Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1007/s00382-017-3898-0 |
Early summer southern China rainfall variability and its oceanic drivers | |
Li, Weijing1,2; Ren, Hong-Chang1,3; Zuo, Jinqing1,2; Ren, Hong-Li2 | |
2018-06-01 | |
发表期刊 | CLIMATE DYNAMICS
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ISSN | 0930-7575 |
EISSN | 1432-0894 |
出版年 | 2018 |
卷号 | 50页码:4691-4705 |
文章类型 | Article |
语种 | 英语 |
国家 | Peoples R China |
英文摘要 | Rainfall in southern China reaches its annual peak in early summer (May-June) with strong interannual variability. Using a combination of observational analysis and numerical modeling, the present study investigates the leading modes of this variability and its dynamic drivers. A zonal dipole pattern termed the southern China Dipole (SCD) is found to be the dominant feature in early summer during 1979-2014, and is closely related to a low-level anomalous anticyclone over the Philippine Sea (PSAC) and a Eurasian wave-train pattern over the mid-high latitudes. Linear regressions based on observations and numerical experiments using the CAM5 model suggest that the associated atmospheric circulation anomalies in early summer are linked to decaying El Nio-Southern Oscillation-like sea surface temperature (SST) anomalies in the tropical Pacific, basin-scale SST anomalies in the tropical Indian Ocean, and meridional tripole-like SST anomalies in the North Atlantic in the previous winter to early summer. The tropical Pacific and Indian Ocean SST anomalies primarily exert an impact on the SCD through changing the polarity of the PSAC, while the North Atlantic tripole-like SST anomalies mainly exert a downstream impact on the SCD by inducing a Eurasian wave-train pattern. The North Atlantic tripole-like SST anomalies also make a relatively weak contribution to the variations of the PSAC and SCD through a subtropical teleconnection. Modeling results indicate that the three-basin combined forcing has a greater impact on the SCD and associated circulation anomalies than the individual influence from any single oceanic basin. |
英文关键词 | Rainfall variability South China SST anomalies Teleconnections |
领域 | 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000432597400041 |
WOS关键词 | SEA-SURFACE TEMPERATURE ; TROPICAL ATLANTIC SST ; WATER-VAPOR TRANSPORT ; INDO-WESTERN PACIFIC ; EAST-ASIAN CLIMATE ; EL-NINO ; MONSOON RAINFALL ; NORTH PACIFIC ; ANOMALOUS ANTICYCLONE ; INDIAN-OCEAN |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/35696 |
专题 | 气候变化 |
作者单位 | 1.Nanjing Univ Informat Sci & Technol, Collaborat Innovat Ctr Forecast & Evaluat Meteoro, Nanjing, Jiangsu, Peoples R China; 2.China Meteorol Adm, Natl Climate Ctr, Lab Climate Studies, Beijing 100081, Peoples R China; 3.China Meteorol Adm, Natl Meteorol Ctr, Beijing 100081, Peoples R China |
推荐引用方式 GB/T 7714 | Li, Weijing,Ren, Hong-Chang,Zuo, Jinqing,et al. Early summer southern China rainfall variability and its oceanic drivers[J]. CLIMATE DYNAMICS,2018,50:4691-4705. |
APA | Li, Weijing,Ren, Hong-Chang,Zuo, Jinqing,&Ren, Hong-Li.(2018).Early summer southern China rainfall variability and its oceanic drivers.CLIMATE DYNAMICS,50,4691-4705. |
MLA | Li, Weijing,et al."Early summer southern China rainfall variability and its oceanic drivers".CLIMATE DYNAMICS 50(2018):4691-4705. |
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