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ANALYSES OF INTRASEASONAL OSCILLATION CHARACTERISTICS OF FLOOD-CAUSING RAINSTORMS IN XIJIANG RIVER VALLEY DURING THE ANNUALLY FIRST RAINING SEASON IN THE PAST YEARS 被引量:1
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作者 罗秋红 纪忠萍 +2 位作者 吴乃庚 蔡洁云 孙汉明 《Journal of Tropical Meteorology》 SCIE 2011年第2期136-146,共11页
Based on the daily precipitation data of nine stations representing the Xijiang River valley and the National Center for Environmental Prediction/National Center for Atmospheric Research (USA) reanalysis data, this st... Based on the daily precipitation data of nine stations representing the Xijiang River valley and the National Center for Environmental Prediction/National Center for Atmospheric Research (USA) reanalysis data, this study uses the wavelet analysis and band-pass filter methods to investigate the atmospheric intraseasonal oscillation characteristics of flood-causing rainstorms in the valley during the annually first raining seasons in 1968, 1994, 1998, 2002 and 2005. Results show that the daily precipitation in the valley exhibits significant quasi-biweekly (10 to 20 days) oscillations. The flood-causing rainstorms in the valley were mainly associated with the confluence of low-frequency warm and humid airflow in the lower latitudes and cold and dry airflow in the higher latitudes. The low-frequency vortexes were propagating or in control when this type of rainstorms took place over the valley, being favorable for the convergence of moisture at lower levels and thus vital to the formation of the rainstorms. 展开更多
关键词 rainstorms intraseasonal oscillation filter Xijiang river valley annually first raining season
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渭河流域两次暴雨过程中尺度诊断对比分析
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作者 李春娥 王英 《咸阳师范学院学报》 2011年第2期76-80,共5页
采用25点低通滤波技术对2006年6月2—3日和2007年8月8—9日渭河流域两次突发暴雨过程环流形势和动力学特征进行了分析,探索渭河流域致洪暴雨形成的中尺度动力机制。结果表明:中低层(700~850hPa)中尺度切变线或辐合是这两次暴雨过程产... 采用25点低通滤波技术对2006年6月2—3日和2007年8月8—9日渭河流域两次突发暴雨过程环流形势和动力学特征进行了分析,探索渭河流域致洪暴雨形成的中尺度动力机制。结果表明:中低层(700~850hPa)中尺度切变线或辐合是这两次暴雨过程产生的直接影响系统,产生于滤波前中低层弱切变线左侧大约50~100km处;垂直运动的上升支两侧有对称分布的下沉运动中心相对应,证明了中尺度次级环流的存在。垂直次级环流圈的形成促进了上升支强烈上升运动的发展,为强对流和暴雨天气提供了良好的动力条件。随着中尺度次级环流缓慢向东北方向移动,强降水区逐渐向次级环流上升支的右侧扩展;正涡度中心向上伸展加强,表明中尺度气旋加深,增强,范围增大,有利于中低层气旋性环流的生成和发展,对暴雨的产生和维持起到了重要作用。 展开更多
关键词 渭河流域暴雨 中尺度诊断分析 中尺度垂直次级环流
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