对流单体

非均匀粘性基流中带状浅对流单体的发展

The Development of the Shallow Band Convection Cell in Nonuniform Viscous Basic Flow

另外，在组成强对流系统的最小单元&对流单体中，存在着动力场、微观场和电活动。

In addition , the severe convective system is composed of convection cell , in which existing the dynamic field , the microscopic field and the electric field having interaction between each other , respectively .

强降水与深对流云团及雷达回波强度强、回波顶高、VIL大的强对流单体有密切的关系。

Heavy rain is close connected with the deep convective cloud clusters and convective cells with the strong radar reflectivity , high echo top and big VIL .

三是井冈山区对流单体在初始阶段的移向移速与700hPa风向风速对应较好；

At third , the direction and speed of convective storm cloud is near to the wind in 700 hPa ;

春季一次典型强对流单体降雹雷达产品特征分析

A typical spring came Hail Radar Products Show monomer feature analysis

关于影响超级对流单体形成因素的数值试验

The numerical experiments about the effects of several factors on the formation of supercell airflow pattern

四是罗霄山脉中部的低空平均径向速度入流区的演变，与井冈山局部对流单体关系密切；

At fourth , convection development over Jinggang mountain is interrelated with the low-level inbound mean radial velocity on the middle of Luoxiao mountain ;

中-β尺度对流单体造成局地特大暴雨分析&以02-07-04子长特大暴雨为例

Analysis of Local Extra-heavy Rainstorm by Meso - β Scale Convective Monomer & Take the example of Zichang extra-heavy rainstorm on July 4 , 2002

对流单体受到超折射污染时，零速度线所在区域多普勒通道可采用中等级抑制，监测通道可采用强等级杂波抑制。

The medium level suppression in the Doppler channel and high level suppression in the Surveillance channel can be invoked when convective precipitation cells are contaminated .

暴雨云团表现为多单体特征，发展旺盛期对流单体的数量明显增加、云团尺度大幅增加。

Convective cloud clusters of the rainstorm were characterized by coexistence of multiple convective cells with their numbers and sizes increased greatly for the fully developing cloud clusters .

从对流单体降落的冷凝物的水平宽度比观测到的做尺度下沉气流的宽度小得多（前者60公里而后者150公里）。

The horizontal width of the condensate falling from the convective cells was much less than the width of the observed mesoscale downdraft ( 60 km compared to150 km ) .

对流单体主要在海拔较高的山脊处生成，并向低海拔地区移动传播，传播的速度和方向主要与地形和中高层风速风向有关。

Convective cells formed at high altitude plots firstly and then spread to lower altitude area , and the speed and directions of cells'spread depend on terrain factors and upper level wind .

断层只在一定岩石圈厚度范围内对强震震中的位置起控制作用。由于软流层的物质活动与相邻板块活动的历史有关以及对流单体活动区随时间的变化，因此地震活动也将发生变化。

It is suggested that active regions of strong earthquakes M ≥ 6 are under the control of lithosphere thickness : the fault only occurred at the some thickness of lithosphere controls the position of epicentre .

锋面系统抬升了中-β涡旋北部的东南暖湿气流，形成垂直上升运动，并形成雷暴云团，同时激发出新的对流单体；

The front lifts the southeasterly warm moist inflow of the meso β vortex , generating the vertical motion upward and the storm cloud in the meso β vortex , and arousing a new convective cell ;

本文介绍了风暴天气的天气学征，对流单体的一般特征及其发展的环境条件，强对流风暴天气的雷达回波特征，从而概述了风暴识别算法的天气学依据；

The paper introduces the meteorological feather of storms , the general feather and development environment condition of convective cell , radar echo character of the severe storm weather , point out the evidence of storm serial algorithm .

这种有利于对流单体从系统的左后方新生，在右前方消亡的配置可能是导致沙兰河上游暴雨的雷暴云具有左移风暴特点的重要动力机制。

This configuration of upper and lower level air flows is favorable for convective cells spawning at the left rear and decaying at the right front of the MCS , which might act as a key dynamic mechanism for the left-moving rainstorm .

2009年广州第一场强对流天气的强对流单体雷达特征

Radar Feature Analysis on the First Convective Event of 2009 in Guangzhou