Data-driven spatiotemporal projections of shallow permafrost based on CMIP6 across the Qinghai‒Tibet Plateau at 1 km^(2) scale  

作　　者：YIN Guo-An NIU Fu-Jun LIN Zhan-Ju LUO Jing LIU Ming-Hao 

机构地区：[1]Liu State Key Laboratory of Frozen Soils Engineering,Northwest Institute of Eco-Environment and Resources,Chinese Academy of Sciences,Lanzhou 730000,China

出　　处：《Advances in Climate Change Research》2021年第6期814-827,共14页气候变化研究进展（英文版）

基　　金：This work was supported by the Strategic Priority Research Program of the Chinese Academy of Sciences(XDA19070504);the National Natural Science Foundation of China(41801037);CAS Light of West China Program.We thank the three anonymous reviewers for their valuable comments and suggestions that helped to improve the manuscript.

摘　　要：The degradation of near-surface permafrost under ongoing climate change on the Qinghai‒Tibet Plateau (QTP) is of growing concern due to its impacts on geomorphological and ecological processes, as well as human activities. There is an increased need for an in-depth understanding of the evolution of permafrost temperature (Ttop) and active-layer thickness (ALT) at a fine scale on the QTP under climate change. This study evaluated the permafrost thermal development over the QTP for the period 1980–2100 at a 1 km^(2) scale using a physically analytical model accounting for both climatic and local environmental factors based on multi-source data. The model results were validated against thermal borehole measurements and baseline maps. The modeled current (2001–2018) permafrost area (Ttop ≤ 0 ℃) covers 1.42 × 10^(6) km^(2) (ca. 56.1% of the QTP land area), 10.1% of which thawed over the historical period 1981–2000. To assess how the ground thermal regime could develop in the future, we utilized the multi-model ensemble mean of downscaled outputs from eight climate models under three Shared Socio-economic Pathways (i.e., SSP126, 245, and 585) in CMIP6 to force the permafrost model. Model results suggest that the current (2001–2018) permafrost extent is likely to dramatically contract in the future period (2021–2100), as indicated by consistent Ttop warming and ALT increasing due to climate changing. About 26.9%, 59.9%, 80.1% of the current permafrost is likely to disappear by the end of the 21st century under SSP126, SSP245, and SSP585 scenarios, respectively. The simulation results may further provide new opportunities to assess the future impacts of climate warming on environments and engineering development over the QTP.

关 键 词：Climate change Analytical model Permafrost degradation Active-layer CMIP6 Qinghai‒Tibet Plateau(QTP) 

分 类 号：P46[天文地球—大气科学及气象学]