鋒生過程 的英文怎麼說

中文拼音 [fēngshēngguòchéng]
鋒生過程 英文
frontogenesis
  • : 名詞1 (銳利或尖端的部分) the sharp point or cutting edge of a sword etc 2 (在前列帶頭的) van;...
  • : Ⅰ動詞1 (生育; 生殖) give birth to; bear 2 (出生) be born 3 (生長) grow 4 (生存; 活) live;...
  • : 過Ⅰ動詞[口語] (超越) go beyond the limit; undue; excessiveⅡ名詞(姓氏) a surname
  • : 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. The result shows that : the sand - dust storm occured in favorable climate background that is drought and rainless, the tilted trough and mongolia cyclone are the important weather systems that caused the severe sand - dust storm, tilted trough and strong frontal zone caused the mongolia cyclone developed and the clod front strengthened at surface, high jet and ferrel circulation are the main reason that momentum spreaded downward from higher level and frontal zone strengthened on lower level

    結果表明:沙塵暴是在乾旱少雨的有利的氣候背景下產的。斜壓槽和蒙古氣旋是觸發這次強沙塵暴天氣的重要的天氣系統,高空斜壓槽和強區促使了地面蒙古氣旋的發展和冷的加強,誘發沙塵暴天氣。高空急流及其下方的ferrel環流起到了高層動量下傳和加強低層區的重要作用。
  2. Analyzing the physics structure of vorticity, divergence, vertical velocity, frontogenesis " function, apparent heat source and apparent moist sink etc. indicated the physics fields are favorable for the occurance of the heavy rain over changjiang - huaihe river basin where the physics values are well according to the heavy rainstorm positions ; the low level jet is closely subject to the moisture and the coupled system of the low and the upper level jetstreams induced the strongly " ascending motion ; the intensity of the frontogenesis varies with the development of the rainfall system and reacts the rainfall intensity

    主要分析了這次中的多種物理量,包括渦度、散度、垂直速度、函數、視熱源、視水汽匯等,對這一暴雨有了比較系統的認識。結果表明:在江淮流域存在著有利於發暴雨的物理量場配置,渦度、散度、垂直速度等物理量,與暴雨的落區都很吻合的;低空急流的產不僅有利於水汽的輸送,而且高低空急流的耦合造成了有利於強上升運動的配置;強度隨著降水系統的發展變化,並影響降水強度。
  3. The above analysis showed that this heavy rainfall event took on obvious meso - scale characters and was the combination of the three flows, so we can deduce : ( 1 ) surface southeasterly wind and topography may play the main role in this event ; ( 2 ) the easterly cold air rushing into the southern shaanxi province in the lower troposphere was strongly relative to the form of surface cold - front type of occlusion ; ( 3 ) there were two reasons for the secondary circulation ' s strengthen in the evening, one was the effect of a mountain - valley wind and the other may be latent heat leading to ascending motion ; ( 4 ) the shape of potential instability stratification corresponded well with the development of the warm - moisture advection ; and ( 5 ) the vapor providing essential thermodynamics was transported by a southwesterly low - level jet from the bay of bengal and the south china sea. furthermore, with the effect of terrain, the southern shaanxi province became the center of this extremely heavy rain process

    中尺度結構分析表明,本次暴雨具有明顯的中尺度特徵,是由三支氣流共同作用的結果,分析發現( 1 )地面東南風和地形在這次大暴雨起主要作用; ( 2 )東路冷空氣主要是通中低層侵入陜南地區的,並與地面冷式錮囚的形成密不可分; ( 3 )夜博士論文:中尺度地形對陜南暴雨的影響研究間垂直次級環流發展加強可能有兩個原因,一個是由於地形山谷風的作用,另一個是降水的潛熱釋放激發了上升運動: ( 4 )位勢不穩定層結的形成與低層暖濕平流的發展有很好的對應關系; ( 5 )本次暴雨的水汽主要靠偏南風急流將孟加拉灣和中國南海的水汽輸送至西北地區東部,為暴雨的發提供了必要熱力條件。
  4. Based on t213 and other observational datasets, a severe heavy rain occurred in changjiang - huaihe basins during 4 - 5 july 2003 is studied. the primary diagnostic analyses show that double or single block is the characteristics of the macroscale circulation in this rainfall process. the strong conflict of warm and cold mass, mesoscale convergence on meiyu front, shear line, and stably maintaining of high and low jets make for the rainfall

    本文採用地面高空常規資料,每6h一次的降水資料,以及t213數值預報資料,對2003年7月4 - 5日發在江淮地區的一次梅雨暴雨的影響系統及其可能機制進行了初步的診斷分析,發現,高緯雙阻、單阻形勢是這次暴雨的大尺度環流特徵;冷暖空氣的激烈交、梅雨上的中尺度輻合線、 700hpa 、 850hpa上的低渦、切變線以及穩定維持的高低空急流是導致這場暴雨的直接影響系統;該地區維持一個高能、飽和、潛在不穩定的環境,有利於特大暴雨的產和維持。
  5. 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、青海湖錮囚以及中尺度低壓、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,中心強度減弱,降水結束。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。
  6. The first diagnostic analyses show that the heavy rainfalls are produced together by vortex, shear line and upper and lower jets, meiyu front. the condition of high energy, saturation, potential instability is propitious to the form and maintenance of heavy rainfall. the result of numerical simulation by mm5 model shows that heavy. rainfall has close relation with meso - scale vortex pole and strong convection

