Permafrost Degradation Diminishes Terrestrial Ecosystem Carbon Sequestration Capacity on the Qinghai‐Tibetan Plateau

• Published in: Global biogeochemical cycles 2022-02, Vol.36 (2), p.n/a
• Main Authors: Liu, Lei, Zhuang, Qianlai, Zhao, Dongsheng, Zheng, Du, Kou, Dan, Yang, Yuanhe
• Format: Article
• Language: English
• Subjects: 21st century; Active layer; Carbon; Carbon dioxide; Carbon sequestration; Climate change; C‐N feedbacks; deep soil; Meadows; Net Primary Productivity; Nitrogen; Organic carbon; Organic soils; Permafrost; Permafrost degradation; Primary production; Soil; Soil degradation; Soil layers; Soils; Steppes; Stocks; Tibetan Plateau
• ISSN: 0886-6236; 1944-9224
• DOI: 10.1029/2021GB007068

Effects of permafrost degradation on carbon (C) and nitrogen (N) cycling on the Qinghai‐Tibetan Plateau (QTP) have rarely been analyzed. This study used a revised process‐based biogeochemical model to quantify the effects in the region during the 21st century. We found that permafrost degradation would expose 0.61 ± 0.26 (mean ± SD) and 1.50 ± 0.15 Pg C of soil organic carbon under the representative concentration pathway (RCP) 4.5 and the RCP 8.5, respectively. Among them, more than 20% will be decomposed, enhancing heterotrophic respiration by 8.62 ± 4.51 (RCP 4.5) and 33.66 ± 14.03 (RCP 8.5) Tg C/yr in 2099. Deep soil N supply due to thawed permafrost is not accessible to plants, only stimulating net primary production by 7.15 ± 4.83 (RCP 4.5) and 24.27 ± 9.19 (RCP 8.5) Tg C/yr in 2099. As a result, the single effect of permafrost degradation would cumulatively weaken the regional C sink by 209.44 ± 137.49 (RCP 4.5) and 371.06 ± 151.70 (RCP 8.5) Tg C during 2020–2099. However, when factors of climate change, CO2 increasing and permafrost degradation are all considered, the permafrost region on the QTP would be a stronger C sink in the 21st century. Permafrost degradation has a greater influence on C balance of alpine meadows than alpine steppes on the QTP. The shallower active layer, higher soil C and N stocks, and wetter environment in alpine meadows are responsible for its stronger response to permafrost degradation. This study highlights that permafrost degradation could continue to release large amounts of C to the atmosphere irrespective of potentially more nitrogen available from deep soils. Key Points Soil carbon release due to permafrost degradation overwhelms net primary production on the Qinghai‐Tibetan Plateau Deep soil nitrogen addition from thawing permafrost has a limited benefit to plant carbon uptake Permafrost degradation has more pronounced influences on carbon cycling of alpine meadows than alpine steppes