凝结潜热

大气凝结水汽汇、凝结潜热作用与积云对流参数化

Vapor sink and latent heat of condensation in the atmosphere and the parameterization of cumulus convection

B方案虽然考虑水汽凝结潜热，但计算方法没有考虑湿绝热线的曲率等问题，计算结果虽优于A方案，但误差仍较大；

Although Scheme B considers the condensation latent heat , the curvature of wet adiabat is not considered in the computational method . Scheme B is superior to Scheme A , but the errors are still large .

模拟结果表明，凝结潜热释放能使高层负涡度和低层正涡度强烈发展，形成地面至500hPa深厚的正涡度柱；

The results indicate that the condensation latent heat releasing can cause negative vorticity in upper level and positive vorticity in lower to develop intensely and then form profoundly positive vorticity columniations from ground to 500 hPa in high ;

对流凝结潜热激发飑线的数值试验

A numerical experiment of squall-line formation with convective condensation heating

凝结潜热加热对台风降水分布的影响

The effect of condensation heating on the distribution of the precipitation of Typhoon

在非绝热加热中，大尺度和对流性凝结潜热的释放对气旋的发展都是重要的。

Both large scale and convective condensation heating are important for development of cyclones .

凝结潜热对大气湍流影响的理论研究

The influence that condensation latent heat exerts on the atmospheric turbulence and its theoretical study

1998年夏季西太副高活动与凝结潜热加热的关系

Relationship between Activity of West Pacific Subtropical High and Condensation Latent Heating in Summer of 1998

A方案没有考虑水汽凝结潜热，计算结果误差大；

Scheme A does not consider water vapor latent heat , resulting in large calculation errors .

03.7江苏大暴雨凝结潜热的数值模拟

Numerical Simulation of Impact of the Condensation Latent Heat on " 03.7 " Rainstorm in Jiangsu Province

南方气旋发展的主要因子为中层槽脊系统及凝结潜热加热；

The main factor of southern cyclone is latent heat release and middle level trough and ridge systems .

物理过程的试验表明，凝结潜热释放在中尺度天气系统的形成过程中起了决定性作用。

Sensitive tests show that latent heat release acts a decisive role in the formation of the meso-scale systems .

充足的湿有效能量和凝结潜热的释放为本次大降水过程提供了物质条件。

The sufficient moist available potential energy and latent heat release offer the material condition for this heavy rain event .

台风凤凰形成发展过程中对流凝结潜热和感热的作用

Effects of Sensible Heat and Convective Condensation Latent Heat on Typhoon Fung-Wong During the Course of Its Formation and Development

亚洲季风区感热凝结潜热对副高带季节演变的影响

Effects of sensible heating flux and latent heating on seasonal evolution of the subtropical high belt over Asia monsoon region

进行三组敏感性试验，研究凝结潜热释放，蒸发冷却与地表热通量对气旋结构与强度的影响。

Three additional sensitive experiments are carried out to investigate the effect of condensation latent heating , evaporation cooling and surface heat flux .

利用模式结果，讨论了凝结潜热释放和行星边界层过程在低涡切变线维持中的作用以及云贵高原在低涡发生发展过程中的作用。

The function of the latent heat release , PBL process and terrain of the Yunnan-Guizhou Plateau is discussed according to the model results .

试验表明对流凝结潜热的释放至少对某一类飑线的生成具有重要作用。

The result shows that latent heat released by cumulus convection plays an important role in the formation of a certain kind of squall-line .

云的发展与良好的热力动力条件互相作用、共同加强，由南风带来的充足的水汽和热量为其发展提供前提条件，凝结潜热使上升运动向更高处伸展。

Heat and vapor transported by the south jet stream were the premise of this rainfall , and latent heat made vertical motion stretched higher .

高原效应的综合影响方面：地形抬升对地面感热通量的影响较小，对凝结潜热的影响明显。

For the integrated effects , the raising of TP has little influence on the surface sensible heat flux , while it greatly affects condensation heating .

后续降水再通过凝结潜热释放形成新的扰动源。不同积云对流参数化方案还可引起扰动源能量传播方式不同，最终使模拟大气的动力和热力结构有差异。

New precipitations become the new source of latent heat and temperature perturbation , which finally makes the dynamic and thermodynamic structures different in the simulations .

夏季孟加拉湾地区的深对流凝结潜热释放远大于长波辐的冷却作用，因而整个对流层几乎都保持较强的非绝热加热。

Over the Bay of Bengal , summertime latent heat release associated with deep convection exceeds longwave radiative cooling , resulting in intense heating in almost the whole troposphere .

发现非绝热因子（辐射、积云对流、大尺度凝结潜热）只影响高原低涡的强度，其中辐射加热对高原低涡强度影响最大。为高原低涡暴雨预报的气候背景提供了科学依据。

, only influence the intensity of the plateau vortex . All this had offered a scientific background for the prediction of the Plateau vortex which lead to the storm rainfall .

一方面是释放凝结潜热，引起热成风调整，产生更有利于扰动发展的环境场，这是一个正反馈过程。

One is releasing latent heat that causes adjustment of thermal wind , it formes environmental field which is favourable for development of disturbances . This is a positive feedback process .

采用广州有限区域数值预报模式，以登陆台风“黄蜂”（0214号）为例，研究海南岛屿地形和对流凝结潜热对登陆台风“黄蜂”的影响。

Taking landfall typhoon Vongfong ( 0214 ) as an example , the effects of Hainan island topography and convective condensation heating are studied by using Guangzhou limited-area numerical forecast model .

发现凝结潜热加热对台风的结构和降水起很重要的作用，是影响台风降水的最重要的物理过程，由此引起的垂直运动基本上决定了整个垂直运动场的分布，与实际降水分布配合甚好。

It is found that the condensation heating has significant effect on the structure and distribution of the precipitation of typhoon and is the most important one of the physical processes which influence the precipitation .

根据此增加量的大小，按比例地在中尺度模式中人为增加冰晶和雪晶含量，并计算凝结潜热的释放所造成的温度改变，能使相应位置的累积降水量有所增加。

Artificially enhancing of ice and snow crystal ratio in the meso-scale model and calculating the change of temperature cause by the release of condensation latent heat make the cumulative precipitation in the corresponding regions increased .

本文利用一包含湿过程的简单热带大气滤波模式，通过引入辐合反馈机制和下垫面的蒸发效应对凝结潜热释放的贡献的物理过程。

A simple moist and filtered model for the tropical atmosphere was constructed , incorporated with a convergence feedback mechanism and a physical process of evaporation from the lower boundary contributed to the latent release due to condensation .

夏季风爆发前期，南海季风区的增温主要由暖平流及非绝热加热过程（主要为凝结潜热）共同作用所致。

During the pre-onset period , the warming over the SCS monsoon region is mainly due to the warm horizontal advection and diabatic heating ( latent heat ) processes , meanwhile the warming is suppressed by the vertical adiabatic process ( cooling ) .

利用1998年南海季风试验逐日再分析资料，分析了1998年夏季梅雨期内凝结潜热加热对西太平洋副热带高压（下称西太副高）中短期活动的影响。

By means of daily reanalysis data of the South China Sea Monsoon Experiment in 1998 , the influence of condensation latent heating on mid - and short-term activities of West Pacific Subtropical High ( WPSH ) during Meiyu period 1998 is studied .