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The link between interannual variation of the South China Sea summer monsoon onset and summer precipitation in Shandong Province
作者姓名:张苏平  刘秦玉  王建波
作者单位:[1]PhysicalOceanographyLab.&Ocean-AtmosphereInteractionandClimateLab.,OceanUniversityofChina,Qingdao266003,China [2]不详,OceanUniversityofChina,Qingdao266003,China [3]MeteorologicalBureauofTaian,Taian271000,China
基金项目:This paper is sponsored by natural science fund of Shandong Province (No.Y2003E01)
摘    要:Relationship between the onset date of South China Sea (SCS) summer monsoon and the summer rainfall in Shandong Province was examined by comprehensive analysis to establish a conceptual model of the link. If the summer monsoon occurs earlier, the 500 hPa level would induce the teleconnection of Eurasian pattern in the summer (June-August), which indicates that the western Pacific subtropical high is displaced northward further than usual, the Siberian high is intensified and the Okhotsk low is deepened. Under such circumstance, Shandong, located in the west side of the subtropical high and in front of the mid-Siberia high, would be expected to have a wet summer because it is quite possible for cold and warm air to meet and interact with each other in Shandong. Statistical analysis revealed that the 500 hPa anomalies over Korea and Japan were sensitive to the SCS monsoon onset date and very important to precipitation in Shandong, and that the convective activities over the deep water basin in the SCS in 24-26 pentads significantly influenced the position of the ridge line of the western Pacific subtropical high. These findings yielded better understanding of the causative mechanisms involved in the precipitation generation, so that the knowledge gained can possibly be applied for long-lead forecast.

关 键 词:中国  南海  季风  年际变化  夏季  山东
收稿时间:8 July 2003
修稿时间:21 December 2004

The link between interannual variation of the South China Sea summer monsoon onset and summer precipitation in Shandong Province
Zhang Suping,Liu Qinyu,Wang Jianbo.The link between interannual variation of the South China Sea summer monsoon onset and summer precipitation in Shandong Province[J].Chinese Journal of Oceanology and Limnology,2005,23(3):275-283.
Authors:Zhang Suping  Liu Qinyu  Wang Jianbo
Institution:(1) Physical Oceanography Lab. & Ocean-Atmosphere Interaction and Climate Lab., Ocean University of China, 266003 Qingdao, China;(2) Meteorological Bureau of Taian, 271000 Taian, China
Abstract:Relationship between the onset data of South China Sea (SCS) summer monsoon and the summer rainfall in Shandong Province was examined by comprehensive analysis to establish a conceptual model of the link. If the summer monsoon occurs earlier, the 500 hPa level would induce the teleconnection of Eurasian pattern in the summer (June–August), which indicates that the western Pacific subtropical high is displaced northward further than usual, the Siberian high is intensified and the Okhotsk low is deepened. Under such circumstance, Shandong, Iocated in the west side of the subtropical high and in front of the mid-Siberia high, would be expected to have a wet summer because it is quite possible for cold and warm air to meet and interact with each other in Shandong. Statistical analysis revealed that the 500 hPa anomalies over Korea and Japan were sensitive to the SCS monsoon onset date and very important to precipitation in Shandong, and that the convective activities over the deep water basin in the SCS in 24–26 pentads significantly influenced the position of the ridge line of the western Pacific subtropical high. These findings yielded better understanding of the causative mechanisms involved in the precipitation generation, so that the knowledge gained can possibly be applied for long-lead forecast. This paper is sponsored by natural science fund of Shandong, Province (No.Y2003E01)
Keywords:summer monsoon in SCS  interannual variations  summer rainfall in Shandong
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