气候变化领域集成服务门户(CCPortal): Linkage between moisture transport over the Yangtze River Basin and a critical area of the Tibetan Plateau during the Meiyu

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DOI	10.1007/s00382-019-04648-w
	Linkage between moisture transport over the Yangtze River Basin and a critical area of the Tibetan Plateau during the Meiyu
	Dong L.; Xu X.; Zhao T.; Ren H.
发表日期	2019
ISSN	0930-7575
起始页码	2643
结束页码	2662
卷号	53 期号:2020-05-06
英文摘要	Located downstream of the Tibetan Plateau (TP), the Yangtze River Basin (YRB) in China frequently experiences torrential rainfall and severe rainstorms within the zonally elongate Meiyu belt. Inter-annual variations in drought and flooding in the YRB are shown to be highly correlated with the upstream surface latent heat flux (SLHF) over the TP, suggesting that the SLHF over the TP can be a “strong signal” of Meiyu variability. Results show that the southeastern margin of the TP (SEMTP) is the most “sensitivity area” of the “strong signal”. On inter-annual scales, low (high) SLHF over the SEMTP corresponds to high (low) humidity at upper levels, strong (weak) zonal moisture transport and a southerly (northerly) pattern of East Asian summer monsoon (EASM) moisture transport circulation in July. The anomalous moisture flow originating from the mid to low latitude oceans, converges in the east of the SEMTP and turns eastward (northward); thus, the SEMTP acts as the key area of redirection of moisture flow. The ridge of moisture transport is located at about 22.5°N (29.5°N) in East China for low (high) SLHF over the SEMTP. Under low SLHF conditions, the warm, humid airflow from the SEMTP creates favorable conditions for Meiyu rainfall and torrential rainstorms. Numerical simulation and sensitivity analyses using the mesoscale Weather Research and Forecasting (WRF) model further reveal that SLHF over the SEMTP shows pronounced “strong signal” features. The variation of intensity of SLHF over the SEMTP corresponds to the moisture transport structure of the Meiyu rain belt and the location of the ridge of the subtropical high in East China. An increase in the apparent heat source Q1 over the main body of the TP might explain the “strong signal” over the SEMTP. This apparent heat source plays an important role in modulating both the SLHF over the SEMTP and the location of the subtropical high circulation system. © 2019, Springer-Verlag GmbH Germany, part of Springer Nature.
英文关键词	Meiyu; Moisture transport; Surface latent heat flux; Yangtze River Basin; “Sensitivity area” of the Tibetan Plateau; “Strong signal”
语种	英语
scopus关键词	latent heat flux; moisture transfer; monsoon; rainfall; surface flux; weather forecasting; China; Qinghai-Xizang Plateau; Yangtze Basin
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/146050
作者单位	Nanjing University of Information Science and Technology, Nanjing, 210044, China; State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing, 100081, China; National Meteorological Center, China Meteorological Administration, Beijing, 100081, China
推荐引用方式 GB/T 7714	Dong L.,Xu X.,Zhao T.,et al. Linkage between moisture transport over the Yangtze River Basin and a critical area of the Tibetan Plateau during the Meiyu[J],2019,53(2020-05-06).
APA	Dong L.,Xu X.,Zhao T.,&Ren H..(2019).Linkage between moisture transport over the Yangtze River Basin and a critical area of the Tibetan Plateau during the Meiyu.Climate Dynamics,53(2020-05-06).
MLA	Dong L.,et al."Linkage between moisture transport over the Yangtze River Basin and a critical area of the Tibetan Plateau during the Meiyu".Climate Dynamics 53.2020-05-06(2019).