不稳定层的英文

• instable layer

• "不稳定"英文翻译    instability; unstabitily; sw ...
• "层"英文翻译    I storey; tier; stratum
• "不稳定层结" 英文翻译 :    unstable stratification
• "不稳定层理" 英文翻译 :    unstable stratification
• "稳定层" 英文翻译 :    persistent horizon; resistant bed; resistant strata; stability layer; stabilized course; stabilizing layer; stable layer; stationary layer
• "非稳定层流" 英文翻译 :    unsteady laminar flow
• "稳定层结" 英文翻译 :    stable stratification; stablestratification
• "稳定层流" 英文翻译 :    stably stratified flow
• "不稳定" 英文翻译 :    instability; unstabitily; swinging; astable; unsteadiness
• "不稳定风；不稳定气流" 英文翻译 :    u teady wind; u teadywind
• "摆动，犹豫、不稳定" 英文翻译 :    wobble
• "波动不稳定" 英文翻译 :    oscillating unsteady flow
• "不稳定，动荡" 英文翻译 :    instability
• "不稳定保" 英文翻译 :    u table protection; unstable protection
• "不稳定爆炸" 英文翻译 :    erratic explosion
• "不稳定币值" 英文翻译 :    unstable dollar
• "不稳定边坡" 英文翻译 :    instable slope; unstable slope
• "不稳定边缘" 英文翻译 :    mobile rim
• "不稳定波" 英文翻译 :    u table wave; unstable wave; unsteady wave
• "不稳定波动" 英文翻译 :    erratic fluctuations
• "不稳定步态" 英文翻译 :    unsteady gait
• "不稳定残体" 英文翻译 :    unstable relict
• "不稳定产量" 英文翻译 :    unsteady rate
• "不稳定常数" 英文翻译 :    i tability co tant; instability constant; unstable constant
• "不稳定沉降" 英文翻译 :    detrimental settlement

• At the same time , the disturbance of the low - level jet might be the triggering condition for heavy rain . but the surface occluded front crossing qinling mountains and strengthening , maybe the direct reason
  同时，由于冷空气是从中层侵入西北地区东部，这样就形成了较强的对流不稳定层结，有利于对流降水的发生。
• It is the important mechanism that middle - level dry and cold air current sunk , low - level warm and wet air current ascended . level direction energy sharp section is important to blaze middle scale hypo - circumfluence . severe convection weather was brought by layer - knot latent instability
  上层干冷、下层暖湿的位势不稳定层结可以使对流层中低层出现明显的逆温层，有利于不稳定能量积累，此次天气过程产生的对流不稳定能量大，形成的上升气流深厚。
• 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。