暖区

台湾锋前暖区一次积云对流过程

On a cumulus convection process in the pre frontal warm sector over Taiwan area

华南暖区暴雨中尺度对流系统的分析

Analysis of mesoscale convective systems associated with a warm sector heavy rainfall event over South China

500hPa螺旋度正值区长轴与造成强对流的暖区弱切变和雷达带状回波走向一致；

The long axis in positive value area of 500 hPa helicity is consistent with the causing severe convective warm area ′ s weak shear and moving towards of radar band echo ;

中、高层是一中尺度暖区。

But at mid-and-high level , there was a warm region .

湖南冬季暖区的研究

Research into winter warm region in Hunan Province

广西前汛期锋前暖区暴雨过程的模拟与分析

Numerical Simulation and Analysis on a Heavy Rain Process in the Warm Sector in Guangxi

华南暖区一次暴雨中尺度系统的数值模拟

Numerical Simulation of Mesoscale System of a Rain Storm in Warm Section of Southern China

二是暖区划分依据与指标。

The second is the reason and indexes for the division of winter warm region .

暖区区域性大暴雨中尺度系统发生发展的研究

A study on the occurrence and development of extremely heavy rain mesoscale system in warm region

三维中－β尺度模式研究：一次气旋暖区锋生活动的中尺度结构的数值模拟试验

A study of meso - β scale model : the experimental simulation of the meso-scale structures generating in Frontogenesis

这是一类华南前汛期锋前暖区暴雨。

There were the heavy rainfalls happening in warm sector ahead of the front in South China during the pre-rainy season .

华南前汛期锋面对流系统与暖区对流系统的个例分析与对比研究但前锋在禁区内犯规了。

A comparative study of a frontal and a non-frontal convective systems But the forward made a foul in the penalty area .

因此，利用数值模拟对此进行了验证，使用CAM3.0的数值试验的结果揭示出，暖区海温的升高会引起中纬度西风急流和低纬度东风的变化。

The numerical results revealed that the increase of SST would cause the changes of the mid-latitude jet stream and low-latitude westerly wind .

一类华南锋前暖区暴雨β中尺度系统环境特征的分析研究

A Study of Circumstances of Meso - β - Scale Systems of Strong Heavy Rainfall in Warm Sector Ahead of Fronts in South China

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 .

分析还发现，台风有沿着对流层深层暖区轴线，按照热成风方向移动的趋势。

The analysis further indicates that typhoons tend to move along the axis line of warm area of deep tropospheric layer in the direction of the thermal wind .

当增大寒潮过境前低层暖区气温，导致寒潮强度增强，区域整体风场的响应强度增大。

When increasing the temperature in low-layer warm area of the cold wave front , the strength of cold wave is increased , the wind strength increased overall wind field .

西太平洋副热带高压强大而稳定、对流层中层存在暖区是该台风路径稳定、移动迅速的主要原因；

The strong and stable west Pacific high pressure and the warm zones in the middle troposphere are the major causes of the stable track and quick movement of the typhoon .

暖区有明显的强降水中心，雨强极大值出现在山区迎风坡，降水雨滴谱谱宽较大，有时滴谱呈双峰型分布；

Heavy rainfall occurred in the warm area , and maximum rainfall lay in the windward slope where the width of raindrop size distribution was broadened and sometimes it was bimodal spectrum .

商丘市的大雾多形成在大陆高压型、冷锋前暖区型、均压场型、（低压）倒槽型天气形势中。

The heavy fogs of Shangqiu are formed by the weather situations : continental anticyclone , warm zone in front of cold front , uniform pressure field , and low pressure with an inverted trough .

雨滴平均直径的起伏暖区要大于冷区，这与暖区中云系结构不均匀及云中对流有关。

The fluctuations of the average diameter of raindrops in the warm sector are larger than those in the cold sector , which is related to the inhomogeneity of the cloud system structure and convection in the cloud .

在西南低空急流十分潮湿的情况下，中尺度对流系统可以在江淮气旋暖区、低空急流大风速中心的前部、位势稳定度倾向维持负值的地区生成和发展。

When the low-level south-west jet stream is very moist , mesoscale convective systems can develop ahead of the wind speed maximum , in the warm sector of Changjiang-Huaihe-River cyclone where the potential stability tends to remain negative .

春、夏季的北迁，迁出地一般位于地面热低压系统的暖区和高空850毫巴图上的偏南气流，特别是西南气流的控制区域；

The emigratory areas in the northward migrating process in spring-summer are located in the warm sector of warm low on surface and in partial southern air stream on 850 mb isobaric chart , especially in the region controlled by SW air stream .

我省暖区共116个（包括片、区、块）占全省土地面积27.02%，其中一级暖区为3.41%、二级暖区6.83%、三级暖区10.07%、四级暖区6.71%。

They occupy 2 (?) . 62 percent of the whole provincial land , of which the first grade winter warm region is 3.41 % , the second , 6.83 % , the third , 10.07 % and the fourth , 6.71 % .

通过对降水云系的综合研究，建立了河南省春季层状云降水概念模型：暖区降水主要通过云水碰并形成，冷区降水机制以冰粒子融化等冷云过程为主；

Through synthetic analysis of stratus cloud systems , stratus precipitation concept model has been primarily established . It was well known that the main process of precipitation formation was collecting cloud water in the warm area and ice phase particles melting in the cold area .

在层状云降水过程中，暖区雨滴谱型由宽谱双峰型演变为窄谱单峰型，冷区雨滴谱型由宽谱单峰型演变为窄谱单峰型。

During the process of stratiformis precipitation , the raindrop spectra in the warm sector evolves from a wide spectra double-peak pattern to a narrow spectra single-peak one , while the raindrop spectra in the cold sector changes from a wide spectra single-peak pattern to a narrow spectra single-peak one .

西太平洋暖池区SST的变化，与南印度洋西风漂流区、赤道北印度洋存在显著的正相关。

It is also found that the variation of WEWP SST is positively correlated with the equatorial northern Indian Ocean and the west wind drift of the southern Indian Ocean .

本文通过对夏季热带西太平洋暖池区SSTA的EOF分析，发现夏季暖池区海温存在两种主要空间分布型，即SSTA的一致性分布和南北半球反对称分布。

Based on the SST data , the temporal and spatial variations of SSTA in Western Pacific Warm Pool region have been analyzed in this paper by means of EOF .

研究表明，西太平洋暖池区的垂向温度存在显著的年际变化，尤其在次表层（120～200m）的变化最为明显。

The research results show that the annual change of the vertical distribution of the ocean temperature in the West Pacific warm pool region is notable and particularly that in subsurface layers ( 120 ~ 200 m ) is most obvious .

赤道太平洋暖池区的异常热源性质，强度和位置是决定中国夏季降水准两年模态的主要因素，而该异常热源的特征与太平洋-亚澳季风系统TBO的强度和状态等密切相关。

Moreover , the character , intensity and location of the anomalous heating resource of the warm pool in the tropical Pacific are key factors controlling the major mode of the TBO of summer rainfalls in China .