降水過程 的英文怎麼說

中文拼音 [jiàngshuǐguòchéng]
降水過程 英文
precipitation producing process
  • 降 : 降動詞1. （投降） surrender; capitulate 2. （降伏） subdue; vanquish; tame
  • 水 : 名詞1 （由兩個氫原子和一個氧原子結合而成的液體） water 2 （河流） river 3 （指江、河、湖、海、洋...
  • 過 : 過Ⅰ動詞[口語] （超越） go beyond the limit; undue; excessiveⅡ名詞（姓氏） a surname
  • 程 : 名詞1 （規章; 法式） rule; regulation 2 （進度; 程序） order; procedure 3 （路途; 一段路） journe...
  • 過程 : process; procedure; transversion; plication; course
  1. 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。
  2. By comparing model simulation with an observed precipitation formed by stratus cloud system, the new scheme shows the improvement of prediction precipitation

    利用新方案模擬了一次層狀雲降水過程，新舊方案降水模擬結果的對比表明新方案的降水預報效果有所改進。
  3. The main relative systems of heavy - hard rainfall in northeast plateau are western pacific subtropical high, south asia high, low latitude systems, upper level jet ( ulj ), low level greater wind speed axes, westerly trough and plateau trough, low level vortex, cold frontal, occluded front in qinghai lake, mesoscale low pressure, heat low - pressure in qinghai, shear line and convergence line, mesoscale cloud cluster, etc. the west subsidiary model of south asia high is the main circulation type of heavy - hard rainfall in this area

    3 、西太平洋副高、南亞高壓、低緯系統、高空急流、低空大風速軸；西風槽和高原槽、低渦、冷鋒、青海湖錮囚鋒以及中尺度低壓、青海熱低壓、切變線與輻合線、中尺度雲團等系統是高原東北部地區大到暴雨的主要相關系統。 100hpa上的南亞高壓中心強度加強，位置東西擺動預示高原地區將有降水產生，中心強度減弱，降水過程結束。南亞高壓西部副型是高原東北部地區大到暴雨的主要流型。
  4. ( 4 ) water flow model experiment is made and hydraulic pressure variation is observed, " the detainment and displacement " of semipervious aquifers in the process of decreasing water is also studied

    （四）模擬二元結構土層，進行土樣滲流試驗，觀測水壓的變化，研究弱透水層承壓水在降水過程中的「滯后和位差」現象和問題。
  5. Combining achievements in past scientific research, this thesis summarizes some problems in the process of decreasing water, the problems contains : important parameters such as percolation coefficient, interfering radius etc ; designers get parameters from their experience and make their choice of limited prospecting materials too simply, because of the limits, designer ca n ' t make quantitative analysis on groundwater ; differences on breakwater effect of setting water - tight screen is still existed, although research evolvement in this field is done ; they ca n ' t grasp the hydrogeology parameters accurately in that it influences rightness of designing in deep excavation water - decreasing

    本文結合以往的研究成果，總結了降水過程中存在的一些問題，主要包括：重要設計參數，如地層滲透性、基坑降水影響半徑等，設計中僅從個人經驗出發取值，對有限的勘探資料進行取捨和過分地簡化。這些局限使設計者不能對地下水進行科學的定量分析，盲目性較大；深基坑降低承壓水引起的周邊地面沉降的研究雖已取得很大的進展，但是一些主要問題仍未解決，對防滲帷幕的實際擋水效果存在不同看法；對於弱透水層的水文地質參數一直難以準確把握，影響了深基坑降水設計的正確性。
  6. In this process, the moisture of the initial field between the lifting condensation level and the cloud top at the point where rain is observed is adjusted to allow precipitation process to be switched on

    在這個過程中，初始場中降雨區域上空，位於抬升凝結高度與雲頂之間的濕度會予以調整，作用是要啟動降水過程。
  7. Mesoscale low vortex ' s " wandering " at eastern anhui province and stronger development at the stiff moist isentropic surfaces are very important to this heavy rainfall process

    中尺度低渦在安徽東部移動過程中的「打轉」和在等熵面上沿梯度密集等壓線的運動和強烈發展，對這次強降水過程具有重要作用。
  8. The gps data from gps networks in yangtze delta is explored to investigate the improvement of mm5 simulation on rainfall event occurred over meiyu period in 2002 with the aid of initial humidity fields reanalysis and assimulation

