Seasonal Variation of the Westerly Jet over Asia in the Last Glacial Maximum: Role of the Tibetan Plateau Heating
Lei, Jing1; Shi, Zhengguo1,2,3,4; Xie, Xiaoning1; Sha, Yingying1; Li, Xinzhou1; Liu, Xiaodong1; An, Zhisheng1
刊名JOURNAL OF CLIMATE
2021-04-01
卷号34期号:7页码:2723-2740
关键词Atmospheric circulation Orographic effects Ice age General circulation models
ISSN号0894-8755
DOI10.1175/JCLI-D-20-0438.1
通讯作者Shi, Zhengguo(shizg@ieecas.cn)
英文摘要The westerly jet (WJ) is an important component of atmospheric circulation, which is characterized by prominent seasonal variations in intensity and position. However, the response of the WJ over Asia during the Last Glacial Maximum (LGM) is still not clear. Using general circulation model experiments, the seasonal behaviors of the WJ over central Asia and Japan are analyzed in this paper. The results show that, compared to the present day (PD), the WJ presents a complicated response during the LGM, both in intensity and position. Over central Asia, it becomes weaker in both summer and winter. But over Japan, it is enhanced in summer but becomes diminished in winter. In terms of position, the WJ over central Asia shifts southward in both summer and winter, whereas the WJ over Japan moves southward in summer but does not change obviously relative to PD in winter. Such WJ changes are well explained by meridional temperature gradients in high troposphere, which is closely linked to seasonal thermal anomalies over the Tibetan Plateau (TP). Despite cooler LGM conditions, the anomalous warming center over the TP becomes stronger in summer. Derived from the heat budget equation, the stronger heating center is mainly caused by the weaker adiabatic cooling generated from ascending motion over the area south of the TP. In winter, the cooling over the TP is also strengthened, mostly owing to the subsidence-induced weaker adiabatic heating. Due to the importance of the WJ, the potential role of TP thermal effects should be a focus when explaining the East Asian climate change during the LGM.
资助项目Strategic Priority Research Program of the Chinese Academy of Sciences[XDB40030000] ; National Natural Science Foundation of China[41888101] ; National Natural Science Foundation of China[41977382] ; Youth Innovation Promotion Association CAS
WOS关键词ATMOSPHERIC CIRCULATION ; NUMERICAL-SIMULATION ; RADIATIVE FEEDBACKS ; SUBTROPICAL JET ; MONSOON ONSET ; EAST-ASIA ; ICE-AGE ; CLIMATE ; EVOLUTION ; RAINFALL
WOS研究方向Meteorology & Atmospheric Sciences
语种英语
出版者AMER METEOROLOGICAL SOC
WOS记录号WOS:000644142700019
资助机构Strategic Priority Research Program of the Chinese Academy of Sciences ; National Natural Science Foundation of China ; Youth Innovation Promotion Association CAS
内容类型期刊论文
源URL[http://ir.ieecas.cn/handle/361006/16409]  
专题地球环境研究所_古环境研究室
第四纪科学与全球变化卓越创新中心
通讯作者Shi, Zhengguo
作者单位1.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian, Peoples R China
2.Chinese Acad Sci, Ctr Excellence Quaternary Sci & Global Change, Xian, Peoples R China
3.Xi An Jiao Tong Univ, Inst Global Environm Change, Xian, Peoples R China
4.Pilot Natl Lab Marine Sci & Technol, Open Studio Ocean Continental Climate & Environm, Qingdao, Peoples R China
推荐引用方式
GB/T 7714
Lei, Jing,Shi, Zhengguo,Xie, Xiaoning,et al. Seasonal Variation of the Westerly Jet over Asia in the Last Glacial Maximum: Role of the Tibetan Plateau Heating[J]. JOURNAL OF CLIMATE,2021,34(7):2723-2740.
APA Lei, Jing.,Shi, Zhengguo.,Xie, Xiaoning.,Sha, Yingying.,Li, Xinzhou.,...&An, Zhisheng.(2021).Seasonal Variation of the Westerly Jet over Asia in the Last Glacial Maximum: Role of the Tibetan Plateau Heating.JOURNAL OF CLIMATE,34(7),2723-2740.
MLA Lei, Jing,et al."Seasonal Variation of the Westerly Jet over Asia in the Last Glacial Maximum: Role of the Tibetan Plateau Heating".JOURNAL OF CLIMATE 34.7(2021):2723-2740.
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