凝结潜热的英文

• latent heat of condensation

• "凝结"英文翻译    condense; condensation
• "潜热"英文翻译    latent heat
• "潜热" 英文翻译 :    [物理学] latent heat◇潜热释放 latent heat release
• "固结潜变（台）" 英文翻译 :    creep
• "凝结" 英文翻译 :    1.(气体变为液体) condense; condensation 云是由大气中的水蒸气凝结成的。 a cloud is a condensation of water vapour in the atmosphere. 水蒸汽触及冷的表面即凝结成水。 steam condenses to water when it touches a cold surface.2.(液体变为固体) coagulate; congeal; congealment; freeze-up; clotting; curdle; coagulation 湖面上凝结了一层薄冰。 a thin layer of ice formed over the lake.3.(结合) cement; concrescence; 凝结点 set point; 凝结剂 coagulant; coagulating agent; 凝结加速剂 setting accelerator; 凝结力 coagulating power; 凝结期 setting period; 凝结时间 setting time; 凝结温度 adiabatic condensation temperature; adiabatic saturation temperature; condensation temperature; 凝结物 [病理学] concretionary; sympexion; coagulum; 凝结作用 coagulation; desublimation
• "比潜热" 英文翻译 :    heat, specific latent; specific latent heat
• "内潜热" 英文翻译 :    internal latent heat
• "潜热能" 英文翻译 :    calorific potential
• "潜热值" 英文翻译 :    potential heat value
• "外潜热" 英文翻译 :    external latent heat
• "真潜热" 英文翻译 :    true latent heat
• "总潜热" 英文翻译 :    total latent heat
• "【物理学】潜热。" 英文翻译 :    latent heat
• "表面潜热" 英文翻译 :    latent heat of surface
• "冰冻潜热" 英文翻译 :    latent heat of freezing
• "化学潜热" 英文翻译 :    potential chemical heat
• "聚变潜热" 英文翻译 :    latent heat of fusion
• "量潜热器" 英文翻译 :    laten heat calorimeter
• "每克分潜热" 英文翻译 :    latent heat per mol
• "每克潜热" 英文翻译 :    latent heat per gram
• "莫耳潜热" 英文翻译 :    molar latent heat
• "凝固潜热" 英文翻译 :    latent heat of freezing; latent heat of solidification
• "气化潜热" 英文翻译 :    gasification latent heat; latent heat of vaporization
• "汽化比潜热" 英文翻译 :    specific latent heat of vaporization
• "汽化潜热" 英文翻译 :    latent heat of vaporization; latentheatofvaporization; vaporization heat; vaporization latent heat; vaporization, latent heat of

• It is necessary to include as a heat source in the thermodynamic energy equation at erm which represems the timerate of release of the latent heat of condensation of water vapor
  译为:有必要把代表水汽凝结潜热释放的随时间变化率的一项作为热源项包括在热力学能量方程中。
• On the beginning , the first low was warmer from the low level to the high level . only after developing , it also became colder on the low level and wanner on the upper level , which was the result of the release of coagulation heat with rainfall
  第一个低涡在出生时从低层到高层都是暖心结构，但在发展之后也成为下冷上暖的结构，三个低涡在发展过程中出现的这种下冷上暖的结构表明在低涡中上层有大量的降水释放凝结潜热。
• The analysis of the large - scale synoptic situation shows that strong precipitation is closely related to the explosion of monsoon and the intensification of cross - equatorial flow which bring a lot of vapor and meet with cold masses at the eastern of northwest district on 8th , june causing extremely heavy rainfall ; that subtropical high - level jet at 200hpa , subtropical high at 500hpa and low - level jet at 850hpa are the weather backgrounds favorable to strong precipitation ; that the pattern of eastern highs and western lows and the establishment of a low - level jet and the coupling between upper - and low - level patterns that determine that the rain occurred in the east of the northwest china ( on average , this is the rainy season for the south of china , but not for the northwest china ) ; that water vapor comes from southerly and easterly flow which converge at the eastern of northwest district with convergence mainly in lower levels and pbl ; that the high value of the whole - level apparent heat source < q1 > is near the area of large rainfall in the direction of northeasterly - southwesterly agreeable to shear line very well and the condensation latent heat releasing is main heat source with vertical advection item playing key role in q1 and q2 ; that there is a vertical secondary circulation crossing low - lever jet whose ascending branch is at the area of large rainfall ; that the construction of convection instability and conditional symmetry instability results that there is not only deep thermal instability , but also moisture influx and triggering mechanism of thermal instability causing strong torrential rain
  作为对比，本文还对2002年6月24 - 25日发生在北京地区的强地形雨进行了分析，并讨论陕南、北京地区两地暴雨的异同点以及地形作用的共性和个性，为两地暴雨预报提供有益的参考，得出了一些很有意义的结果： 1大尺度环流背景分析表明： ( 1 ) “ 02 . 6 ”强降水与6月上旬越赤道气流和季风爆发密切相关，携带大量水汽的偏南气流与冷空气于6月8日交汇在西北地区东部，导致了这次强降水的发生； ( 2 ) 200hpa的副热带西风急流、 500hpa副高以及850hpa的低空急流的配置非常有利于本文分析之陕西强降水的发展与维持。大尺度形势分析表明，东高西低形势场、低空急流的建立和高低空形势的配置决定了这场降雨出现在西北地区东部。与暴雨区相联系，存在一支横越低空急流的经向垂直环流，暴雨区处于该垂直环流的上升支； ( 3 )偏南和偏东气流水汽通道在西北地区东部交汇，水汽的辐合积聚主要在对流层低层和行星边界层内完成； ( 4 )整层的视热源< q _ 1 >高值区在暴雨区附近呈东北-西南向分布，与切变线走向非常一致，降水产生的凝结潜热释放是强降水区大气的主要热源。
• Strongly strengthening of the low level jet and releasing of the latent heat of condensation have effect on the occurrance of the disturbance of the moist potential vorticity in low lever , which is important conditions to the genesis and development of mesoscale vortex
  低空急流的加强以及凝结潜热的释放均可以影响到低层湿位涡扰动的产生，从而有利于中尺度低涡的生成和发展。减弱低空急流的对比实验证明了低空急流在对流层中低层中尺度低涡的生成和发展过程中起着关键性作用。