convective precipitation 中文意思是什麼

convective precipitation 解釋
對獵降水
  • convective : adj. 1. 有傳送力[運輸力]的，傳送性的。2. 【物理學】對流的。
  • precipitation : n. 1. 猛然摔下，落下。2. 猛沖；急躁，輕率，魯莽。3. 【化學】沉澱（作用）；降雨（量）；（雨、雪等的）降落。
  1. The result indicates that, in the course of the rainstorm in huoshan, there are obvious low - level jet of great intensity, infection of mesoscale shear line, enhancement of plus vorticity which increases intensity of convergence, improves ascending velocity and brings on precipitation, and quick enhancement of helicity which provides the basis to forecast, in addition, convergence of moisture flux and analyzed potential vorticity which reflects baroclinic convective instability sufficiently indicate the characteristics of the rainstorm

    結果表明：此次霍山暴雨發生前後，存在明顯的大強度低空急流，並受到中尺度切變線的影響，而且正渦度的加強引起了輻合加劇，提高了上升速度從而引起降水，同時暴雨發生前螺旋度的迅速增強，也為預報提供了根據，另外水汽通量的輻合以及分析位渦反映出的斜壓對流不穩定都充分體現了這次降水的特點。
  2. Orographic influence on precipitation of a meso - scale convective system over taiwan on 7 - 8 june

    8日中尺度對流系統降雨的影響
  3. While the precipitation of southeast of inner - mogolio is attributed as the strong convective precipitation, the rainfall of liaoning and northeast of heilongjiang is induced by subtropical high and westerly trough, and that of west of heilongjiang is influenced directly by vortex in upper air

    各區域產生極端降水的天氣背景也不相同：內蒙古東南部的降水是前傾槽引起的強對流降水天氣，遼寧和黑龍江東北部的降水是由於副熱帶高壓和西風槽的共同作用引起的。黑龍江西部的降水是由於高空渦的直接作用引起的。
  4. Rainfall and vertical profile of hydrometers are retrieved for land and ocean using tmi 1b11 data. the comparison of retrievals of gprof v6. 1 and v6. 2 with ground - based radar and gauge data on land and pr data on ocean show that the gprof - v6 algorithm can retrieve rain intensity much well and indicate vertical distribution of hydrometers mainly. as far as retrieved precipitation area, it is better for convective precipitation type than stratified precipitation type

    將陸地的反演結果與地基雷達資料和地面雨量計資料進行比較，海洋的反演結果結合trmmpr的降水產品進行比較，結果表明： gprof - v6演算法反演的降水產品可以較好地反映降水強度並反映降水的主要垂直結構；在落區方面，對流降水反映較好，層雲降水則較差；雲-輻射數據集的擴充與改進可提高反演精度。
  5. 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。
  6. 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。
  7. By mesoanalysis of a precipitation that occurred in the middle reaches of the changjiang river, 8th jul. in 2003, the formation and development of the event, its relation with the meso - microscale system are studied, it is emphasized that the low - level jet would cause favorable thermodynamic, moisture and dynamic conditions for the heavy rainfall in the middle reaches of the changjiang river and that the mesoscale vortex formed in the left of the low - level jet would stimulate strong convective clouds and cause the heavy rain

    摘要通過對2003年7月8日發生在長江中游的一場大暴雨進行中尺度分析，初步研究了暴雨的形成及發展過程，總結了暴雨的產生與中小尺度系統的關系，著重闡述了低空急流在暴雨形成中的作用，以及在低空急流左側強正渦度中心附近形成中尺度渦旋，激發暴雨雲團等。
  8. 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。
  9. 2 ) because the si mainly reflect the information of ice layer above the precipitation, si > = 60k is a good index of strong convective precipitation

    2 ）由於si主要對應的是降水層上部冰晶層， si與強對流性降水有很好的相關， si ? 60是一個好的暴雨指標。
  10. It ' s also found that the reanalysis influences the results of 6h accumulated precipitation through changing the non - convective precipitation prediction mainly, while results improved by the nudging assimulation are substantially associated with convective precipitation change

    總體上，應用gps可降水量資料調整模式濕度初始場對6h累積降水預報效果的改善優于連續nudging同化對6h累積降水預報效果的改善。
  11. The analyses suggest that the first and second categories of rainstorms are associated commonly with the strong inertial instability in the upper troposphere, as well as respectively with symmetry and convective instabilities, and their rainfall is large ; and the third and fourth categories generally produce stable precipitation with a small rainfall, and their upper tropospheres are usually inertially stable

    分析濕位渦與梅雨暴雨中的慣性不穩定、對稱不穩定、對流不穩定的關系發現：第1類暴雨往往與對稱不穩定有關，第2類暴雨與對流不穩定有關，且這兩類暴雨高層多具有強慣性不穩定，降水相對較大；第3 、第4類暴雨是穩定性降雨，高層一般不具備慣性不穩定，雨量一般較小。
  12. 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。
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