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《Plateau Meteorology》 2004-06
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Relationship between Precipitation for Meiyu in Mid-and-Lower Reaches of the Yangtze River and Summer Precipitation over Eastern Part of Northwest China

WANG Xiao-fang~(1, 2),XIE Jin-nan~3,LUO Zhe-xian~1 Institute Meteorology, Nanjing 210044, China; 2. Wuhan Institute of Heavy Rain, China Meteorological Administration, Wuhan 430074, China; 3. Meteorological Bureau of Gansu Province, Lanzhou 730020, China)  
Using the Meiyu data in the mid-and-lower reaches of Yangtze River in the period from 1951 to 2000, the precipitation at 160 stations during 1951 to 2000 and the NCEP reanalysis data, the relationship between the precipitation for Meiyu in the mid-and-lower reaches of Yangtze River and the summer precipitation on the eastern side of the Northwest China was analyzed. The results show that, in the years of more precipitation for Meiyu, the summmer precipitation in the eastern part of the Northwest China is normal or drought; but in the years of less precipitation for Meiyu, vice versa. The composite flow pattern of the most (least) precipitation for Meiyu years is corresponding to the typical flow pattern for drought (rainy) years in the east of Northwest China. The different featares of 500 hPa height field in more(less) Meiyu years and its relation to the precipitation in east of Northwest China are numerically simulated by using the norhydrostatic version MM5 with one nested grid.
【Fund】: 甘肃省十五科技攻关计划项目"西北干旱成因及其应用研究"(GS012 A45 118)资助
【CateGory Index】: P426.613
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