静止锋

在弱流场型（R）下，其前一天天气形势是中低层有足够水汽输入条件或存在中尺度低值系统，对应地面存在静止锋或为均压场。

While in the case of Pattern R , there exists sufficient inflow of water vapor or a mesoscale low-pressure system in the lower and middle troposphere , associated with a stationary front or homogeneous distribution of sea surface level pressure .

条件性对称不稳定与昆明准静止锋风雹南岭静止锋上的对称不稳定性

Conditional symmetric instability and high-wind and hail accompanying with Kunming quasi - stationary front

梅雨静止锋积云群整体属性的诊断研究

Diagnostic Study of Bulk Properties of the Cumulus Ensembles inside Meiyu Quasi-stationary Front

静止锋附近中尺度流场运动学特征

The Mesoscale Characteristics of Kinematics of a Wind Field near the Stationary Front

昆明静止锋下的云南强倒春寒天气分析

Analysis of Yunnan Severe Coldness in the Late Spring under Kunming Quasi-stationary Front Weather

主要影响系统来自低层切变线、高空低槽和地面静止锋；

The major systems come from the shear line of low-layer , the low trough of upper air and the ground stationary front .

稻飞虱迁入期，该区稳定维持静止锋及低涡切交系统，持续阴雨，有利于虫源的迁入和降落；

3 ) weather that during the period of the planthopper immigration ( from April to September ) is usually characteristic by maintained stationary front .

中国淮河以南地区夏季最易受到洪水灾害的威胁，这种致洪暴雨一般出现在沿着河谷走向的静止锋上。

During summer the southern part of China to the south of the Huaihe River is vulnerable to the threat of the heavy rainfall causing flood damages .

介绍了一次华南准静止锋暖区内降水的物理化学特征的综合观测分析结果。

The results are presented of a comprehensive observational analysis of physical and chemical characteristics of precipitation within the warm sector of a quasi-stationary front in South China .

造成6月华南地区强降雨的影响天气系统为切变线和地面静止锋，主要为从东北和西北来的冷空气与暖湿气流交汇于华南地区而形成。

The severe heavy rainfall over South China was caused by the shear line at lower troposphere and stationary front at surface , which was associated with the convergence of cold air from northwestern and northeastern China and warm-wet air from South China Sea .

利用安装在南京气象学院的天气多普勒雷达收集到的雷达资料，分析了在江淮流域大暴雨后期静止锋附近风场的中尺度结构特征。

In this paper , the characteristics of mesoscale structures of wind fields near the stationary front in the late period of a heavy rain in the Jiang - Huai area are analysed based on the wind data of doppler radar located in the Nanjing Institute of meteorology .

运动缓慢近于静止的阵风锋则常出现在风暴的减弱阶段，它的出现加速了风暴的消亡。

The other is the gust front moved slowly ( static gust fronts ) which is often occurred at the weakening stage of the relevant storm , the occurrence of it speeds up the end of the storm .