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《SCIENTIA ATMOSPHERICA SINICA》 1997-03
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A Study of Summer Precipitation Features and Anomaly in Northwest China

Li Dongliang and Xie Jinnan (Meteorological Bureau ofGansu Province, Lanzhou730020) Wang Wen (Department ofAtmospheric Sciences, Lanzhou University, Lanzhou730000)  
With EOF, REOF, spectral analysis and atmospheric circulation model, the spatial anomaly features and time evolution rule and the mechanism of summer precipitation anomaly in Northwest China are studied by using the precipitation data in June, July and August for the period 1960~1990 from 90 observational stations. The results show that the first three loading vector fields could reflect the whole anomaly structures of summer rainfall in Northwest China, for example, wet or dry in all area pattern, wet (or dry) in east and dry (or wet) in west pattern, wet (or dry) in north and dry (or wet) in south pattern. The first six rotated loading vector fields represent six principal precipitation anomaly areas: east of the Qinghai-Xizang Plateau, the Weishui River basin, the Qinghai plateau, northern Xinjiang, the desert basin and Hexi corridor. The rotated principal component and the data in the representative stations show that in the recent 30~60 years, the driest period was in the 1960′s and 1970′s in Northwest China. From the 1980′s to early 1990′s, an increasing rainfall trend, more and less, appeared in every area except desert basin. When the sensible heat anomaly in the underlying surface is strong in the Qinghai-Xizang Plateau in early summer (June), the northern Northwest China is wet in the same time, but the western, northern Northwest China is dry and the eastern and southern is wet in July and August. The numerical experiment of IAP 2-L AGCM shows that when the sensible heat anomaly in the underlying surface increases in the Qinghai-Xizang Plateau in summer, the subtropical ridge in the western Pacific Ocean elongates westerly and the warm and cold air meets in the upstream of the Yangtze River and Yellow River. As a result, the rainfall increases in the eastern Northwest China. The wet areas are in the southeastern Qinghai, southern Gansu and south-eastern Shaanxi, and the dry center is in the west of the northwestern area.
【Fund】: 国家“九五”重中之重科技项目专题的资助
【CateGory Index】: P426.622
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