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DOI | 10.1007/s00704-021-03631-y |
Change in soil organic carbon and its climate drivers over the Tibetan Plateau in CMIP5 earth system models | |
Li, Suosuo; Liu, Yuanpu; Lyu, Shihua; Wang, Shaoying; Pan, Yongjie; Qin, Yanyan | |
通讯作者 | Li, SS (通讯作者),Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Key Lab Land Surface Proc & Climate Change Cold &, Lanzhou 730000, Peoples R China. |
发表日期 | 2021 |
ISSN | 0177-798X |
EISSN | 1434-4483 |
起始页码 | 187 |
结束页码 | 196 |
卷号 | 145期号:1-2 |
英文摘要 | Soil organic carbon (SOC) is the largest carbon pool in the terrestrial carbon cycle, which is closely linked to climate change and global warming feedbacks. Based on proxy observation data and outputs from the fifth phase of the Coupled Model Inter-comparison Project (CMIP5), we analyzed quantitatively the spatial distribution and temporal change for SOC using boosted regression trees (BRT) over the Tibetan Plateau (TP). The ensemble proxy observation SOC stock data indicated a decreasing spatial distribution from southeast to northwest over the TP. We used data from ten CMIP5 earth system models (ESMs) for SOC, which exhibited differences. However, the CMIP5 multi-model ensemble (MME) result presented a similar spatial distribution pattern to the ensemble proxy observation SOC, while SOC storage and turnover times from the CMIP5 MME model were less than the ensemble proxy observation. The BRT results indicated that air temperature (Ta) accounted for 44.81% of the relative contribution and was the most influential variable on MME SOC. This was followed by net primary production (NPP), with a 19.09% relative contribution. The relative influence of the top 10 cm soil temperature, total soil water, and precipitation on MME SOC was 13.55%, 12.68%, and 9.87%, respectively. Using the BRT method to determine the spatial distribution of relative contribution of SOC for these five variables demonstrated that Ta was mainly higher over the central and northwestern regions of the TP, and NPP was higher over the western central regions and along the plateau's eastern edge. The statistical frequency of maximum relative contribution to SOC for the five variables indicated that the relative contribution of NPP covered the largest area, with 32% of the total grid numbers, followed by Ta, with 25%. |
关键词 | NET PRIMARY PRODUCTIONTURNOVER TIMESPERMAFROSTUNCERTAINTYVEGETATIONPATTERNSIMPACTSCHINAWATERFLUX |
语种 | 英语 |
WOS研究方向 | Meteorology & Atmospheric Sciences |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS记录号 | WOS:000643182000001 |
来源期刊 | THEORETICAL AND APPLIED CLIMATOLOGY |
来源机构 | 中国科学院西北生态环境资源研究院 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/253940 |
作者单位 | [Li, Suosuo; Wang, Shaoying; Pan, Yongjie; Qin, Yanyan] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Key Lab Land Surface Proc & Climate Change Cold &, Lanzhou 730000, Peoples R China; [Liu, Yuanpu] China Meteorol Adm, Key Lab Arid Climat Change & Reduct Disaster, Gansu Prov & Key Lab Arid Climat Change & Reduct, Inst Arid Meteorol, Lanzhou 730020, Peoples R China; [Lyu, Shihua] Chengdu Univ Informat Technol, Sch Atmospher Sci, Plateau Atmosphere & Environm Key Lab Sichuan Pro, Chengdu 610225, Peoples R China |
推荐引用方式 GB/T 7714 | Li, Suosuo,Liu, Yuanpu,Lyu, Shihua,et al. Change in soil organic carbon and its climate drivers over the Tibetan Plateau in CMIP5 earth system models[J]. 中国科学院西北生态环境资源研究院,2021,145(1-2). |
APA | Li, Suosuo,Liu, Yuanpu,Lyu, Shihua,Wang, Shaoying,Pan, Yongjie,&Qin, Yanyan.(2021).Change in soil organic carbon and its climate drivers over the Tibetan Plateau in CMIP5 earth system models.THEORETICAL AND APPLIED CLIMATOLOGY,145(1-2). |
MLA | Li, Suosuo,et al."Change in soil organic carbon and its climate drivers over the Tibetan Plateau in CMIP5 earth system models".THEORETICAL AND APPLIED CLIMATOLOGY 145.1-2(2021). |
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