Substantial non‐growing season carbon dioxide loss across Tibetan alpine permafrost region

• Published in: Global Change Biology
• Main Authors: Li, Qinlu, Liu, Yang, Kou, Dan, Peng, Yunfeng, Yang, Yuanhe
• Other Authors: Chinese Academy of Sciences, National Natural Science Foundation of China, Youth Innovation Promotion Association of the Chinese Academy of Sciences
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2022
• Subjects: Arctic; permafrost
• Online Access: http://dx.doi.org/10.1111/gcb.16315; https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.16315; https://onlinelibrary.wiley.com/doi/full-xml/10.1111/gcb.16315

Abstract One of the major uncertainties for projecting permafrost carbon (C)‐climate feedback is a poor representation of the non‐growing season carbon dioxide (CO 2 ) emissions under a changing climate. Here, combining in situ field observations, regional synthesis and a random forest model, we assessed contemporary and future soil respired CO 2 (i.e., soil respiration, R s ) across the Tibetan alpine permafrost region, which has received much less attention compared with the Arctic permafrost domain. We estimated the regional mean R s of 229.8, 72.9 and 302.7 g C m −2 year −1 during growing season, non‐growing season and the entire year, respectively; corresponding to the contemporary losses of 296.9, 94.3 and 391.2 Tg C year −1 from this high‐altitude permafrost‐affected area. The non‐growing season R s accounted for a quarter of the annual soil CO 2 efflux. Different from the prevailing view that temperature is the most limiting factor for cold‐period CO 2 release in Arctic permafrost ecosystems, precipitation determined the spatial pattern of non‐growing season R s on the Tibetan Plateau. Using the key predictors, model extrapolation demonstrated additional losses of 38.8 and 74.5 Tg C from the non‐growing season for a moderate mitigation scenario and a business‐as‐usual emissions scenario, respectively. These results provide a baseline for non‐growing season CO 2 emissions from high‐altitude permafrost areas and help for accurate projection of permafrost C‐climate feedback.