梅雨梅雨 的英文怎麼說

中文拼音 [méiyǔméiyǔ]
梅雨梅雨 英文
bai-u
  • 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. 1 ) the analyse of mei - yu front structure there is stable mei - yu front along the middle and lower reaches of yangtze river during the mei - yu period in 1999. the temperature contrast in the low level of mei - yu front almost disappeared, which existed only in the upper level. so the mei - yu front is " footless " from the temperature field

    得到的基本結果如下： 1 ）梅雨鋒結構的分析1999年梅雨期間，在長江中下游維持著穩定的梅雨鋒，梅雨鋒在低層的溫度對比幾乎消失，只存在於對流層中上層，因此從溫度常看梅雨鋒是一種「無腳鋒」 ，在對流層中上層具有上寬下窄的梅雨鋒機構。
  2. In this paper, four cases of heavy rainfalls and snowfalls in china are simulated by using mm5. cloud microphysical characteristics and sources of rain, snow and graupel have been particularly studied

    運用中尺度非靜力數值模式mm5v3 ，對我國華南前汛期暴雨、梅雨鋒暴雨、北京東風迴流降雪和遼寧寒潮大風雪等四次過程分別進行了模擬研究。
  3. ( 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。
  4. 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。
  5. Things easily get mildewed in the rainy season. .

    梅雨季節東西容易發霉。
  6. Adopting high resolution nested grid project and proper physical parameter, a mei - yu heavy rain process during eight july 22, 2002 and eight july 23, 2002 and the meso - b - scale systems alongwith it, were simulated by use of psu / ncar meso - scale nonstatic numerical forecast model mm5 in this paper. the simulation result describes successfully the spatial and temporal distribution of this rain process and the developing course of the concomitant meso - ? - scale systems

    本文利用psu ncar的中尺度非靜力數值預報模式mm5 ，採用高解析度套網格方案和適當的物理過程，對2002年7月22日08時到23日08時的一次強梅雨暴雨過程和伴隨的中-尺度系統進行了數值模擬，結果很好地描述了本次暴雨降水的時空分佈及相伴隨的中-尺度系統的發生發展過程。
  7. Below 600hpa, the front of east asia was mei - yu front ; mei - yu equatorial front and polar front from the south to the north ; while above 600hpa, there was only mei - yu front. upon these conclusions, we put forward a conception model of east - asia front

    在600hpa以下，東亞地區的經向方向鋒區從南到北依次表現為梅雨鋒，梅雨赤道縫和極鋒；而在600hpa以上，只是極鋒型的梅雨鋒的單一結構。
  8. When the intensity of meiyu increasing, the continental low in the northwest of meiyu rainband is getting stronger and the west pacific subtropical high is getting weaker

    當梅雨強度增大時，梅雨西北部的大陸低壓加強而西太平洋副熱帶高壓減弱。
  9. 3. the correlation between the precipitation total for meiyu and the summerly precipitation in sichuan ( the areas of southeast china along sea ) are negative. in the years of much precipitation total for meiyu, the center of anticorrelation lies in chengdu ( fuzhou ) ; and in the years of less precipitation total for meiyu, the center of nagative correlation extends southeastwards from chengdu, and in the areas of southeast china along sea, the center of nagative correlation also lies in fuzhou

    3長江中、下游地區梅雨量與四川盆地、東南沿海地區夏季降水也存在顯著的負相關聯系；四川盆地多梅雨年相關中心在成都附近，少梅雨年相關中心推向東南方向的樂山附近；東南沿海地區負相關中心多、少梅雨年份均在福州附近。
  10. We also analyzed the relation between the precipitation for meiyu and the summerly precipitation in sichuan, the areas in southeast china along sea. the main results show as following : 1. the correlation between the precipitation total for meiyu and the summerly precipitation in the east of nw china are negative. in the years of much precipitation total for meiyu, the center of anticorrelation lies in tianshui ; and in the years of less precipitation total for meiyu, the center of nagative correlation extends northwestwards from tianshui

