热带低压

OLR低值中心存在于辐合带中热带低压易发展；

Tropical depression would easily develop into tropical storm when OLR low center embedded in ITCZ .

研究结果表明：南海热带低压能否发展加强成热带风暴与南海区及其附近OLR值的变化有较好的对应关系；

The results show that there is a good relationship between the development of South China Sea tropical depression and the OLR variation over the South China Sea .

通过定义一个南海热带低压的发展指数IOD（IndexofDevelopment）来定量描述OLR等值线的梯度变化和南海热带低压发展的关系；

IOD ( Index of development ) was defined to describe the relationship between the variation of OLR and the development of South China Sea tropical depression quantitatively .

积云摩擦效应和ITCZ&热带低压的诊断分析

Cumulus friction effects and diagnostic analysis of ITCZ - tropical low

热带低压环流引发的中尺度特大暴雨过程分析

Analysis of a mesoscale torrential rainstorm triggered by the tropical depression system

东海热带低压发展的预报模式

Forecasting method of tropical depression development over East China Sea

越赤道气流对台风、热带低压天气系统的影响

The Influence of Crossing-Equatorial Flaw on Typhoon and Tropical depression Weather System

热带低压欧内斯特继续变弱，但是它仍然存在威胁。

Tropical depression Ernesto continues to weaken but it 's still a threat .

上海热带低压特大暴雨分析

Analysis of tropical depression rainstorm in Shanghai

热带低压远外围强对流天气的动力机制

Dynamic Mechanism Analysis on an Severe Convection in The Outer Periphery of A Tropical Depression

热带低压台风的发生发展与其周围流场垂直切变的关系

On relation between generation and development of tropic depression and vertical shear of ambient flow

上海0185热带低压特大暴雨过程触发机制研究

A research on the trigger of 0185 tropical depress rainstorm in Shanghai , eastern China

“黑格比”减弱为热带低压，离开该地区。

Hagupit has been downgraded to a tropical depression as it 's leaving the region .

热带低压、台风发生发展过程中的自激加热、耗散和非线性作用

Self-exciting heating dissipation and nonlinear action in the process of generation and development of Typhoon Depression

台风“桑美”已经降级为热带低压，目前正向江西省移动。

The Typhoon Saomai has been downgraded to a tropical depression and is moving into Jiangxi province .

热带低压没有风眼，也不像更强的风暴系统那样呈螺旋状。

It has no eye and does not typically have the spiral shape of more powerful storms .

北部湾热带低压发展成台风的结构演变和动能收支的诊断分析

An analysis of structure evolution and kinetic energy budget during a tropical depression intensification into a storm in the Beibu Bay

缩短热带低压电工产品湿热试验周期数的检验绝缘电阻误差分析

Error Analysis of Testing Insulation Resistance of Low-Voltage Electrical Products in Tropical Areas After Reducing the Number of Cycles in Damp-Heat Test

本文用非线性耗散理论研究第二类条件不稳定下的自激加热的热带低压、台风系统。

A highly truncated spectral model is used to study the self-exciting heating , dissipation and nonlinear action in the typhoon depression system .

在双台风状态下，两个低值中心的强弱情况和距离决定热带低压能否发展。

Under the state of binary typhoons , the development of South China Sea tropical depression depended on the strength and distances of two OLR low centers .

在东风气流中，低压中心位于15～20°N之间，低压中心位置跟实际热带东风气流中低压形成位置比较一致

In the easterly flow , the center position of depression appears between 15 ° N to 20 ° N. The center position of depression is relatively consistent with the position of depression formation in the observational tropical easterly flow . COMPARE

热带东风气流中低压形成的非线性过程

The Nonlinear Process of the Depression Formation in the Tropical Easterly Flow

热带气旋是在世界热带地区形成的低压区域。

A tropicalcycloneis an area of low pressure that forms in the tropical regions of the world .

根据强度的不同，热带气旋可以划分为三类：热带低压，热带风暴，以及更强的、在不同地区名字有所不同的一类风暴。

Tropical cyclones are classified into three main groups , based on intensity : tropical depressions , tropical storms , and a third group of more intense storms , whose name depends on the region .