| 2001-2010年辽宁区域性暴雨阶段性特征 |
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| 引用本文： | 公颖,陈力强,隋明.2001-2010年辽宁区域性暴雨阶段性特征[J].辽宁气象,2011(6):14-19. |
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| 作者姓名： | 公颖 陈力强 隋明 |
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| 作者单位： | [1]中国气象局沈阳大气环境研究所,辽宁沈阳110016 [2]抚顺市气象局,辽宁抚顺113006 |
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| 基金项目： | 公益性（气象）行业科研专项（GYHY200906011）资助. |
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| 摘 要： | 利用辽宁自动气象站逐小时降水资料和1。X1。NCEP资料，对200l-2010年汛期共25次辽宁暴雨过程进行分析，以期得到暴雨过程时间分布特征和典型影响系统。结果表明：25次辽宁暴雨过程中有7次为阶段性暴雨即两段持续性暴雨过程中间有明显的降水减弱与天气系统转换，占总数的28％；辽宁暴雨过程高层（以200hPa为代表）主要影响系统为高空急漉，中层（以500hPa为代表）主要影响系统92％为高空槽（其中57％为高空槽与副热带高压共同影响），低层（以850hPa为代表）诱发系统88％为气旋（或倒槽）顶部（或东部）切变线、12％为鞍形场切变。阶段性暴雨过程两阶段的高中层影响系统基本一致，高层影响系统均为高空急流，中层多为副热带高压和高空槽的共同影响、少数仅受高空槽影响，在低层，阶段性暴雨过程均伴随着低层要素场（特别是风场）的调整，导致低层天气系统的转换或强度的变化，低层要素场的调整阶段即为阶段性强降水的间歇期；阶段性暴雨过程在天气系统的配置及时段长度方面无明显特征，即在暴雨过程发生初期，从这两方面均无法判断该暴雨过程是否将发展为阶段性暴雨。25次辽宁暴雨过程中，丹东本溪地区17次降水有陡增现象，这与丹东、本溪地区处于长白山东南部和丹东地区东南侧临海有密切关系。
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| 关 键 词： | 暴雨 阶段性特征 影响系统 |
Temporal distribution character of regional heavy rain from 2001 to 2010 in Liaoning province |
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| GONG Ying,CHEN Liqiang,SUI Ming.Temporal distribution character of regional heavy rain from 2001 to 2010 in Liaoning province[J].Liaoning Meteorological Quarterly,2011(6):14-19. |
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| Authors: | GONG Ying CHEN Liqiang SUI Ming |
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| Institution: | 1. Institute of Atmospheric Environment, China Meteorological Administration, Shenyang 110016, China; 2. Fushun Meteorological Service, Fushun 113006, China) |
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| Abstract: | Based on the hourly precipitation data from automatic weather stations in Liaoning province and the NCEP data （1 o x 1 o resolution）, the 25 heavy rain events in the flood seasons from 2001 to 2010 were analyzed in order to obtain the temporal distribution characteristics and typical weather systems of the heavy rain events. The results show that among the 25 heavy rain events ,7 events （28 % ） have two main rain phases, i. e. there are obviously decreasing precipitation and transformation of weather system between two rain phases. The upper air jet stream is the main weather system at high level （200 hPa） during the heavy rain process. 92% of main weather systems are upper trough at middle level （in 500 hPa）. Among 92% ,the common influence of upper trough and subtropical high accounts for 57%. 88% of inducing systems is a shear line of the top （ or eastern） of cyclone （ or inversion trough） at low level （in 800 hPa）, and 12 % is a shear of saddle field. In general, the weather systems of heavy rain events with two rain phases at high and middle levels do not change in the two stages. The main weather systems are upper jet stream at high level and the common influence of upper trough and subtropical high at middle level （ a few of them are only influenced by upper trough）. The heavy rain processes with two rain phases are accompanied with the adjustment of the elements fields at low level, especially the adjustment of wind field, which results in the transformation of weather systems at low level or the change of intensity. The adjustment stage of the elements fields at low level is also the interval period of two rain phases. The collocation of weather system and duration of the heavy rain process do not have obvious characteristics for the heavy rain events with two rain phases. That is to say, the heavy rain events in their early period could not be identified whether they could develop into two or more rain phases. 17 events in Dandong and Benxi have the phenomena of abruptly increasing precipi- tation among 25 heavy rain events, which is related to the location of two cities, namely, Benxi is located in the southeastern Changbai Mountain and the southeast of Dandong is close to the sea. |
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| Keywords: | Heavy rain Temporal distribution character Influencing system |
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