雨带

由于降水性质的不同，两次过程中雨带的形状和移动各有特点。

Because of the different nature of precipitations , rain band shape of two process were different too .

结果表明：①该数值预报系统对三峡库区主雨带的位置有较好的预报；

The results show that : ① The system can predict the position of the main rain band of Three Gorges reservoir area very good .

源涡位于32°35°N之间时，夏季雨带多出现在淮河流域（Ⅱ类雨型）；

Between 32 ° N and 35 ° N longitude , the belt is appeared in Huaihe River basin ( second pattern - ⅱ);

我国西部（85°105°E）冬季扰动源涡的位置对夏季东部雨带的配置具有支配作用。

In summer , the distribution of rain belt over East was controlled by the last winter position of Disturb source vortex over West China , during 85 ° E to 105 ° E latitude .

通过对一次暴雨个例的比较研究表明，在雨带形势和暴雨中心位置的动力识别方面，改进的Q矢量分析方法比传统的单纯依靠Q矢量散度分析方法具有更好的效果。

Through a case study of a torrential rain event , potential advantages of the improved Q analyses approach can be seen in dynamic identification of both the location and the po .

热带气旋活动对中国夏季雨带类型与ENSO的响应关系

Interrelation between the Tropical Cyclon action and the types of the rain band in summer in China as well as the action of ENSO

涡旋Rossby波说和重力惯性波说仍然是螺旋雨带形成理论的两种不同观点；

Vortex Rossby waves theory and inertia-gravity waves theory are the two main different viewpoints about the formation of spiral rain bands ;

分析了各类型所对应的500hPa环流背景和太平洋海温场分布特点，进而探讨了导致各类雨带分布可能的物理机制。

Furthermore , the possible cause of every precipitation distribution is studied .

细网格域内前36h的降水分布和雨强与观测的大体相应，扩展域细网格的降水模拟明显改进了原细网格的模拟，特别是雨带。

The rainfall distribution and intensity before 36 h in the fine domain were roughly correspondent with observations , the simulated precipitation as mentioned above is obviously improved by the simulation of the extended fine domain , especially rainfall belt .

结果表明：AMSU资料作为一种新的卫星微波探测资料，在热带气旋的结构、螺旋雨带的强度及其降水强度的分析预报中具有一定的应用价值。

As a result , as a new kind of satellite soundings , AMSU microwave data are of some utility in analyzing and forecasting the structure of tropical cyclones , and intensity of a spiral rainband and rainfall .

利用包含冰相微物理过程参数化方案的三维非静力中尺度/云模式（ARPS）模拟了与冷锋有关的冷锋雨带（NCFR）结构，着重分析了锋面云系发展演变的主要特征。

Three-dimensional simulation of cold-front rain-band ( NC'FR ) associated with a straight cold front has been studied by use of a non-hydrostatic , full compressible storm-scale model ( ARPS ) including multi-phase microphysical parameterization .

研究9012号台风（YANCY）中尺度螺旋雨带结构特征及其与闽东北沿海地区特大暴雨的关系。

This paper is to analyse the structure of the mesoscale rotational rain belt of Typhoon 9012 ( YANCY ) and its relationship with the heavy rainfall in north east of Fujian .

中国东部夏季雨带类型与前期北半球500hPa环流异常的关系7月份两种东亚阻塞形势对中国主要雨带位置的不同影响

Relationship between Summer Rainbelt Patterns in the Eastern China and 500 hPa Circulation Anomalies over the Northern Hemisphere DIFFERENT INFLUENCE OF TWO EAST ASIAN BLOCKING SITUATIONS IN JULY ON RAIN BELT LOCATION IN CHINA

采用非静力中尺度数值模式（MM5）对这次大暴雨过程进行初步模拟试验，结果表明模式对这次强降水的雨带分布、暴雨中心强度及其位置的模拟也与实况较为接近。

The preliminary simulation test was carried by means of the non-static medium-scale numerical forecast model ( MM5 ), the result indicated that the simulation for this rainstorm belt distribution , the rainstorm center intensity and its position also approached with the real situation .

根据1951～1986年的资料，在文献〔1〕对中国东部夏季（6～8月）雨带分布类型的基础上，分析了各雨型与前期北半球500hPa环流异常的关系。

In this paper , on the basis of the classification of summer rainbelt distribution in the eastern China , we using 1951-1986 monthly 500 hPa height data over the Northern Hemisphere analyze the relationship of summer rainbelt patterns with 500 hPa circulation anomalies of the previous stage .

2005年6月我国南方雨带异常偏南的分析

Analysis of Rainband Anomaly in the Southern China in June 2005

梅雨锋暴雨中尺度雨带特征剖析

Analysis of the characteristics of the Meiyu front mesoscale rain band

梅雨期中尺度强雨带的若干特征

Some characteristics of the meso-scale intense rain-band in the Mei-yu season

我国东南象限冬、春季雨带的相关分析

Analyses on Correlation between Rain Belts in Winter and Spring

中国东部夏季雨带推进过程的年际、年代际变化

Interannual and Interdecadal Changes of Summer Rain Band Propagation over Eastern China

一次连续性暴雨中双雨带的成因分析

Research on the causes of double rain belts during a sustained rainstorm

世界大洋中的锋面我国雨带的季节变化

Fronts in the world oceans seasonal variation of the RAIN-BELTS in China

我国东部夏季雨带类型的划分及预报

The classification and forecasting of summer rain-belt in the east part of China

一条中尺度雨带的多普勒雷达回波特征及环境条件分析

Doppler radar echo feature and environmental condition analysis of a mesoscale rain belt

梅雨锋中尺度切变线雨带的动力结构分析

The dynamical structure of a mesoscale shear - line rain belt on Meiyu-front

中国夏季主雨带的形成过程

The formation of main rain-band in Summer in China

我国雨带的季节变化

Seasonal variation of the RAIN-BELTS in China change

500年来中国东部雨带的南北摆动

North-South migration of rain belt over the eastern China in the past 500 years

水汽厚度变化试验表明，水汽厚度的变化会导致降水的强度及雨带的分布发生变化。

Different thickness of water vapor may cause strength and distribution of precipitation change .

东亚季风和季风槽雨带影响副热带高压进退活动的机理分析

A Mechanism Analyses of East-Asia Monsoon and its Rainfall Influencing West-Pacific Subtropical High Activity