rainband

With thickness increasement of water vapor, the intensity, location of precipitation core and distribution of rainband came close to controlled test'.

所以，随着水汽的厚度增加，降水中心强度、位置、雨带分布与控制试验越接近。

It is shown that the energy dispersion of gravity inertial waves forced by one meso-scale rainband is probably a mechanism in the generation and the maintenance of another meso-scale rainband;

研究发现，由一条中尺度雨带强迫产生的重力惯性波的能量频散可能成为另一条中尺度雨带生成和维持的机制；

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.

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。

What is the impact on wind speed when the rainband of a tropical cyclone moves across?

当热带气旋的雨带经过时，对风速有甚么影响？

Analysis of Rainband Anomaly in the Southern China in June 2005

2005年6月我国南方雨带异常偏南的分析

The results show that drawing the isoline of standardized rainfall index of 1.5 that is better indicative of the meridional shifting of the summer rainband in eastern China, and its phased and abrupt change in its northward march.

结果表明：标准降水指数为1.5的等值线较好反映了中国东部夏季雨带的南北移动，以及雨带推进过程中呈现的阶段性与突变性特征。

On the causes of rainband breaking and asymmetric precipitation in typhoon haitang ( 2005) before and after its landfall

台风登陆前后雨带断裂与非对称降水的成因分析

When rainstorms happen in the rainband of East Asian subtropical monsoon on the STH north side, the downdrafts are distinct around the ridge at a related meridian.

在副高北侧东亚副热带季风雨带上有暴雨发生时，其凝结海热激发的经圈环流对相应经度上的副高脊线附近的下沉气流有显著贡献。

Mesoscale rainband activities and the distribution characteris-tics of the weather elements in the vicinity during the Meiyu periodare examined based on exhaustive data.

本文用详尽的资料分析了梅雨期中尺度雨带的活动及其周围气象要素的分布特征。

Seasonal coupling features between the East Asian summer monsoon rainband and West Pacific subtropical high

东亚夏季风雨带和西太平洋副高季节变化的耦合特征

There existed the characteristics of short period and less rainfall during the Meiyu in 2005, which made the main rainband occur in the Jiangnan area and South China.

2005年7月5日入梅，7月14日出梅，入梅晚，梅雨期短，梅雨量少，致使我国主要雨带位置不是如常年一样维持在江淮流域，而是在江南地区南部和华南地区。