Direct radiative effects of dust aerosols emitted from the TibetanPlateau on the East Asian summer monsoon – a regional climatemodel simulation

doi:10.5194/acp-17-13731-2017

IEECAS OpenIR > 古环境研究室

	Direct radiative effects of dust aerosols emitted from the TibetanPlateau on the East Asian summer monsoon – a regional climatemodel simulation
	Sun,H(Sun,Hui)1; Liu,XD(Liu,Xiaodong)1,2; Pan,ZT(Pan,Zitao)3,4; Sun,Hui
	2017-11
发表期刊	Atmospheric Chemistry and Physics
卷号	17 期号:22 页码:13731-13745
文章类型	期刊论文
其他摘要	While dust aerosols emitted from major Asian sources such as Taklimakan and Gobi deserts have been shown to have strong effect on Asian monsoon and climate, the role of dust emitted from Tibetan Plateau (TP) itself, where aerosols can directly interact with the TP heat pump because of their physical proximity both in location and elevation, has not been examined. This study uses the dust-coupled RegCM4.1 regional climate model (RCM) to simulate the spatiotemporal distribution of dust aerosols originating within the TP and their radiative effects on the East Asian summer monsoon (EASM) during both heavy and light dust years. Two 20-year simulations with and without the dust emission from TP showed that direct radiative cooling in the mid-troposphere induced by the TP locally produced dust aerosols resulted in an overall anticyclonic circulation anomaly in the low troposphere centered over the TP region. The northeasterly anomaly in the EASM region reduces its strength considerably. The simulations found a significant negative correlation between the TP column dust load produced by local emissions and the corresponding anomaly in the EASM index (r = −0.46). The locally generated TP dust can cause surface cooling far downstream in Bohai Gulf and the China–North Korea border area through stationary Rossby wave propagation. Although dust from within TP (mainly Qaidam Basin) is a relatively small portion of total Asian aerosols, its impacts on Asian monsoon and climate seems disproportionately large, likely owning to its higher elevation within TP itself.
DOI	10.5194/acp-17-13731-2017
收录类别	SCI
所属项目编号	2016YFA0601904 ; 41405093 ; 41572150 ; 41475085
语种	英语
项目资助者	National Key Research and DevelopmentProgram of China ; National Key Research and DevelopmentProgram of China ; National NaturalScience Foundation of China ; National NaturalScience Foundation of China
引用统计	被引频次：18[WOS] [WOS记录] [WOS相关记录]
文献类型	期刊论文
条目标识符	http://ir.ieecas.cn/handle/361006/5590
专题	古环境研究室
通讯作者	Sun,Hui
作者单位	1.SKLLQG, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an, 710061, China 2.CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing, 100101, China 3.Department of Earth and Atmospheric Sciences, Saint Louis University, St. Louis, Missouri, MO 63108, USA 4.Key Laboratory of Meteorological Disaster, Ministry of Education, Nanjing University of Information Science andTechnology, Nanjing, Jiangsu, China
推荐引用方式 GB/T 7714	Sun,H(Sun,Hui),Liu,XD(Liu,Xiaodong),Pan,ZT(Pan,Zitao),等. Direct radiative effects of dust aerosols emitted from the TibetanPlateau on the East Asian summer monsoon – a regional climatemodel simulation[J]. Atmospheric Chemistry and Physics,2017,17(22):13731-13745.
APA	Sun,H,Liu,XD,Pan,ZT,&Sun,Hui.(2017).Direct radiative effects of dust aerosols emitted from the TibetanPlateau on the East Asian summer monsoon – a regional climatemodel simulation.Atmospheric Chemistry and Physics,17(22),13731-13745.
MLA	Sun,H,et al."Direct radiative effects of dust aerosols emitted from the TibetanPlateau on the East Asian summer monsoon – a regional climatemodel simulation".Atmospheric Chemistry and Physics 17.22(2017):13731-13745.

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