    主要結果歸納如下： 1梅雨量與西北地區東部夏季降水量之間存在反相關。即梅雨量特多的年份，西北地區東部夏季乾旱；反相關的中心位於甘肅省中部地區的天水附近。梅雨量特少年份，西北地區東部夏季降水偏多；反相關中心位置從天水向西北方向推移。
  11. The ncep / ncar global reanalysis data about 55 yean ; ( 1948 - 2002 ), the observed data about 2 years ( 1999 - 2000 ), the meiyu data in the mid - lower reaches of the yangtze river and the precipitation data at 160 stations in china duing 1951 to 2000 are used in the paper. we present a preliminary study on the relationship between the precipitation total for meiyu and the summerly precipitation in the eastern side of the northwest china. then using nonhydrostatic version mm5 with one nested grid, the effect of the circulation patterns for meiyu on the summerly precipitation in the eastern side of the northwest china was simulated by numerical simulation of full physics

    本文採用1948 2002年ncep再分析資料、 1999 2000年的全球地面、高空觀測資料、 1951 2000年梅雨以及全國降水量資料，初步研究了長江中、下游地區梅雨事件與西北地區東部夏季降水的聯系，並用mm5中尺度非靜力模式模擬了多（少）梅雨環流型對西北東部夏季降水的影響；另外，還分析了梅雨與四川盆地、東南沿海地區夏季降水的聯系。
  12. Because meiyu rainstorm happens quickly, predicts in short time and often causes disaster. so study on the mechanism of mesoscale rainstorm system has a great value

    由於梅雨暴雨突發性強、預報時效短，常造成重大自然災害，研究梅雨暴雨中尺度系統的發生發展機理，具有重要的理論和實際意義。
  13. 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。
  14. The results show that there are two centers of occurrence of llsw respectively in dong bei and jiang nan ; the regional torrential rain over the yangtze river basin is closely associated with llsw during the major periods of heavy rainfall ; the diurnal variation of the number of occurrence in the middle and low reaches of the yangtze river is the strongest in china there are some significant differences between llj and nallsw in positive season, spatial variation, diurnal variation and field of pressure. by the way, the important effect of inertial stability on heavy rainfall with both low level south - westerly jet and high level northerly strong flow is analyzed theoretically. the results show that the existence of the maximum of inertial stability in the left font of the low level jet is favor of the accumulation of the moist thermal energy, and conditional symmetric instability or convective instability can be expected in this region

    另外，慣性穩定性的作用以往不受重視，本文通過對西南低空急流左前方和高空偏北大風軸右後方的慣性穩定性和對稱穩定性的理論分析和實例計算，表明慣性穩定性在伴有高低空急流的暴雨中有重要意義，揭示了梅雨暴雨的一種新的高低空急流耦合機制：低空急流左前方慣性穩定度大值區的存在，有利於低層濕熱能量的積累，使低層傾斜對流的不穩定發展更多期望于條件性對稱不穩定或對流不穩定；高空偏北大風軸（西風急流）的存在，是其右後方（右側）出現對稱不穩定的有利條件，高空相對容易出現干對稱不穩定；慣性穩定性的作用，使低層的傾斜對流更偏向於垂直方向，有利於對流發展，使高層的傾斜對流更偏向於水平方向，有利於高層輻散。
  15. 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。
  16. Diagnostic analysis are carried out in the meiyu storm rainfall process from 00ut of 20th july to 00ut of 01st august 1998 in this study. results showed that the patterns in high benifit to this rainfall process

    本文首先對98年7月20日00時~ 8月1日00時的梅雨暴雨的環流形勢和降水要素進行了實況的診斷分析，結果表明：高空環流形勢有利於該段降水。
  17. The families are corresponded to synoptic systems, also are results of their interactions

    梅雨暴雨系統的雲系成員是相應的天氣系統相互作用的產物。
  18. 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。
  19. Use radar and satellite data to improve initial humidity field and four dimensional variational data assimilation to improve initial wind field, and simulate it with mm5, which has improved the simulation ability of meiyu heavy rainfall

    利用雷達、衛星資料對初始濕度場的改進和四維變分同化對初始風場的改進進行中尺度數值模式（ mm5 ）模擬，提高了梅雨暴雨模擬能力。
  20. 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。
分享友人
分享到 Line

分享到臉書