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Home > english-chinese > "cold mass" in Chinese

Chinese translation for "cold mass"

寒癖
冷气团


Related Translations:
masses:  包块马塞斯民众, 劳动阶层群众
mass:  n.弥撒;弥撒的仪式[祷告、音乐];弥撒曲。 a high [solemn] Mass (有烧香、奏乐等的)大弥撒。 a low [private] Mass (无烧香、奏乐的)小弥撒。 by the Mass 一定,的确。 say [read] Mass 作弥撒,念经。n.1.块,堆,团。2.群众,集团;〔the masses〕群众;民众。3.大量;大宗;众多;〔the
masser:  马瑟逐年信条
massing:  马辛梅辛
Example Sentences:
1.Thunderstorm form when a warm air mass is forced by a cold mass at a front
当暖气团在锋面处受到冷气团的作用时,就会形成雷暴雨。
2.It is during these seasons that the differences in temperature between warm and cold masses of air are greatest
就在这些季节里,热气团与冷气团的温差最大。
3.The performance of energy separation on the vortex tube designed by the author is studied at different cold mass flow ratios , and the characteristic curve has been drawn
对于本文设计的涡流管,研究了不同冷气流率时涡流管的能量分离特性,并且绘制了性能曲线。
4.The experimental results show that adiabatic efficiency has a remarkable improvement in low cold mass flow ratios , adiabatic efficiency can improve by 30 % in the best condition
实验表明,在冷流率小的情况下,通过加湿可以使得绝热效率得到显著的提高,最好可以提高30 。
5.Based on t213 and other observational datasets , a severe heavy rain occurred in changjiang - huaihe basins during 4 - 5 july 2003 is studied . the primary diagnostic analyses show that double or single block is the characteristics of the macroscale circulation in this rainfall process . the strong conflict of warm and cold mass , mesoscale convergence on meiyu front , shear line , and stably maintaining of high and low jets make for the rainfall
本文采用地面高空常规资料,每6h一次的降水资料,以及t213数值预报资料,对2003年7月4 - 5日发生在江淮地区的一次梅雨锋暴雨过程的影响系统及其可能机制进行了初步的诊断分析,发现,高纬双阻、单阻形势是这次暴雨过程发生的大尺度环流特征;冷暖空气的激烈交锋、梅雨锋上的中尺度辐合线、 700hpa 、 850hpa上的低涡、切变线以及稳定维持的高低空急流是导致这场暴雨的直接影响系统;该地区维持一个高能、饱和、潜在不稳定的环境,有利于特大暴雨的产生和维持。
6.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。
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