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2001-2010年辽宁区域性暴雨阶段性特征

公颖 陈力强 隋明

气象与环境学报2011,Vol.27Issue(6):14-19,6.
气象与环境学报2011,Vol.27Issue(6):14-19,6.

2001-2010年辽宁区域性暴雨阶段性特征

Temporal distribution character of regional heavy rain from 2001 to 2010 in Liaoning province

公颖 1陈力强 1隋明2

作者信息

  • 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
  • 折叠

摘要

Abstract

Based on the hourly precipitation data from automatic weather stations in Liaoning province and the NCEP data (1° × 1° 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 precipitation 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.

关键词

暴雨/阶段性特征/影响系统

Key words

Heavy rain/Temporal distribution character/Influencing system

分类

天文与地球科学

引用本文复制引用

公颖,陈力强,隋明..2001-2010年辽宁区域性暴雨阶段性特征[J].气象与环境学报,2011,27(6):14-19,6.

基金项目

公益性(气象)行业科研专项(GYHY200906011)资助. (气象)

气象与环境学报

OACSTPCD

1673-503X

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