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暖云
相关语句
  warm cloud
     In the warm cloud, the relative humidity is 100 %.
     暖云中相对湿度为100%。
短句来源
     Simulated results of the explicit cloud scheme are better than those of warm cloud scheme.
     不同云降水方案对短期气候影响的试验结果表明暖云方案和混合相云方案模拟的降水、地表气温、云量等有显著的差异。
短句来源
     In the paper, The result indicates that the optimum seeding height and the optimum seeding efficiency of liquid droplet seeding precipitation in warm cloud is restricted by vertical velocity of the air (w), Water content of the clouds (Q), radius of thd clouds drops (r), and thickness of the clouds (ΔH).
     用液滴催化暖云降水,达到“以小得大”的降水目的,结果指出:液滴催化暖云降水的最佳播撒高度和最佳播撒效率受到云中垂直气流速度(ω),云含水量(Q),云滴半径(r)和云层厚度(ΔH)的制约。
短句来源
     STUDY ON THE OPTIMUM SEEDING HEIGHT FOR LIQUID DROP IN WARM CLOUD
     液滴催化暖云最佳播撒高度的研究
短句来源
     AN EXPERIMENTAL STUDY ON SPECIFIC PROPERTY OF SEVERAL CATALYTIC AGENT APPLIED IN ARTIFICIAL WARM CLOUD AND FOG DISSIPATION
     几种消暖云(雾)催化剂性能的实验研究
短句来源
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  warm clouds
     AN OBSERVATIONAL STUDY ON THE CHARGE-SIZE OF RAINDROPS FROM WARM CLOUDS
     暖云雨滴大小和电荷的观测研究
短句来源
     The results show that the distribution of convective clouds is evidently different in time and space, and mixed clouds are the main cloud water resources in South China, but warm clouds can not be ignored.
     结果表明 ,中国南方夏季对流云时空分布很不均匀 ,不同地区、不同时段均表现出较大的差异 ; 无论是从对流云出现频数还是云区面积来看 ,混合云在南方对流云中占绝对优势 ,是南方降水的主要降水云 ,但暖云仍然是不可忽视的云水资源。
短句来源
     The results are discussed and explained in terms of the electric-f ica tion mechanism through ion-drop interaction during the formation of raindrops in warm clouds.
     本文用暖云中雨滴形成时离子与雨滴的相互作用的起电机制来讨论和解释上述结果。
短句来源
     The convective bubbles were observed in the warm clouds under the middle of the cumulostratus on 21,June 1992. The bubbles clearly show that they are one kind of mesoscale organization. It suggests that the synoptic system is situable to produce convective bubbles. It's contrastly analysed that the particle concentration and the liquid water content are higher.
     1991年6月21日个例观测到对流泡位于层积云下部暖云中的部分,泡状结构明显,呈现出中尺度组织特征,天气系统的配置有利于垂直上升运动的发展:通过对比分析,发现对流泡内具有云滴浓度高、液态水含量较高、云谱型相似以及2D-C粒子尺度大等特点:本次个例观测到的对流泡内云滴谱表现为单峰型。
短句来源
     The effects of the fluctuating condensation of Markor type and the single discontinuous gravitational coagulation on closing the droplet growth gap in convective warm clouds pointed out by Mason and Fruppacher are considered .
     对于Mason,Pruppacher等人指出的对流暖云大云滴增长速度谷,本文从马尔柯夫型起伏凝结过程的作用,以及它和一次不连续碰并过程在分段模型下的作用观点出发,进行了一次初步的分析。
短句来源
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  “暖云”译为未确定词的双语例句
     This paper analyses climatic features of cloud and precipitation on the Leizhou Peninsula,researches cloud dynamics and forming mechanism of precipitation and artificial precipitation and catalyst,and summarizes test results. The conclusion is that : there are abundant resources of water in the air on the Leizhou peninsula; and mechanisms of precipitation of warm-cloud,cold-cloud and mixed-cloud are possible.
     通过对雷州半岛云水资源气候分布、云的宏观动力学和微观物理学、降水形成机制、人工增雨机制、冷云催化剂与暖云催化剂、播云方式与催化方法的研究和对外场试验的总结,表明:雷州半岛空中具有丰富的云水资源,有暖云降水机制、冷云降水机制和混态云“播种—供水”降水增强机制。
短句来源
     Contrast experiment show that this paper's retrieved variables are available to Kessler warm microphysical scheme and NCEP-3Class simple ice scheme, while Liuqijun simple ice scheme's forecast results are worse.
     (4) 对比试验表明,本文方案反演的水成物和垂直速度比较适合Kessler暖云模式和NCEP-3Class简冰模式,对Liuqijun简冰方案不太适用。
短句来源
     The three layers,ice crystal layer,supercooled water layer and warm water layer,contribute 7%,54% and 39% to the surface precipitation,respectively. The first layer seeds ice crystals and a little snow crystals to the feeder cloud (the second layer). And the second layer seeds snow crystals,graupel particles and raindrops to the feeder cloud(the third layer).
     云的第一层对第二层有播种作用,冰晶层对降水的贡献为7%,过冷水层对降水的贡献为54%,暖水层对降水的贡献为39%,降水的产生中冷云过程作用稍大,但暖云过程也起重要作用。
短句来源
     A new cloud model of two-dimensional time-dependent anelastic, nonstatic equilibrium has been used to simulate the effects of low-level wind shear on convection in this paper.
     本文对已有的二维时变的深对流型模式[1]进行了部分修改和补充,尤其对于云微物理过程参数化方案进行了一些改进,使原有的模式对暖云、雹云和雪云都具有一定的模拟能力。
短句来源
     The hail embyros were formed mainly through conversion of cloud droplets to graupels in the hail clouds of the colder cloud base,while for the warmer cloud base, they were formed through the conversin of raindrops to graupels.
     云底温度较低的冰雹云的雹胚形成以云霰转化过程为主,暖云底的雹云则以雨霰转化为主。
短句来源
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  warm cloud
Rainfall that occurs during days without low OLR (weak convection with warm cloud tops or isolated deep convection) contributes to 69% of the total rainfall during dry sequences and 45% during wet sequences.
      
