Arid
DOI10.1111/1755-6724.14542
The PMIP3 Simulated Climate Changes over Arid Central Asia during the Mid-Holocene and Last Glacial Maximum
Xu Hongna; Wang Tao; Wang Huijun; Miao Jiapeng; Chen Jianhui; Chen Shengqian
通讯作者Wang, T
来源期刊ACTA GEOLOGICA SINICA-ENGLISH EDITION
ISSN1000-9515
EISSN1755-6724
出版年2020
卷号94期号:3页码:725-742
英文摘要In this study, the climate changes over Arid Central Asia (ACA) during the mid-Holocene (approximately 6,000 calendar years ago, MH) and the Last Glacial Maximum (approximately 21,000 calendar years ago, LGM) were investigated using multimodel simulations derived from the Paleoclimate Modelling Intercomparison Project Phase 3 (PMIP3). During the MH, the multimodel median (MMM) shows that in the core region of ACA, the regionally averaged annual surface air temperature (SAT) decreases by 0.13 degrees C and annual precipitation decreases by 3.45%, compared with the preindustrial (PI) climate. The MMM of the SAT increases by 1.67/0.13 degrees C in summer/autumn, whereas it decreases by 1.23/1.11 degrees C in spring/winter. The amplitude of the seasonal cycles of the SAT increases over ACA due to different MH orbital parameters. For precipitation, the regionally averaged MMM decreases by 5.77%/5.69%/0.39%/5.24% in spring/summer/autumn/winter, respectively. Based on the analysis of the aridity index (AI), compared with the PI, a drier climate appears in southern Central Asia and western Xinjiang due to decreasing precipitation. During the LGM, the MMM shows that the regionally averaged SAT decreases by 5.04/4.36/4.70/5.12/5.88 degrees C and precipitation decreases by 27.78%/28.16%/31.56%/27.74%/23.29% annually and in the spring, summer, autumn, and winter, respectively. Robust drying occurs throughout almost the whole core area. Decreasing precipitation plays a dominant role in shaping the drier conditions, whereas strong cooling plays a secondary but opposite role. In response to the LGM external forcings, over Central Asia and Xinjiang, the seasonal cycle of precipitation has a smaller amplitude compared with that under the PI climate. In the model-data comparison, the simulated MH moisture changes over ACA are to some extent consistent with the reconstructions, further confirming that drier conditions occurred during that period than during the PI.
英文关键词PMIP3 climate changes Arid Central Asia mid-Holocene Last Glacial Maximum
类型Article
语种英语
收录类别SCI-E
WOS记录号WOS:000544351300016
WOS关键词SOUTHERN ALTAI MOUNTAINS ; ENVIRONMENTAL-CHANGES ; HOLOCENE CLIMATE ; COUPLED SIMULATIONS ; MOISTURE EVOLUTION ; GLOBAL TEMPERATURE ; VEGETATION CHANGES ; NORTHERN XINJIANG ; SUMMER CLIMATE ; PEAT SEQUENCE
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
来源机构兰州大学 ; 中国科学院大气物理研究所 ; 南京信息工程大学
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/324877
作者单位[Xu Hongna; Wang Tao; Wang Huijun] Nanjing Univ Informat Sci & Technol, Collaborat Innovat Ctr Forecast & Evaluat Meteoro, Nanjing 210044, Peoples R China; [Wang Tao; Wang Huijun] Chinese Acad Sci, Climate Change Res Ctr, Beijing 100029, Peoples R China; [Wang Tao; Wang Huijun; Miao Jiapeng] Chinese Acad Sci, Nansen Zhu Int Res Ctr, Inst Atmospher Phys, Beijing 100029, Peoples R China; [Wang Huijun] Nanjing Univ Informat Sci & Technol, Key Lab Meteorol Disaster, Nanjing 210044, Peoples R China; [Miao Jiapeng] Univ Chinese Acad Sci, Beijing 100029, Peoples R China; [Chen Jianhui; Chen Shengqian] Lanzhou Univ, Coll Earth & Environm Sci, Key Lab Western Chinas Environm Syst, Lanzhou 730000, Peoples R China
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Xu Hongna,Wang Tao,Wang Huijun,et al. The PMIP3 Simulated Climate Changes over Arid Central Asia during the Mid-Holocene and Last Glacial Maximum[J]. 兰州大学, 中国科学院大气物理研究所, 南京信息工程大学,2020,94(3):725-742.
APA Xu Hongna,Wang Tao,Wang Huijun,Miao Jiapeng,Chen Jianhui,&Chen Shengqian.(2020).The PMIP3 Simulated Climate Changes over Arid Central Asia during the Mid-Holocene and Last Glacial Maximum.ACTA GEOLOGICA SINICA-ENGLISH EDITION,94(3),725-742.
MLA Xu Hongna,et al."The PMIP3 Simulated Climate Changes over Arid Central Asia during the Mid-Holocene and Last Glacial Maximum".ACTA GEOLOGICA SINICA-ENGLISH EDITION 94.3(2020):725-742.
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