The change of climate and terrestrial carbon cycle over Tibetan Plateau in CMIP5 models
文献类型：期刊论文
| 作者 | Li, Suosuo1,2; Lu, Shihua1; Gao, Yanhong1; Ao, Yinhuan1 |
| 刊名 | INTERNATIONAL JOURNAL OF CLIMATOLOGY
 |
| 出版日期 | 2015-11-30 |
| 卷号 | 35期号:14页码:4359-4369 |
| 关键词 | CMIP5 climate change carbon cycle multi-model ensemble (MME) Tibetan Plateau |
| ISSN号 | 0899-8418 |
| DOI | 10.1002/joc.4293 |
| 通讯作者 | Li, Suosuo(liss@lzb.ac.cn) |
| 英文摘要 | Six earth system models from phase 5 of the Coupled Model Inter-comparison Project (CMIP5) are evaluated over Tibetan Plateau (TP) by comparing the modelled temperature (Tas), precipitation (Pr), net primary production (NPP) and leaf area index (LAI) with the observed Tas, Pr, International Geosphere Biosphere Program (IGBP) NPP and Max-Planck Institute for Meteorology (MPIM) LAI in the historical, and then we analysed the change of climate and carbon cycle and explored the relationship between the carbon cycle and main climatic drivers in the historical and representative concentration pathway 4.5 (RCP4.5) simulation over TP. While model results differ, their region spatial distributions from 1971 to 2000 agree reasonably with observed Tas, Pr and proxy LAI and NPP. The climatic variables, LAI and carbon flux vary between two simulations, the ration of NPP to gross primary production (GPP) does not change much in the historical and RCP4.5 scenarios. The linear trends of LAI and carbon flux show an obvious continuous increase from historical climatic period (1971-2000) to the first two climatic periods (2011-2040; 2041-2700) of RCP4.5, then the trends decrease in the third climatic period (2071-2100) of RCP4.5. The cumulative multi-model ensemble (MME) net biome production (NBP) is 0.32 kg C m(-2) year(-1) during 1850-2005 and 1.43 kg C m(-2) year(-1) during 2006-2100, the TP is a carbon sink during the historical scenario, and TP will uptake more carbon from atmosphere during 2006-2100 than 1850-2005 under RCP4.5 scenario. LAI, GPP, NPP, Ra and Rh appear more related to the Tas than Pr and Rsds, and the Tas is the primary climatic driver for the plant growth and carbon cycle. With the climate change in 21st century under RCP4.5 scenario, Tas still is the primary climate driver for the plant growth and carbon cycle, but the effect of temperature on plant growth and carbon cycle gets weaker. |
| 收录类别 | SCI |
| WOS关键词 | GLOBAL SOLAR-RADIATION ; NPP ; MONSOON ; CHINA ; RATIO ; WATER |
| WOS研究方向 | Meteorology & Atmospheric Sciences |
| WOS类目 | Meteorology & Atmospheric Sciences |
| 语种 | 英语 |
| WOS记录号 | WOS:000365518600026 |
| 出版者 | WILEY-BLACKWELL |
| URI标识 | http://www.irgrid.ac.cn/handle/1471x/2557172 |
| 专题 | 寒区旱区环境与工程研究所 |
| 通讯作者 | Li, Suosuo |
| 作者单位 | 1.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Key Lab Land Surface Proc & Climate Change Cold &, Lanzhou 730000, Gansu, Peoples R China 2.China Meteorol Adm, Inst Arid Meteorol, CMA,Gansu Prov & Key Lab Arid Climat Change & Red, Key Lab Arid Climat Change & Reduct Disaster, Lanzhou, Gansu, Peoples R China |
| 推荐引用方式 GB/T 7714 | Li, Suosuo,Lu, Shihua,Gao, Yanhong,et al. The change of climate and terrestrial carbon cycle over Tibetan Plateau in CMIP5 models[J]. INTERNATIONAL JOURNAL OF CLIMATOLOGY,2015,35(14):4359-4369. |
| APA | Li, Suosuo,Lu, Shihua,Gao, Yanhong,&Ao, Yinhuan.(2015).The change of climate and terrestrial carbon cycle over Tibetan Plateau in CMIP5 models.INTERNATIONAL JOURNAL OF CLIMATOLOGY,35(14),4359-4369. |
| MLA | Li, Suosuo,et al."The change of climate and terrestrial carbon cycle over Tibetan Plateau in CMIP5 models".INTERNATIONAL JOURNAL OF CLIMATOLOGY 35.14(2015):4359-4369. |
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来源：寒区旱区环境与工程研究所
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