globalchange  > 气候变化事实与影响
DOI: 10.1175/JCLI-D-16-0041.1
Scopus记录号: 2-s2.0-85010840101
论文题名:
Impacts of spatiotemporal anomalies of tibetan plateau snow cover on summer precipitation in Eastern China
作者: Wang C.; Yang K.; Li Y.; Wu D.; Bo Y.
刊名: Journal of Climate
ISSN: 8948755
出版年: 2017
卷: 30, 期:3
起始页码: 885
结束页码: 903
语种: 英语
Scopus关键词: Fighter aircraft ; Kinetic energy ; Kinetics ; Precipitation (chemical) ; Precipitation (meteorology) ; Rain ; Singular value decomposition ; Watersheds ; Atmosphere-land interactions ; Forcing ; Geo-potential heights ; Planetary atmosphere ; Singular value decomposition method ; Snow covers ; Spatiotemporal distributions ; Temporal and spatial variation ; Snow ; air-soil interaction ; kinetic energy ; planetary atmosphere ; precipitation (climatology) ; rainfall ; snow cover ; summer ; water vapor ; China ; East China Sea ; Pacific Ocean ; Qinghai-Xizang Plateau ; Yangtze River
英文摘要: Tibetan Plateau (TP) snow cover undergoes significant temporal and spatial variations during the winter and spring months. This study investigates the relationship between the spatiotemporal distribution of winter-spring snow cover (SC) over the TP and summer precipitation in eastern China (EC) using the singular value decomposition (SVD) method. Four simulation experiments are designed to validate the results of SVD analysis. Both observations and simulations show that heavier snow cover in the southern TP leads to more rainfall in the Yangtze River basin and northeastern China, and less precipitation in southern China, whereas heavier snow cover in the northern TP results in enhanced rainfall in southeastern and northern China and weakened precipitation in the Yangtze River basin. The linkage is attributed to anomalous westerly winds in the upper troposphere at around 200 hPa and to changes of the southern branch of westerlies at 500 hPa on the south side of the TP, which are caused by lasting diabatic heat anomalies over the TP. The shifts in position of the westerly jet at the exit region and negative anomalies of geopotential height at 500 hPa further result in anomalous anticyclone over the East China Sea and the corresponding 850-hPa water vapor convergence and influence the anomalous summer precipitation belt in EC.
资助项目: NSFC, National Natural Science Foundation of China ; NSFC, National Natural Science Foundation of China ; NSFC, National Natural Science Foundation of China ; NSFC, National Natural Science Foundation of China
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/49863
Appears in Collections:气候变化事实与影响

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作者单位: Key Laboratory of Arid Climate Change and Disaster Reduction of Gansu Province, College of Atmospheric Sciences, Lanzhou University, Lanzhou, China

Recommended Citation:
Wang C.,Yang K.,Li Y.,et al. Impacts of spatiotemporal anomalies of tibetan plateau snow cover on summer precipitation in Eastern China[J]. Journal of Climate,2017-01-01,30(3)
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