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气象:2008,34(8):58-62
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东营市暴雨气候特征
(1.山东省气象科学研究所,济南 250000;2.山东省东营市气象局)
Analysis on Climatic Character of Rainstorm in Dongying, Shandong
(1.Meteorology Research Institute of Shandong Province,Jinan 250000;2.Dongying Meteorological Office, Shandong)
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投稿时间:2008-02-19    修订日期:2008-04-17
中文摘要: 利用1971—2004年东营市5个气象站近34年的日降水量资料,采用Petitt方法和合成分析等 方法,研究了东营市暴雨的气候特征,及产生这种特征的原因。研究表明:自1970年代以来 ,东营市暴雨的年代际变化呈现出3个特征时段:1974/1975年发生突变,突 变前暴雨年出现站次基本呈上升趋势,突变后明显减少;1990年成为二级变点,之后暴雨年 出现站次又有明显增多。1990年代后东营市暴雨明显偏多是在有利的高空环流背景下,北方 冷空气和南方暖湿气流频繁交汇的结果。由于东营市特殊的地理位置和地形、地貌影响,导 致东营市降水的气候特征与山东省的气候特征变化并不一致,前者呈现出两头高、中间低的 倒抛物线形状,而后者却一直呈现出下降趋势。
中文关键词: 暴雨  气候特征  Petitt方法
Abstract:Based on daily precipitation data of five weather stations of Dongying City from 1971 to 2004, the characteristic of rainstorm change and the produce reasons in this region are studied by using Petitt method and composite analysis. The resu lts show that the inter decadal variation of Dongying rainstorm has pr esented 3 characteristic time intervals since the 1970s. The abrupt change of ra instorm happens in 1974/1975. The rainstorm has a trend of escalation before abr uption, and it quickly reduced after abruption. 1990 was the second level chang e point, afterward the rainstorm frequency obviously increased. Increase in Dong ying rainstorm after 1990's is attributable to the advantageous upper air circul ation background, frequent interaction between the north cold air and south warm and humid air streams. As a result of the Dongying special geographical positio n, the terrain and landform influence cause the Dongying precipitation's climate characteristics being inconsistent with that of Shandong Province. The former c hange is counter parabola shape, but in the whole province it appears to be consistently decreas ing tendency.
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郑丽娜,靳军,李建明,2008.东营市暴雨气候特征[J].气象,34(8):58-62.
Zheng Lina,Jin Jun,Li Jianming,2008.Analysis on Climatic Character of Rainstorm in Dongying, Shandong [J].Meteor Mon,34(8):58-62.