江淮梅雨 的英文怎麼說

中文拼音 [jiānghuáiméiyǔ]
江淮梅雨 英文
changjiang-huaihe river valley meiyu
  • 江 : 名詞1. （大河） （large） river 2. （指長江） the changjiang [yangtze] river 3. （姓氏） a surname
  • 淮 : 名詞1. （淮河） the huaihe river （我國大河之一, 全長1000公里）2. （姓氏） a surname
  • 梅 : 名詞1. [植物學] （薔薇科落葉喬木） prunus mume; plum 2. （梅花） plum blossom3. （梅子） plum4. （姓氏） a surname
  • 雨 : 雨名詞（從雲層中降向地面的水） rain
  • 梅雨 : [氣象學] mould rains; plum rains
  1. ( 5 ) there exists close relationship between the meiyu period precipitation in jianghuai valleys and the anomalies of subtropical summer monsoon, the anomalies of cold air, not the same so the indian summer monsoon

    （ 5 ）江淮地區梅雨期降水與東亞副熱帶季風、北方冷空氣異常密切相關，與印度西南季風關系並不密切。
  2. The storm rainfall during the jianghuai meiyu period is one of china ' s representative meteorologic disasters

    江淮梅雨暴雨是我國典型的氣象災害之一。
  3. Extremely heavy meiyu over the yangtze and huaihe valleies in

    1931年江淮異常梅雨
  4. Besides, aao has a leading influence on easm

    此外，南極濤動對我國江淮夏季降水尤其是梅雨有重要影響。
  5. To the large - scale atmosphere, we separate the terms of the horizontal vorticity converting into the vertical vorticity, which considered as the baroclinic terms, from the terms that not including horizontal vorticity by the rules of the p coordinate transforming to the z coordinate in the traditional vorticity equation, and carry out the scale analysis, and then conclude that the baroclinic terms are able to reach the same magnitude grade as the partial derivative of the vertical vorticity to time when it takes place the large scale precipitation in the summer monsoon period in china. by analyzing the game reanalysis data from april to august in 1998 in the region of chinese continent, we found that the baroclinic terms is important to the large - scale cyclone developing above the 600hpa, and the magnitude changing of the baroclinic terms is nearly in - phase as the monsoon movement, so which imply exactly that the magnitude changing of the baroclinic terms is the one of the natural characters of the summer monsoon evolution and equivalent to the movement rule of the subtropical high of the western pacific

    在p坐標垂直渦度方程中，利用p坐標向z坐標轉換的公式將水平渦度向垂直渦度轉化的所有項分離出來，這些項具有明顯的斜壓特徵，對其進行尺度分析后，得出在可以忽略潛熱釋放對渦度影響的對流層中、高層，此轉化項是大尺度斜壓渦度發展的重要項。通過對1998年48月的game再分析資料進行實際計算也發現，轉化項在東亞夏季風上升支的600hpa及以上層次對垂直渦度的局地變化貢獻很大，不能忽略。同時發現水平渦度向垂直渦度的轉化在南海季風爆發時和江淮梅雨入梅及發展過程中均有指示性意義，在南海季風爆發以後，在中國東南部地區，轉化項的大小與夏季風的活躍和中斷等活動有著幾乎一致的變化規律，這從側面也指出了，此轉化項的變化是夏季風演變所具有的本質特徵，並且它反映出了西太平洋副高在中國大陸的活動情況。
  6. 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。
  7. The institute concentrates on the study of forming mechanism, physical process, forecasting technology of mesoscale heavy rain especially jianghuai meiyu front rain gush or heavy rain in prefrontal warmer area

    研究重點是我國陸地暴雨，特別是江淮梅雨鋒暴雨和鋒前暖區暴雨，同時開展我國北方暴雨的比較研究。
  8. Numerical study on the genesis and development of the low vortex - rain gush system on a jianghuai meiyu front

    江淮梅雨鋒強暴雨低渦系統發生發展的數值研究
  9. Diagnostic analysis and numerical simulation of the meso - scale system during quot; 03. 7 quot; meiyu frontal rainstorm event

    江淮梅雨鋒暴雨中尺度系統的數值模擬研究
  10. ( 7 ) there is a apparent positive correlation between the meiyu period precipitation in the north region and ssta ( 1 - 2 monthly averaged in present year ) in the " key regions " ( 44 - 50 n, 152 - 166 e ) of north pacific ocean

    （ 7 ）江淮北區梅雨期降水與當年1 - 2月勘察加半島以南的海域海溫有較好的正相關關系。江淮北區以北地區和key區（ 44 50 n ， 152 166 e ）為耦合相關的顯著部位。
  11. Firstly, the resault of daily calculation about all kinds of potential instability parameter in a month show that, as a vertical integral potential instability parameter, cape ' s daily variation corresponded to the severe convective storms " occurrence

    首先，逐日計算2003年江淮梅雨期的各種位勢穩定度因子，結果表明， cape屬於垂直積分穩定度指數，其日變化與強對流風暴的發生有較好的對應關系。
  12. 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過程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、低空急流和梅雨鋒區共同影響造成的，該地區維持高能、飽和、潛在不穩定的環境，有利於暴雨的產生中尺度數值模式（ 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。
  13. 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日發生在江淮地區的一次梅雨鋒暴雨過程進行數值模擬。
  14. On the basis of the typical weather situation in huaihe river basin in 1998, the paper analyses the features of the land temperature of huaihe river basin in the four stages of the 1998 s meiyu of yangtze

    最後結合1998年淮河流域試驗加密觀測期間的主要天氣形勢，分析了江淮梅雨4個階段相對應的地面溫度的特徵。
  15. Using the new generation mesoscale model of the weather research and forecast ( wrf ) model, the mesoscale numerical simulation of the heavy storm rainfall of the jianghuai mei - yu front during 4 july 2003 was carried out

    利用美國新一代中尺度天氣和研究數值模式（ wrf ） ，對發生在2003年7月4日的江淮梅雨強暴雨過程進行了數值模擬。
  16. In contrast, there is less rainfall with a shorter period when aao is weaker. aao is therefore an important interannual signal influe ncing summer rainfall especially the mei

    因此，南極濤動是一個能夠對中國夏季降水尤其是梅雨異常產生重要影響的年際變化強信號，對江淮梅雨的預報也有重要意義。
  17. Currently, many meaningful researches about continual heavy rainstorm during the meiyu period have been done by domestic and foreign meteorologists and a lot of meaningful results have been achieved

    目前我國和國外的許多氣象學者對江淮梅雨暴雨曾作了大量有意義的工作，取得了許多積極的成果。
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