microphysical 中文意思是什麼

microphysical 解釋
微觀物理學的
  1. In this paper, four cases of heavy rainfalls and snowfalls in china are simulated by using mm5. cloud microphysical characteristics and sources of rain, snow and graupel have been particularly studied

    運用中尺度非靜力數值模式mm5v3 ,對我國華南前汛期暴雨、梅雨鋒暴雨、北京東風迴流降雪和遼寧寒潮大風雪等四次過程分別進行了模擬研究。
  2. The main mechanism of enhancing precipitation is that much ice nuclei turn into ices, and then snow ; graupel are formed more by microphysical processes. the melting of graupel makes precipitation more than that of unseeded clouds

    主要的增雨機制是大量冰核活化成冰晶,冰晶通過增長和其他的微物理過程形成雪晶、霰,霰最後融化成降水使地面降水量增加。
  3. Based on the dynamic frame of mm5 and reisner 2 explicit cloud scheme, a new double - moment microphysical scheme was developed, in which both the mixing ratios and number concentrations of cloud water, rain water, cloud ice, snow and graupel were predicted

    從本質上說,該方案預報的僅僅是粒子的比含水量。在mm5動力框架內,在其中的reisner2方案基礎上採用雙變參數方案,增加了雲水、雨水、雪和霰的數濃度預報方程。
  4. A complex mixed - phase explicit microphysical parameterization scheme, which also be known as reisner 2 explicit scheme was developed for use in the ncar / penn state mesoscale model versions ( mm5 ). the single - moment schemes has additional variables for graupel and ice number concentration, in which the mixing ratio of cloud water, rain water, cloud ice, snow and graupel are predicted and number concentration specified

    Mm5中的reisner2方案是一種含霰的復雜混合相顯式雲物理方案,該方案包含了雲水、雨水、冰晶、雪和霰的混合比預報方程,同時對冰晶的數濃度作了預報。
  5. Using the 1ap 3 - d hailstorm numerical model, we analyze influence of variation on rainfall amount, hail fallout amount, dynamical process of cloud, microphysical process, mechanism of hail suppression with seeding, and seeding outcome. besides, we use those study outcomes and bring forward some advice about using and improving model. we simulate a hailstorm occurred in nanjing county and analyze influence of raindrop, ice crystal, graupel size distribution on outcome of model

    本文利用中國科學院大氣物理研究所的三維冰雹雲催化數值模式,通過對冰雹雲的模擬和對譜參數的數值試驗結果,分析了冰雹雲中粒子譜形的變化,對雲和降水過程的影響,其中包括雨滴譜、冰晶譜、霰譜的形狀參數對自然雲的發展過程、降雨降雹、雲中微物理過程、霰以及冰雹的形成機制的影響。
  6. A comparison between microphysical characteristics derived from 3 - d cloud model and the results from trmm tmi and pr products show that the selected cloud model gives a relatively realistic hydrometeor profiles

    由三維雲模式得到的微物理特徵與由微波圖像儀tmi和pr產品提供的結果之間的對比表明,所選用的雲模式能夠給出相對真實的水汽凝結體廓線。
  7. In this paper aircraft has made vertical and synthetic detecting flying purposefully on 9. 17, 2003 according to cloud ' s macro and microstructure. vertical layers and representative places of stratiform cloud on 9. 17, 2003 are analyzed using the observational data of particle measurement system ( pms ), combined with satellite data, radar data, and precipitation data on ground. by this we have got cloud ' s microphysical structure and physical process of the natural precipitation, and the physical effect evidence has been testified according to observational data after lco2 seeding

    本文用綜合觀測的方法,利用機載pms雲粒子探測系統,根據雲系的宏微觀結構特徵進行有針對性的垂直探測飛行,配合衛星、雷達、地面雨量、雨強計網觀測資料對2003年9月17日延安降水性層狀雲系中那些有代表性的部位或垂直分層做細致的觀測分析,獲得雲系的微物理結構和自然降水形成的物理過程,並用觀測事實來驗證人工增雨引晶催化后的物理響應判據。
  8. ( 3 ) chapter v. plasma characteristics of rf ion source is investigated. a zero - dimensional numerical dynamic colisional radiative atomic and molecular ( cram ) model is suggested to simulate the microphysical process. all species " population number densities in plasma are calculated in non - thermodynamics equilibrium condition, and proton content in extracted ion current are measured with 60 ? magnetic analyzer

