特大暴雨 的英文怎麼說

中文拼音 [tèdàbàoyǔ]
特大暴雨 英文
extraordinary storm
  • 特 : Ⅰ形容詞（特殊; 超出一般） particular; special; exceptional; unusual Ⅱ副詞1 （特別） especially; v...
  • 暴 : Ⅰ形容詞1 （突然而且猛烈） sudden and violent 2 （兇狠; 殘酷） harsh and tyrannical; cruel; fierce...
  • 雨 : 雨名詞（從雲層中降向地面的水） rain
  • 特大 : especially [exceptionally] big; the most
  • 暴雨 : torrential rain; rainstorm; hard rain; intense fall; squall; downpour; gush暴雨放大 storm maximiz...
  1. It was the vane on the roof turning round and this change in the wind was the signal for a disastrous rain.

    這是房頂上的風標在轉動，風向的這種變化，就是一場特大暴雨的信號。
  2. The amount of daily rainfall was over 88 mm on august 12

    災害主要原因是特大暴雨激發所致。
  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過程起主要作用； （ 2 ）東路冷空氣主要是通過中低層侵入陜南地區的，並與地面冷式錮囚鋒的形成密不可分； （ 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，為暴雨的發生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日發生在江淮地區的一次梅雨鋒暴雨過程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過程發生的大尺度環流特徵；冷暖空氣的激烈交鋒、梅雨鋒上的中尺度輻合線、 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生和維持。
  5. The weather analysis and climatic characteristics of the heavy - hard rainfall in this area, structure characteristics during the rainstorm, the mechanism and structure of mesoscale systems bringing rainstorm and etc. are studied by conducting diagnostic analysis, theory of dynamics and numerical simulation. the influence on the rainstorm causing by mesosc ale topography piling on the plateau, the particular valley topography in northeast plateau and complex surface vegetation are researched by numerical experiments

    本論文試圖採用診斷方法、診斷和天氣動力學理論相結合的方法、數值模擬等方法對高原地區大到暴雨的天氣、氣候特徵，暴雨產生時的物理量場特徵、產生暴雨的中尺度系統的發生機理和結構特徵等方面進行研究，對疊加在高原上的中尺度地形、高原東北部特殊的外流河谷地形及復雜下墊面性質對暴雨的可能影響進行數值試驗，以揭示高原暴雨發生發展的物理機制。
  6. Using satellite cloud pictures and data from the intensive and conventional observation, the reason of the heavy rainfall event on 16 - 17 july 2004 over shah river area is studied

    摘要應用常規、加密氣象資料及衛星雲圖，分析了2004年7月16 ~ 17日沙澧河流域特大暴雨成因。
  7. Strange assassination cases of two heads of state

    川北兩次特大暴雨天氣過程成因的對比分析
  8. Contrast analysis of two heavy rain cases over northern sichuan basin

    川東北兩次特大暴雨過程對比分析
  9. Mathematical simulation of rainstorm waterlogging on quot; 030704 quot; in nanjing city

    南京市特大暴雨內澇災害的模擬模擬
  10. Experiments for the case of the rainfall occurred in the changjiang river during 9 - 10, july, 2003, are carried out

    對2003年7月9日至10日發生在我國長江流域的一次特大暴雨天氣過程用mm5模式進行了數值模擬。
  11. The 5 - day mean and daily mean images show that the long severe rainfall of yangtze river was produced by the meso -

    候和日平均雲圖表明，降雨雲帶上頻繁產生中尺度暴雨雲團造成了7月下旬長江中游連續出現特大暴雨。
  12. A total of 3000 kg fish was killed in the li wan lake by flood caused by a heavy rain in guangzhou, august 9, 2005

    2005年8月特大暴雨期間，受珠江水位提高城內河涌泄洪不暢的影響，荔灣湖3000多公斤鮮魚被倒灌的污水活活嗆死。
  13. At least three others are missing. forecasters say the storm could drop another 20 inches of rain before heading northwest toward the bahamas

    氣象預報顯示在轉向巴哈馬群島西北前，暴風雨還將帶來20英寸（換算成500毫米，特大暴雨了）高（ ）的降雨。
  14. The persistent downpour in chifeng since the start of the rainy season has caused a severe flood disaster rarely seen in history. the heavy casualties and damage to personal possessions and local farming include 3. 85 million acres of farmland submerged, over 70, 000 houses destroyed, and 1. 62 million people affected with more than 60, 000 homeless

