| 连晴和连阴雨前两支气流变化的一般特点 |
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| 引用本文： | 刘延英,彭治班.连晴和连阴雨前两支气流变化的一般特点[J].应用气象学报,1990,1(3):298-304. |
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| 作者姓名： | 刘延英 彭治班 |
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| 作者单位： | 1.国家气象局气象科学研究院
(刘延英)，国家气象局气象科学研究院(彭治班) |
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| 基金项目： | “长江中下游连阴雨、连晴天气研究”，“国家气象局高原基金”课题 |
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| 摘 要： | 本文使用10次连晴和7次连阴雨天气过程合成资料，分析了长江中下游春季连晴和连阴雨前700hPa的流场及青藏高原东北侧和东南侧两支气流变化的一般特点。结果发现，连晴前，高原东侧纬向气流较弱，北支气流向南扩展，使高原东侧的流场变成连晴时的经向型；连阴雨前，高原东侧有较强的纬向气流，南支气流向北扩展，是造成连阴雨时两支气流相向运动较强的主要原因。
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Features of Two Flows Prior to Sustained Fine Periods or Overcast-with-rainy Periods |
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| Institution: | (Academy of Meteorological Science, SMA) |
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| Abstract: | Based on the data about 10 cases of sustained fine periods and 7 cases of sustained overcast-with-rainy periods in spring time 1980—1986 in the middle and lower reaches of Changjiang River, the features are analysed of 700 hPa streamline fields and of the two flows northeast and southeast of the Qinghai–Xizang Plateau. It is found that prior to sustained fine periods, the zonal flow east of the Plateau is weaker, and the north branch flow spreads southward, thus forming the meridional streamline field and initiating the sustained fine periods. Prior to sustained overcast-with-rainy periods, the zonal flow east of the plateau is stronger, and the south branch flow spreads northward. This is the reason why the stronger interfacing motion occurs between the two flows during the sustained overcast-with-rainy periods |
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