Like a spark between a cloud and a lightning conductor, the liquid stretches out to the collector.
就像云块与避雷针之间的一个火花，液体向收集器扩展。
If the planet has an atmosphere like ours, it would need about 50 percent cloud cover to stay cool enough for liquid water to exist on the surface.
如果这颗行星有跟我们一样的大气层，就需要覆盖大约50%的云层来保持它足够凉，这样液态水才能在行星的表面存在。
Alien world could host liquid water if it has 50 percent cloud cover, study says.
研究表明，如果外星星球覆盖50%云层就可能拥有液态水。
Cloud liquid water path (i. e. vertically-integrated cloud liquid water) is an important parameter in meteorology and cloud and mist physics.
云水总量(也可称为液水路径)是一个重要的气象学和云雾物理参数。
The introduced mathematical model takes into account the action of the kinetic fractionation effect in super saturation environment at ice surface as liquid and solid phases coexist in mixed cloud.
文中介绍的数学模型考虑了混合云中液、固相共存时以及冰面过饱和环境下稳定同位素的动力分馏效应。
The introduced mathematical model takes into account the role of the kinetic fractionation effect in a supersaturation environment at the ice surface as liquid and solid phases coexist in mixed cloud.
介绍的数学模型考虑了混合云中液、固态共存时以及冰面过饱和环境下稳定同位素的动力分馏效应。
Numerical simulation for the cloud movement during explosive dispersion of liquid fuel was carried out.
对液体燃料的爆炸抛撒形成的云雾运动作了数值模拟。
A waxy cloud or haze appears in the liquid.
在液体中出现蜡点或混浊。
Before the precipitation, there appears a process of obvious increase in the amount of water vapor and cloud liquid water, and after the precipitation, a process of obvious decreases.
在降水发生之前，水汽和云中液态水含量均会出现一个显著增加的过程，而在降水结束之后则会出现一个显著减少的过程。
The fundamentals and method of deducing path-integrated cloud liquid water content (L)by an airborne up-looking microwave radiometer are introduced in this paper.
本文介绍机载对空微波辐射计探测云中路径积分液态水含量（L）的辐射传输原理和反演方法；
Retrieving spatial distributions of cloud liquid water content (LWC) from the airborne double-antenna microwave radiometer data by tomography method is a limited-angle image reconstruction.
通过机载双天线微波辐射计的观测数据层析反演出云液水的空间分布是一个有限角度的图像重建问题。
The fundamental and method of the ground-based microwave radiometer remote sensing retrieval of integrated water vapor(V) and cloud liquid water(L) in the atmosphere are introduced herein.
介绍了地基微波辐射计遥感反演大气柱中的水汽总量和云液态水总量的辐射传输原理和反演方法。
Macro and micro physics conditions of supercooled fog dissipation operation using liquid Nitrogen with that of the cold cloud seeding are compared.
对用液氮消过冷雾和冷云催化增雨作业的宏、微观条件进行比较，找出其异同点。
If consider the maximum radius of the dispersed cloud only, the solid FAE bomb isn't superior to liquid FAE bomb in the same mass, but the increasing action volume of the solid FAE bomb is bigger.
若仅考察弹体云雾最大半径，固相fae弹体并不比等质量的液相fae弹体优越太多，但固相fae弹体的爆炸作用体积增大较多。
If a flammable cryogenic liquid is involved, the flammable mixture zone, under unusual atmospheric conditions, may extend beyond the normal fog cloud produced by condensing water vapor in the air.
如果同易燃低温液体有关，在异常大气条件下，易燃混合物地带会延伸到空气中的水蒸汽的浓缩产生的正常雾云以外。
The number of ice crystals generated from lg liquid Nitrogen was determined in a cloud chamber.
该文对液氮成冰效率作了小云室实验介绍。
It is a new method for liquid - liquid extraction that the preconcentration of samples is based on micelle - mediated phase separation by the character of surfactant cloud point.
通过表面活性剂浊点特性实现胶束相分离以达到样品预富集，是一种新兴的液-液萃取方法。
A statistical method for retrieving the total water vapor and cloud liquid water content and a non-linear iterative algorithm for retrieving the water vapor profiles in the troposphere are discussed.
讨论了水汽总量和云中液态水含量的统计反演法以及水汽垂直分布的迭代反演法。
The precipitation is composed of ice particles in the upper altitude, snow, graupel, raindrops and the cloud liquid water in the lower altitude.
分析模拟结果中特定点的水成物垂直分布发现：降水云由高空冰晶、中低空雪、霰、云水及低空雨水等组成。
The distribution place of pw retrieved by the databases controlled with compositive criteria is consistent with cloud liquid water computed from Doppler Radar.
综合判据法控制的数据库对可降水的位置的反演与地面雷达反演的液态水位置最接近。
The results show that, the content of cloud liquid water is overestimated by the AREM while the content of precipitation ice is underestimated.
研究结果表明，AREM模拟的云水含量稍偏高， 降冰含量稍偏低；
The results show that, the content of cloud liquid water is overestimated by the AREM while the content of precipitation ice is underestimated.
研究结果表明，AREM模拟的云水含量稍偏高， 降冰含量稍偏低；
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