    今年入汛以來，我市由於連降大暴雨，遭受了歷史罕見的特大洪澇災害，給人民群眾生命財產和農牧業生產造成嚴重損失，致使385萬畝農作物被沖淹， 162萬人受災，倒塌民房7萬多間， 6萬多人無家可歸。
  15. The analysis of dry pv shows that the high pv dominate the area of typhoon, the higher is the center value of pv, the stronger is the typhoon. lt is also shown that the most important reason resulting in rainstorm is the cold air ( high pv ) which spreads to south from the upper troposphere or lower stratosphere and transports into the warm air. the joining situation of upper and lower pv area make vortex develop. pv transpotation reduces static stability, which increases the releasing of instability energy and makes rainstorm amplify

    對干位渦的分析表明：臺風或臺風環流區為高值位渦區，臺風越強，位渦中心值越大；對流層上部或平流層下部冷空氣（高位渦）的擴散南下與暖濕氣流的交匯是造成特大暴雨的重要原因，因為上游斜壓性的發展使對流層頂發生折疊，平流層與對流層相互作用增強，上下位渦區相接的形勢使低層渦旋發展，上升運動加強，位渦的下傳有效地降低了靜力穩定度，有利於位勢不穩定能量的釋放，使得暴雨增幅。
  16. The results show that the event is directly affected by the formation and evolution of southwest vortex and mcc cloud cluster which locate in the intersection region of the upper - level jet and the low - level jet

    結果表明：高、低空急流耦合區中西南低渦及mcc特徵雲團的形成和維持是造成此次特大暴雨的直接影響系統。
  17. The mesoscale model mm5 was successfully used to simulate the rainstorm caused by the weaken 9907 typhoon circulation in shandong province during 11 - 12 auguest 1999. based on the outputs of the model, the mesoscale vertical structure of regular physical variables was analyzed

    本文利用非靜力中尺度模式mm5對1999年8月11 12日由冷空氣侵入臺風低壓環流造成半島西部和魯東南特大暴雨過程成功地進行了數值模擬。
  18. On july 8th, gongbei customs sent 80, 000 yuan rbm contributed by all the customs staff to zhuhai charity society, presenting their love and concerns to the people suffered from severe storms and floods

    拱北海關8日將全關幹部群眾捐獻的8萬元人民幣送到市慈善會，向我市遭受特大暴雨、洪災的群眾送上一份愛心。
  19. The assimilation experimentation results indicate that after assimilating radar wind field of small spatial scale, mesoscale and small - scale precipitation prediction can be improved and mesoscale and small - scale information which ca n ' t appear by tradition datum can be gained, which is valuable to analyze the mesoscale and small - scale system structure ; the effect assimilating radar humidity field is n ' t obvious, which is perhaps correlation with precipitation types and assimilating time. the results also show that adding radar humidity field to initial condition at initial time can supply the gap of the regular data in reflecting the mesoscale and small - scale systems, strengthen the humidity in the initial field, and eventually help to improve precipitation. the experiment of assimilating radar wind field and radar humility field at the same time shows that vapor transportation and local vapor divergence play more significant role in causing excessively heavy rain than only high wet center

    同化試驗結果表明：同化空間解析度很高的雷達風場后，能改善中小尺度降水的預報效果，並且能夠得到常規觀測資料所不能得到的中小尺度信息，對分析中小尺度系統結構具有重要意義；同化雷達濕度場效果不明顯，可能與降水類型和同化時刻有關；而直接在初始時刻加入雷達濕度場，補充了常規資料在反映中小尺度系統方面的不足，增強了初始場中的水汽，有利於降水量的增加；同時同化雷達風場和雷達濕度場的試驗表明，水汽的輸送和局地的水汽輻合對于產生特大暴雨的貢獻遠大於僅有高濕中心的貢獻。
  20. This scheme was finally tested by a typical meso - scale severe rainstorm process which happened on the middle - lower parts of the yangtze river in china during the period of july 4th - 5th, 2003

    並以2003年7月4日? 5日發生在江淮流域的特大暴雨過程為例，對該方案進行了驗證。
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