convective cloud 中文意思是什麼

convective cloud 解釋
對療
  • convective : adj. 1. 有傳送力[運輸力]的，傳送性的。2. 【物理學】對流的。
  • cloud : n 1 雲。2 雲狀塵埃、煙（等）；（鳥、蟲、飛機等的）大群，大隊。3 （水晶等的）霧斑，（鏡子等上的）...
  1. The brightness temperature is highly related to the density of ice hydrometeor. since the convective cloud system is tilted, and the viewing angle is oblique, the area displacement between ice hydrometeor and the surface rainfall rate makes the relation between tb and surface rainfall rate is relatively small

    但亮溫和地面降水強度之間的相關性較弱，這是由於該對流系統為傾斜的，冰相粒子和地面降水強度之間存在著位置上的不一致，並且觀測角為傾斜的。
  2. The tbb ( black - body temperature ) analysis depicts that several meso - p - scale cloud clusters and convective cells are embedded and alternately developed within a mcc

    （ 2 ）梅雨鋒中的mcc內嵌有若干個中-雲團，對流體此生彼消十分活躍。
  3. In an unstable and moist atmosphere, water droplets and ice pellets in the cloud will become electrically charged in convective motion

    在不穩定及潮濕的大氣中，雲層內的水滴及冰粒在對流活動中產生電荷。
  4. From the courtyard boarded layers level, is the main hall of nanyan palace ruins, 36 stone carving pillars on the construction of convective cloud patterns still visible when the grand scale

    從院落登上層層臺階，是南巖宮大殿遺址， 36座精雕石柱上有石雕流雲瓊花圖案，仍然可見當年宏偉規模。
  5. In addition, a thought of how to use the mesoscale convergence center, tbb of convective cloud and the radar echo for rainfall rate to predict the mesoscale rain cluster is presented

    提出利用逐時的中尺度輻合中心、衛星紅外雲圖雲頂亮溫及雷達回波降水率做中尺度雨團量級預測思路。
  6. These mean images reveal not only the synoptic cloud systems but also the mesoscale convective cloud cluster. the long - term high water level of mid - yangtze river and the frequent flood peak of the upper yangtze river from the middle of june to the middle of august in 1998 was caused by the high frequent activity of convection

    旬月和季平均雲圖表明，長江上游從6月中旬開始到8月中旬長達兩個多月對流的頻繁發生是「 98洪水」長江上游洪峰多，中游高水位維持時間長的重要原因。
  7. 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。
  8. The results show that unbalance force of atmospheric motion and the coupling reaction among convective cloud cluster and moisture frontal zone and low level jet lead to the continuation of strong convergence in low layer and the maintenance of torrential rain

    分析結果發現，大氣運動非平衡強迫、凝結降水的非均勻分佈與強烈垂直風切變的耦合作用、 「濕度鋒」與低空急流的耦合相互作用通過促進低空輻合流的維持，導致了對流雲團和暴雨天氣的持續。
  9. 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。
  10. The cloud model gives a complete structure of the partical microphysics of a convective cloud system over chinese mainland

    雲模式給出了中國陸地上兩個對流系統的粒子微物理特徵的完整結構。
  11. A severe convective storm accompanied with severe wind, heavy rain and hail on 23 august 2001 in beijing was simulated by mm5 initiated with ncep reanalysis data and a three - dimensional cloud model with hail - bin microphysics, which was initiated with the air soundings at beijing at 20 : 00 on 23 august 2001, and some comparisons were also made between the simulated and natural storm

    首先利用中尺度非靜力平衡模式（ mm5 ） ，模擬了2001年8月23日北京一次伴有大風、暴雨、冰雹的強對流天氣發生發展的中尺度背景場，並根據mm5的輸出結果分析了此次大風發生發展過程。
  12. Through the analysis of 11 typical mesoscale convective systems occurring at china continent and adjacent ocean on june, july and august, 1998, it is found that 10. 65ghz v channel and 19. 35ghz v channel can well response to the absorbability and emission of liquid water in cloud and precipitation, and that 85. 5ghz v channel and 37. 00ghz v channel can response to the ice scatting in cloud well

    通過對1998年68三個月內發生在我國大陸和鄰近洋麵上的11個中尺度對流系統的分析，發現10 . 65和19 . 35ghz垂直通道能較好的反應雲中液態水和降水的吸收和發射85 . 5和37 . 0ghz垂直通道能較好的反應雲中冰晶冰粒的散射。
  13. Cumulus is also a convective cloud by virtue of the strong upward current inside it

    由於積雲內上升氣流非常旺盛，故積雲亦稱對流雲。
  14. It usually involves a fast rotating column of air extending from the base of a convective cloud to the water surface

    它通常有一條快速旋轉的漏斗狀雲柱，由對流雲底部下伸至水面。
  15. A waterspout is a fast rotating column of air ( made visible by water droplets in the cloud ) extending from the base of a convective cloud to the water surface

    水龍卷是一個快速旋轉的雲柱（由於水滴的存在而變得明顯） ，由對流雲底部下伸至水面。
  16. The three - dimensional convective storm numerical model system is based on the three - dimensional convective storm model ( csm3d ) developed in the institute of atmospheric physics ( 1ap ), chinese academy of sciences. this system is an interactive system running in windows operating system and can be used in severe convective cloud numerical simulation and numerical forecast in the system designation, software is programmed in vc + +, fortran and grads. mixed - languages programming ( vc + + and fortran ), multithreading programming, vc + + interface programming and windows shell programming are applied

    使用visualc + +和fortran語言以及grads等軟體，利用vc + +和fortran混合語言編程技術、 visualc + +界面編程技術、 windowsshell編程等多種編程技術，基於多線程程序設計思想，將原來的基於dos操作系統的強對流雲數值模式系統移植到windows操作系統下，理順了原系統各個模塊之間的邏輯關系，建立了具有windows風格的友好界面，本系統操作簡單直觀，交互性好，方便使用者的操作。
  17. The residual effects of the cloud clusters are generally ignored even though the area they cover is perhaps an order of magnitude larger than the convective region itself

    雲團的殘余影響通常是忽略不計的，即使它們覆蓋的地區比對流區本身可能大一個量級也如此。
  18. In this study, the mechanism of the severe convective storm accompanied with severe wind was investigated using both mm5 and a hail - bin cloud model

    本文主要研究了產生災害性大風的強風暴的形成環境與機理。
  19. In this paper, firstly large - scale air circulation and weather system evolution are analyzed, and get the scale feature and spread process of the meso - scale convective system by analyzing time - space layout of precipitation and satellite cloud maps. the lower resolution of t213 model and less time - space resolution of data were responsible for the above mentioned misforecast. in this study, the event is simulated by mm5v3. 6 with two - way - interaction and triple nested grid

    分析並指出了此次過程中對流降水的演變規律：對流活動引起的高層重力波和邊界層冷涌是對流傳播和觸發大暴雨中心對流活動的主要機制，地面冷空氣的侵入，引起邊界層暖濕空氣的交匯和強烈輻合是對流活動顯著加強的原因。
分享友人
分享到 Line

分享到臉書