    採用ncep全球譜模式和常規觀測資料對「 03 . 7 」江淮地區的兩次暴雨的影響系統及其可能機制進行了初步診斷分析,發現梅雨暴雨是受低槽、低渦、切變線、高、低空急流和梅雨區共同影響造成的,該地區維持高能、飽和、潛在不穩定的環境,有利於暴雨的產中尺度數值模式( mm5 )模擬結果表明梅雨暴雨與中尺度渦柱、強對流運動密切相關。
  7. Organic c in the soil profiles were measured as in total and fractionated into microbial biomass - c, water - soluble organic - c, light - fraction organic - c, and heavy - fraction organic - c. the amounts of microbial biomass - c, and water content in soil profiles were consistently analyzed. the aim of this study was to investigate interactions between the accumulation of soil organic c and vegetation successions in the region, in a purpose to improve understanding on how changes in soil conditions affect vegetation successions in the region

    分析植被演替各個群落(棄耕地先群落、草本群落、灌叢群落、早期森林群落、遼東櫟群落) 0 50cm深度內土壤有機碳、微物碳、水溶性有機碳、輕組有機碳、重組有機碳的變化規律及相互關系,初步探討了植被正向演替中土壤有機碳的積累與變化規律。
  8. Next, the round robin test progress report and explanations of the up - coming schedule of activities by the head chairman, mr. ishii of pioneer corporation was made

    在這之後,循環對比試驗首席代表石井先株式會社作了試驗報告與今後日安排的說明。
  9. The result shows that the dynamic field and thermodynamic field in the zone of the meiyu front have obvious meso - scale structure characters, the meiyu frontal rainfall is caused by a series of meso - scale convective systems in the zone of meiyu fron t, the dynamic field and thermodynamic field corresponding to the meso - scale convective systems take on evident meso - scale structure, the structure of the dynamic field and thermodynamic field will adjust correspondingly in the course of the development of the meso - scale convective systems, what ' s more, the adjustments and the changes of the physical parameters will restricted the development and transformation of the meso - scale convective systems in reverse

    試驗結果表明,梅雨帶內的動力、熱力場具有明顯的中尺度結構特徵,梅雨降水是由梅雨帶內的一連串中尺度對流系統造成的,中尺度對流系統對應的動力場、熱力場均呈明顯的中尺度結構,中尺度對流系統發發展中,其伴隨的動力、熱力場結構均會作相應的調整,這些物理量場的調整和變化又制約了中尺度對流系統的發展變化。
  10. The condition of high energy, saturation, potential instability benefits for the form and maintenance of this rainfall. the mesoscale numerical model mm5 ( v3 ) is used to simulate the heavy rain process

    採用ncep全球譜模式資料,利用中尺度數值模式mm5 ( v3 )對2003年7月4 - 5日發在江淮地區的一次梅雨暴雨進行數值模擬。
  11. In the prune if cultural and educational reform in modem china, " absorbing western technology on the basis of the chinese traditional system " has the epoch - making significance in changing traditional education and abolishing eight - legged essay to select scholars for public office system

    摘要鴉片戰爭以後,中國在政治、軍事、經濟和文化教育等各個領域都面臨著深刻的危機,西方思想文化與中國傳統文化發了激烈的交在近代中國文化教育轉型中, 「中體西用」對于改變傳統教育的空疏之風,打破八股取士制度的禁錮具有劃時代意義。
  12. In this endeavour, i would like to thank ms winnie yuen and mr po fung for providing supplementary information, ms tong ka - wai for verifying the variants in source content of cantonese opera films and their originals, and ms liu suet - wan for verifying the titles of original sources which in turn provide an insight into the transformation of literary adaptations by the film medium

    中感謝阮紫瑩小姐蒲提供補充資料和意見,唐嘉慧小姐專就粵劇片方面進行覆核,廖雪雲小姐就文學方面查證有關原著的名稱,藉以顯示電影內容的源頭和素材及其轉化。
  13. 2 ) the analyse of the structure of mei - yu low and the elationship between the low and rainfall three lows moved along the mei - yu front towards the northeast during mei - yu period in 1999, which produced three intensive rainfall periods along the yangtze river : ill the station of huangshan, the most heavy rainfall center, totally had 850mm rain during 11 days. the reason for the heavy rainfall was the sustaining moisture supply from the south, and the deep moist layer and the high relative humidity in the south - east quadrant

    2 )梅雨低渦的結構及其與降水關系分析1999年在梅雨上有三個梅雨低渦相繼在其上產,冰箱東北方向移動,分別對應著長江中下游的三次強降水:最大降水中心黃山11天累計降水量達到850mm ,為梅雨期間平均降水量的150以上。低渦之所以產這么大的降水和降水強度是因為低渦在移動中不斷有水汽輸入和補充,在其東南象限對流層中低層維持了深厚的濕層和很高的相對濕度。
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