, long-term trajectory of net CH<sub>4</sub> balance in permafrost regions, particularly high-altitude permafrost regions, remains unknown. Based on literature synthesis and CLM5.0 model, we evaluate the contemporary and future CH<sub>4</sub> fluxes across the Tibetan alpine permafrost region from 1989-2100. Here, we find that this permafrost region functions as a marginal CH<sub>4</sub> sink during 1989-2018 (-0.01 ± 0.01 Tg CH<sub>4</sub> yr⁻¹), and future trajectories diverge, with warming and wetting under low- and medium-emission scenarios (SSP1-2.6/SSP2-4.5) driving persistent CH<sub>4</sub> emissions (0.07 Tg CH<sub>4</sub> yr⁻¹). By contrast, under higher emission scenarios (SSP3-7.0/SSP5-8.5), the region shifts to net emissions by mid-century but enhanced atmospheric CH<sub>4</sub> concentrations strengthen sink, returning it to a net sink by century's end (-0.06 ~ -0.02 Tg CH<sub>4</sub> yr⁻¹). These results demonstrate that climate change and atmospheric CH<sub>4</sub> dynamics jointly mediate the trajectory of alpine permafrost CH<sub>4</sub> balance.

Nature CommunicationsVol. 16(1)
Qinghai University (CN), Centre National de la Recherche Scientifique (FR), University of Eastern Finland (FI), Université de Versailles Saint-Quentin-en-Yvelines (FR), San Diego State University (US), Commissariat à l'Énergie Atomique et aux Énergies Alternatives (FR), Université Paris-Saclay (FR), Beijing Botanical Garden (CN), Laboratoire des Sciences du Climat et de l'Environnement (FR), CEA Paris-Saclay (FR), Centre for Research on Ecology and Forestry Applications (ES), Institute of Botany (CN), University of Chinese Academy of Sciences (CN), Global Ecology Unit CREAF-CSIC-UAB, China National Botanical Garden, Zhejiang University (CN)
National Natural Science Foundation of China
Climate action
Openalex Percentile: Top 10%
Climate change and permafrost
2.60
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