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warm rain process
相关语句
  暖雨过程
     (4)According to the analysis, cold rain process is much more important than warm rain process.
     (4)该地区暖雨过程不易启动,降水过程主要启动机制为冷雨过程。 雨滴谱观测资料分析结果显示,双峰谱型是该地区积雨云降水的主要谱型;
短句来源
     In contrast, the warm rain process is characterized by short life period, more pronounced rearward tilt structure and extension of stratiform cloud.
     相比之下,暖雨过程中飑线的生命周期缩短,而系统倾斜结构更明显,层状云区的发展比较旺盛。
短句来源
     What is more,the warm rain process can be useful to precipitation although cold rain process is the main precipitation mechanism over Qinghai-Xizang Plateau.
     分析发现,虽然高原地区冷雨过程是主要的降水机制,但是暖雨过程仍然对降水有贡献。
短句来源
     Rain water is produced first at low level through warm rain process during the initial stage of precipitation,and ice phase particles are very important to rain water during the mature stage.
     云发展初期降雨首先产生于低层,以暖雨过程为主,成熟期云中冰相粒子对降水非常重要。
短句来源
  “warm rain process”译为未确定词的双语例句
     The“seeder-feeder”mechanism,seeding by generating cells and warm rain process in shallow stratiformclouds have been demostrated.
     模拟得出了同实测比较一致的层状云“播种-供应”机制,高空发生胞的“播种”作用和暖层云中的降雨过程等。
短句来源
     The main purpose of this paper is to improve the warm rain process in the LASG-REM(State Key Laboratory of Numerical Model for Atmospheric Sciences and Geophysical-Regional ETA Model),via adding the explicit prediction of water vapor,cloud water and rainwater for mesh resolvable systems and the parameterization scheme for subgrid cumulus convective systems. The sounding data of Eurasian as well as the surface data at 0000Z 21st July 1998 are used as the initial fields in the simulation.
     改进中尺度动力预报模式中较为简单的云雨过程处理方案,用预报方程对大尺度(即网格尺度)的水汽、云水和雨水作显式求解,对次网格尺度的积云对流进行参数化处理,并以1998年7月21日00时(UTC)的欧亚探空资料和地面资料为初始场,对武汉地区的暴雨过程进行数值试验。
短句来源
  相似匹配句对
     Rain
     雨
短句来源
     ON THE CONDITIONS OF WARM RAIN FORMATION IN CUMULUS CLOUDS
     积云形成暖雨的条件
短句来源
     Yellow Rain.
     黄雨——八十年代国际上的一场重大争论
短句来源
     Cold and Warm
     第六层:冷暖世界
短句来源
     Warm diamond
     让钻石温暖起来
短句来源
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  warm rain process
Characteristic features of atmospheric aerosols over India and their role in warm rain process
      
Seeding of Cell 3 leads to very different results for Case II, with the warm rain process turned off.
      
In the warm rain process, raindrops develop by the collision and coalescence of cloud droplets.
      
In this study, a simple warm rain process is introduced into the WRF/MM5 3D-Var system.
      
Hygroscopic seeding seeks to increase the efficiency of the warm rain process.
      


An one-dimensional time-dependent model of precipitation in warm layer cloud is given. The influence of some factors on warm rain process and its initiation is tested. The process of rain enhancement by salt-seeding is simulated and discussed.

本文提出层状暖云降水的一维时变模式,用数值试验方法探讨了层状暖云降水的临界条件,各种物理参量对降水过程的作用以及播撒盐粉的增雨效果和最佳催化技术。

Our cloud model (paper Ⅰ)was run to calculate the microphysicalstructures of clouds and preci pitation associated with middle latitude cyclo-nes,by using the observed temperature and updraft as input.The resultsagree with observations in many aspects.The“seeder-feeder”mechanism,seeding by generating cells and warm rain process in shallow stratiformclouds have been demostrated.The two-parameter model and the equationsof ice nucleation,cloud-rain autoconversion and ice multiplication seem tobe reasonable,but...

Our cloud model (paper Ⅰ)was run to calculate the microphysicalstructures of clouds and preci pitation associated with middle latitude cyclo-nes,by using the observed temperature and updraft as input.The resultsagree with observations in many aspects.The“seeder-feeder”mechanism,seeding by generating cells and warm rain process in shallow stratiformclouds have been demostrated.The two-parameter model and the equationsof ice nucleation,cloud-rain autoconversion and ice multiplication seem tobe reasonable,but the equation of ice aggregation is not good enough.

本文用我们的微物理模式根据 P.V.Hobbs 在美国获得的中纬度气旋云系和降水的中尺度和微尺度结构的探测资料进行了计算。在计算的六个例子中,微物理垂直剖面同实测结果在很多方面是相符的。模拟得出了同实测比较一致的层状云“播种-供应”机制,高空发生胞的“播种”作用和暖层云中的降雨过程等。分析表明,模式所用的双参数方案、冰晶核化、云雨自动转化、冰晶繁生等方程能较好地反映云中微物理过程,但是冰晶聚合过程的模拟(主要是碰并系数E_(ii)的表达式)需要改进。

The development of shower, hail and heavy rain was simulated by an one-dimensional time-dependent model, using real rawinsonde data as input. Calculations demonstrated the continuity of heavy rain and the low precipitation efficiency in hail cloud. It also showed that Bergeron's process was not important and the warm-rain process was essential for precipitation development in modeled cumulonimbus with warm cloud bases. Comparision of calcutation with observation showed...

The development of shower, hail and heavy rain was simulated by an one-dimensional time-dependent model, using real rawinsonde data as input. Calculations demonstrated the continuity of heavy rain and the low precipitation efficiency in hail cloud. It also showed that Bergeron's process was not important and the warm-rain process was essential for precipitation development in modeled cumulonimbus with warm cloud bases. Comparision of calcutation with observation showed agreement in many aspects.

用文(一)的微物理模式在一维时变动力学框架里模拟了江西阵雨云,75·8暴雨和张家口冰雹云。用实测探空作为输入,计算结果同实测的云降水和雷达回波特征相比,在很多方面相当一致。它展示了暴雨云的持续性和冰雹云的低降水效率等,表明了在这些云底较暖的积雨云中贝吉隆过程对降水作用不大,而暖雨过程则是启动降水的主要环节。

 
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