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

Abstract 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, CO 2 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.