    ( 3 )提出了高頻離子源等離子體的零維cram模型( collisionalradiativeatomicandmolecularmodel ) ,計算了非平衡態( nte )下等離子體中分子、電子、離子、基態原子、激發態原子等粒子濃度,並在zf - 200kev中子發生器上,用60磁分析器實驗測定了引出束流的質子比。
  9. The main results show that i variation in two hailstorms has different effect on surface rainfall, surface hail fallout, rainfall intensity, hail fallout intensity. in two hailstorm, i variation has no effect on formation mechanism of particles in cloud, but i variation has different effect on microphysical processes in cloud

    主要結果表明,不同地區冰雹雲中冰晶譜形的變化對自然雲中降水的影響程度是不同的,當降雹強烈時,冰晶譜形的變化對自然雲中降水的影響尤為明顯。
  10. These works include the cloud system families of the meiyu heavy rainfall and their interactions, the structure, precipitation characteristics and microphysical features of the mesoscale convective complexes ( mcc ), the favorable genesis and evolution settings for mcs, the different environments between mcc and meso - p - scale convective system, the relationship between the tropical water vapor plume ( wvp ) and mcs, and what characteristics of the wvp

    先後分析了梅雨暴雨系統的雲系成員及其相互作用;中尺度對流復合體( mcc )的結構、降雨特徵、微物理特徵及其形成和發展的有利環境條件;不同類型中尺度對流系統( mcs )形成與發展的環境條件差異;熱帶水汽羽和暴雨雲團的關系,水汽羽的動力和熱力特徵。
  11. In this thesis a three - dimensional cloud model - microwave radiation transfer model combination is used to study the relations among the precipitation, other microphysical characteristics of a convective cloud system and the upwelling radiance at pertinent microwave frequencies. the results of the model are preliminarily compared with trmm products

    本文利用對流性降水雲微物理模式和三維微波輻射傳輸模式,研究了中國陸地上暴雨系統的微物理結構,以及在特定的微波頻率對流性降水雲的降水強度、雲中各種微物理量與上行輻射之間的關系。
  12. The observation of cloud microphysical structure and the analysis of seeding physical effect play an important role in artificial precipitation - enhancement

    降水過程的雲微物理結構的觀測和催化效應的分析在人工增雨中佔有重要的地位。
  13. Introduction of mm5 meso - scle model and its microphysical process

    5中尺度模式及其微物理過程
  14. Review on ground - based sounding and retrieving of cloud microphysical parameters

    雲微物理參數的地基探測反演研究綜述
  15. By adding the calculation and output program for new prognostic variables, the new scheme is incorporated in the three - dimensional non - hydrostatic model mm5 and becomes a new option in its explicit microphysical scheme, which will be so - called as the new scheme in the paper

    通過增加新預報量的計算和輸出程序,在mm5顯式方案中新增加了一個可選方案,以下稱之為新方案。
  16. The output of the new scheme could give reasonable microstructure of cloud and indicate some characteristics of stratus cloud, which enhances the capability of mm5 to study the cloud microphysical process. the numerical simulation reveals the possible mechanism of the rainfall by one station microphysical process analysis

    模擬給出了雲的合理微觀結構,揭示了層狀雲的一些特徵,增強了mm5研究微觀雲物理的能力;通過單站微物理過程分析,揭示了降水過程的可能形成機制。
  17. The cloud water in the concerned clouds was consumed quickly after seeding. ice - phase particles appear earlier, and their concentrations and contents increased. microphysical processes turn more active

    在雲體內部,雲水迅速被消耗,冰相粒子出現時間提前,濃度和含量明顯增加,各種冰相過程反應強烈。
分享友人