潜热释放的英文

• latent heat release

• "潜热"英文翻译    latent heat
• "释放"英文翻译    release; deliver; clearing; ...
• "热释放" 英文翻译 :    heat release; thermal desorption; thermal discharge; thermal release; thermal relief
• "峰热释放率" 英文翻译 :    peak heat release rate
• "热释放带" 英文翻译 :    zone of heat liberation
• "热释放基座" 英文翻译 :    thermal relief pad
• "热释放机理" 英文翻译 :    mechanism of thermal release
• "热释放率" 英文翻译 :    rate of heat release
• "热释放信号" 英文翻译 :    heat release signal
• "热释放动力学" 英文翻译 :    heat release kinetics
• "潜热" 英文翻译 :    [物理学] latent heat◇潜热释放 latent heat release
• "俄亥俄州立大学热释放率测试仪" 英文翻译 :    ohio state university heat release rate apparatus
• "建筑材料热释放速率试验方法" 英文翻译 :    test method for heat release rate of building materials
• "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
• "热释光" 英文翻译 :    thermal glow; thermoluminescence; tl
• "释放" 英文翻译 :    1.(恢复被拘押者的人身自由) release; deliver; clearing; set free 取保释放 be released on bail; be bailed out; 刑满释放 be released upon completion of a sentence; 他被释放出狱。 he was released from the gaol.2.[物理学] relief; rid; detachment; trip; tripping; release 释放出能量 release energy; 释放裁定书 rulings of acquittal; 释放程序 release procedure; 释放出狱令 order of release; 释放激素 releasing hormone; 释放令 order for discharge; order of acquittal; 释放囚犯 discharge for prisoner; release a prisoner; 释放语句 free statement; 释放者 releaser; 释放证书 release certificate
• "释放……" 英文翻译 :    release sb/sth from sth
• "【物理学】潜热。" 英文翻译 :    latent heat
• "表面潜热" 英文翻译 :    latent heat of surface

• 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。
• In a word , convective instability strong baxoclinicity barotropic advection of potential vorticity and latent heat release are factors which activize this explosive development of cyclone
  总之，对流不稳定、强斜压性和正压位涡平流、潜热释放是本次气旋发展的启动因子。
• The effect of dragging force weakens the convection and the effect of latent - heat release strengthens the instability . both of them are evidently feedback actions to the environment
  云中水凝物下落的拖曳作用削弱了对流，相变潜热释放加剧了层结不稳定，均对热力动力过程有明显反馈作用。
• After the storm move in shandong area , the moist downdrafts appears , the mgws apart from the thunderstorm and move faster , the mgws weaken gradually because absence of wave duct and energy supply
  成熟阶段的对流风暴，由于中高层潜热释放和湿下沉气流进一步加强，波动传播加快； mgws和对流风暴分离后，因无“波道”机制和波能供给，波幅逐渐减小。
• In order to overcome the difficulty mentioned above , this paper provides an improved heat transfer equation and a mended bem for the problems . first of all , the enthalpy and the " virtual temperature " are introduced into the paper to eliminate several mutative thermophysical properties in the heat transfer equation . secondly , the movement of the boundary between the solid and liquid phases in the billet is educed by virtue of the laplace transform
  这些改进包括：引入热焓和“虚拟温度”的概念，对非常数的热物性参数进行整合：充分考虑铸坯凝固潜热释放带来的影响，利用“温度回升法”来加以处理；利用拉氏变换和反拉氏变换的原理来对凝固过程中铸坯内部固液相界面的移动方程进行了推导和求解，在凝固过程中充分考虑铸坯内部的固液两相的影响等等。
• Wet and dry numerical simulation tests for explosive cyclone over western pacific were performed . by contrast the results show that : tropopause and constant temperature surface were raised by latent heat release in upper level and disturbance trough was produced because air flow ascended and became cold . owing to this process adaption , inertial instability emergenced
  对气旋强烈爆发的过程进行干湿对比数值模拟试验，得出：潜热释放使对流层项和等温面抬高，气流在高层的上升冷却形成扰动槽，其适应过程使高层出现惯性不稳定。
• 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。
• The above analysis showed that this heavy rainfall event took on obvious meso - scale characters and was the combination of the three flows , so we can deduce : ( 1 ) surface southeasterly wind and topography may play the main role in this event ; ( 2 ) the easterly cold air rushing into the southern shaanxi province in the lower troposphere was strongly relative to the form of surface cold - front type of occlusion ; ( 3 ) there were two reasons for the secondary circulation ' s strengthen in the evening , one was the effect of a mountain - valley wind and the other may be latent heat leading to ascending motion ; ( 4 ) the shape of potential instability stratification corresponded well with the development of the warm - moisture advection ; and ( 5 ) the vapor providing essential thermodynamics was transported by a southwesterly low - level jet from the bay of bengal and the south china sea . furthermore , with the effect of terrain , the southern shaanxi province became the center of this extremely heavy rain process
  中尺度结构分析表明，本次暴雨具有明显的中尺度特征，是由三支气流共同作用的结果，分析发现( 1 )地面东南风和地形在这次大暴雨过程起主要作用； ( 2 )东路冷空气主要是通过中低层侵入陕南地区的，并与地面冷式锢囚锋的形成密不可分； ( 3 )夜博士论文:中尺度地形对陕南暴雨的影响研究间垂直次级环流发展加强可能有两个原因，一个是由于地形山谷风的作用，另一个是降水的潜热释放激发了上升运动: ( 4 )位势不稳定层结的形成与低层暖湿平流的发展有很好的对应关系; ( 5 )本次暴雨的水汽主要靠偏南风急流将孟加拉湾和中国南海的水汽输送至西北地区东部，为暴雨的发生提供了必要热力条件。
• To the large - scale atmosphere , we separate the terms of the horizontal vorticity converting into the vertical vorticity , which considered as the baroclinic terms , from the terms that not including horizontal vorticity by the rules of the p coordinate transforming to the z coordinate in the traditional vorticity equation , and carry out the scale analysis , and then conclude that the baroclinic terms are able to reach the same magnitude grade as the partial derivative of the vertical vorticity to time when it takes place the large scale precipitation in the summer monsoon period in china . by analyzing the game reanalysis data from april to august in 1998 in the region of chinese continent , we found that the baroclinic terms is important to the large - scale cyclone developing above the 600hpa , and the magnitude changing of the baroclinic terms is nearly in - phase as the monsoon movement , so which imply exactly that the magnitude changing of the baroclinic terms is the one of the natural characters of the summer monsoon evolution and equivalent to the movement rule of the subtropical high of the western pacific
  在p坐标垂直涡度方程中，利用p坐标向z坐标转换的公式将水平涡度向垂直涡度转化的所有项分离出来，这些项具有明显的斜压特征，对其进行尺度分析后，得出在可以忽略潜热释放对涡度影响的对流层中、高层，此转化项是大尺度斜压涡度发展的重要项。通过对1998年48月的game再分析资料进行实际计算也发现，转化项在东亚夏季风上升支的600hpa及以上层次对垂直涡度的局地变化贡献很大，不能忽略。同时发现水平涡度向垂直涡度的转化在南海季风爆发时和江淮梅雨入梅及发展过程中均有指示性意义，在南海季风爆发以后，在中国东南部地区，转化项的大小与夏季风的活跃和中断等活动有着几乎一致的变化规律，这从侧面也指出了，此转化项的变化是夏季风演变所具有的本质特征，并且它反映出了西太平洋副高在中国大陆的活动情况。