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DOI10.1007/s00382-020-05246-x
Influence of wintertime surface sensible heat flux variability over the central and eastern Tibetan Plateau on the East Asian winter monsoon
Chen L.; Zhang R.; Pryor S.C.; Li X.; Wang H.
发表日期2020
ISSN0930-7575
起始页码4589
结束页码4603
卷号54
英文摘要Analyses of in situ and reanalysis output are performed to examine linkages between surface sensible heat fluxes over the central and eastern Tibetan Plateau (CETP) and indices of the East Asian winter monsoon (EAWM) and wintertime near-surface air temperatures over China. The results demonstrate that the sensible heat fluxes over CETP exhibit substantial decadal variability with positive, negative and positive phase during 1980–1987, 1988–2002 and 2003–2014, respectively. This decadal variability exhibits statistically significant associations with sub-components of EAWM and surface temperature anomalies over eastern China. The recovery of decadal change in wintertime sensible heat fluxes from negative to positive phase over CETP over the past decade (since 2003) has been associated with intensification and northward displacement of the East Asian subtropical jet (EASJ), enhanced and westward displacement of East Asian trough and strengthening of the Siberian High. Such processes are associated with the strengthening of EAWM, as well as cold air advection from high latitudes towards the south. Increased wintertime sensible heat fluxes over CETP is associated with markedly changes in the meridional temperature gradient that in term intensifies upper-level zone flow in the EASJ region, which provides a key physical factor linking the anomalies of sensible heat fluxes and EAWM. © 2020, Springer-Verlag GmbH Germany, part of Springer Nature.
语种英语
scopus关键词advection; air temperature; boundary layer; decadal variation; monsoon; sensible heat flux; surface temperature; winter; China; Qinghai-Xizang Plateau
来源期刊Climate Dynamics
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/145454
作者单位Department of Atmospheric and Oceanic Sciences and Institute of Atmospheric Sciences, Fudan University, Shanghai, 200433, China; CAS Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences, Beijing, 100101, China; Department of Earth and Atmospheric Sciences, Cornell University, Ithaca, NY 14853, United States; School of Atmospheric Sciences, Chengdu University of Information Technology, Chendu, 610225, China; Key Laboratory of Meteorological Disaster, Ministry of Education (KLME)/Joint International Research Laboratory of Climate and Environment Change (ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science and Technology, Nanjing, 210044, China
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GB/T 7714
Chen L.,Zhang R.,Pryor S.C.,et al. Influence of wintertime surface sensible heat flux variability over the central and eastern Tibetan Plateau on the East Asian winter monsoon[J],2020,54.
APA Chen L.,Zhang R.,Pryor S.C.,Li X.,&Wang H..(2020).Influence of wintertime surface sensible heat flux variability over the central and eastern Tibetan Plateau on the East Asian winter monsoon.Climate Dynamics,54.
MLA Chen L.,et al."Influence of wintertime surface sensible heat flux variability over the central and eastern Tibetan Plateau on the East Asian winter monsoon".Climate Dynamics 54(2020).
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