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《SCIENTIA ATMOSPHERICA SINICA》 2000-06
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A Study of the Precipitation of the Tibetan Plateau Northeastern Side during Flood Seasons

Wang Baoling, Xie Jinnan, Wu Guoxiong and Yu Yaxun (Lanzhou Arid Meteorological Institule, Lanzhou 730020) (Gansu Meteorology Bureau, Lanzhou 730020) (State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, In  
The NCEP / NCAR reanalysis monthly 500 hPa grid data (2.5°x 2.5°Lat / Lon) and the monthly precipitation of the Tibetan Plateau Northeastern side from 1958 to 1997 are used and analyzed. The results show that: (l) The precipitation for the recent fourly years is obviously decreased in July, August and September when the precipitation is most concentrated. And the quasi-three year period oscillation, which distinctly existed in the past years, has been in low phase since the 1980s in the Tibetan Plateau Northeastern side. (2) It is the most typical drought indicator in July, August and Sep- tember of the Tibetan Plateau Northeastern side that the reduction of geopotential height near Japan to the northern Pacific and the intensification of Okhotsk blocking high. (3) For the drought flow patterns, the circulation of the drought years is very similar to that of the Changjiang-Huaihe Meiyu in July. In general, the heavy drought years occur in the Tibetan Plateau northeastern side when the rainy years occur in the Changjiang-Huaihe river basin. (4) The typical flow patterns during July to September for drought years in the Tibetan Plateau northeastern side are actually the EI Nino patterns. (5) The EI Nin o events have evident influence on the precipitation in the Tibetan Plateau northeastern side, i.e., the typical drought years usually appear in the EI Nino events years. In view of the time stage, the total precipitation during July to September is most closely correlated to the EI Nino events, and the relationship is most notable in September.
【Fund】: 国家“九五”重中之重项目! 96—908—05—03;; 甘肃省气象局科研项目! 98—04
【CateGory Index】: P426.6
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