    利用建立在長江三角洲地區gps觀測網中gps資料，針對2002年梅雨期間影響長江三角洲地區的降水過程進行了gps資料在mm5中尺度數值預報模式中的應用研究。
  9. Experts from the atmospheric composition observation and service centre of cma say, according to the acid rain observation network, the frequency of acid rain of 19 provinces in china is 100 % in this year ' s rainy season ; the rain in late august in beijing was all acid rain, with a high proportion of strong acid rain, which has never happened since 1993 ; strong acid rain occurred for five times in july when it rained frequently in beijing

    中國氣象局大氣成分觀測與服務中心的專家介紹，酸雨觀測網顯示，今年雨季，全國有19個省市酸雨頻率為100 % ，北京地區8月中下旬的降水過程均為酸性降水，強酸性降水比例很高，而這是自1993年以來觀測中沒有過的，同時， 7月的頻繁降雨中，監測到5次降雨達到強酸性。
  10. Analyses on the first strong precipitation process in 2006 summer in changzhi city

    長治市2006年夏季首次強降水過程分析
  11. The results indicate that in the earlier stage of the development of a hailstorm, an artificial restraint with a common intensity can highly influence the development and precipitation of the hailstorm, increasing its surface precipitation, especially the hailfall amount, but in the later stage of the hailstorm development, the restraint has a small influence on the precipitation

    結果表明，在雹雲發展階段的早期，對雲中上升氣流施加人工抑制將對冰雹雲的發展和降水過程產生明顯的影響，使地面降水量增加，尤其是使降雹量顯著增加；而在雲發展階段的後期，這樣的抑制不會導致地面降水明顯的增加。
  12. This paper firstly applied sequential cluster method to set up the classification standard of precipitation state based on the fact that there are much uncertainty and imprecise characteristics in the precipitation course ; then this paper presented a method which is called markov chain with weights to predicted the future precipitation state by regarding the standardized self - coefficients as weights based on the special characteristics of precipitation being a dependent stochastic variable ; and applied this method to a real hydrological observation station with nearly 50 years precipitation information in shanxi province at last, an ideal result was obtained

    摘要首先基於降水過程存在大量不確定性、不精確性的特點，應用有序聚類的方法建立降水豐枯狀況的分級標準；然後針對降水量為相依隨機變量的特點，採取以規范化的各階自相關系數為權重，用加權的馬爾可夫鏈模型來預測未來降水的豐枯變化狀況；最後以山西省某水文站近50年的降水資料為實例對該方法進行了具體的應用，獲得了較為滿意的結果。
  13. Some kind of precipitation

    某種降水過程吧
  14. Climatic trends of different intensity heavy precipitation events concentration in china

    中國強降水過程時空集中度氣候趨勢
  15. The heating rate of the precipitation process is also adjusted to correspond to the rainfall amount observed

    此外，降水過程的加熱率亦會相應地調整，以符合實況觀測的雨量。
  16. 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。
  17. It is revealed that the heavy rainfall is mainly induced together by the trough at 500hpa, mesoscale vortex at 850hpa and stable mei - yu front at surface

    發現這次強降水過程是在受500hpa低槽、 850hpa中尺度低渦和地面靜止鋒的共同影響造成的。
  18. Under the influence of a weak cold air southward from the north china, some parts of shanghai will see scattered showers from this afternoon to tomorrow

    受北方一股弱冷空氣擴散南下影響，今天下午到明天白天本市將有一次弱降水過程，氣溫有所下降。
  19. On base of the associated explore data of the hefei station and the maanshan station in anhui province and applying the upwards retrieval method that the relatively simple mass continuous equation is used to calculate vertical velocity, to retrieve the three - dimensional construe of the atmospheric wind field, the retrieval construe of the atmospheric three - dimensional wind field and the allocation of the convective system are in reason

    然後再用此反演方法對2003年7月5日發生在安徽省的一次降水過程進行分析，根據安徽省合肥站和馬鞍山站對此次降水過程的聯合探測資料，應用上述質量連續方程求取垂直速度方案反演出大氣風場的三維結構。反演出的大氣三維風場的結構及中尺度對流系統配置基本合理。
  20. 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。
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