More locally it is embedded in a small warm cloud of density 0.07cm-3, temperature 7000 K, column density ~ 5 × 1017 cm-2 - which gives a mass of about 0.1M⊙.
      
It is suggested that the initiation of rainfall in a precipitating warm cloud can be viewed as an instability triggered by the presence of a power-law distribution.
      
A warm cloud seeding experiment under AARRP was carried out during 1995-1998.
      
Cloud cost with single window channel tends to overlook ice cloud and lower-level warm cloud.
      
更多          
  warm clouds
Emission was detected toward molecular clouds with kinetic temperatures of 20-60 K (so-called "warm clouds").
      
For most sources, the statistical-equilibrium calculations yielded gas temperatures of about 20-30 K and densities of about 104-106 cm-3, which are typical for warm clouds.
      
On the use of poorly soluble hygroscopic substances for modification of warm clouds and fogs
      
Aircraft observations of electrical conductivity in warm clouds
      
The value of electrical conductivity in warm clouds is found to be in the order of 10-12 ohm-1 m-1 which is two orders higher than that observed in clear-air at cloud-base levels in some regions by other investigators.
      
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试验对象是暖云,用食盐水和干冰等作催化剂.食盐水对人工降水来说比干冰好.以自然冰花加盐作为催化剂也进行了试验.

An one-dimensional time-dependent model of precipitation in warm layer cloud is given. The influence of some factors on warm rain process and its initiation is tested. The process of rain enhancement by salt-seeding is simulated and discussed.

本文提出层状暖云降水的一维时变模式,用数值试验方法探讨了层状暖云降水的临界条件,各种物理参量对降水过程的作用以及播撒盐粉的增雨效果和最佳催化技术。

The initial stage echoes in convective clouds and their growth processes were observed by 711 type radar at Tunxi Anhui Province during June to July, 1979-1981. Analysis of the data yields the following conclusions: (1) In summer most of initial stage echoes are appeared in warm region of convective clouds. It implies that the dominant precipitation initiation mechanism in convective clouds at Tunxi is the condensation-coalescence process. (2) By the use of the thickness of echo (35 dbz), the rise velocity and...

The initial stage echoes in convective clouds and their growth processes were observed by 711 type radar at Tunxi Anhui Province during June to July, 1979-1981. Analysis of the data yields the following conclusions: (1) In summer most of initial stage echoes are appeared in warm region of convective clouds. It implies that the dominant precipitation initiation mechanism in convective clouds at Tunxi is the condensation-coalescence process. (2) By the use of the thickness of echo (35 dbz), the rise velocity and the height of echo top, and the height change of reflectivity core in the initial stage echo, the intensity of convective precipitation can be qualitatively estimated.

1979—1981年6和7月份在安徽屯溪机场,用711雷达对对流云初期回波及其发展过程进行了观测。资料分析表明:(1)对流云的初期回波绝大多数是在云的暖区形成的,因此,屯溪地区夏季对流云中暖云过程对降水形成起重要作用.(2)用回波顶升速、回波顶高和强度为35dbz回波的厚度、初期回波中心高度变化情况可以定性估计积云降水的强弱.

 
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