梅雨 的英文怎麼說

中文拼音 [méiyǔ]
梅雨 英文
[氣象學] mould rains; plum rains
  • 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
  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. It also explain that the correlation between ssta of kuroshio and the change of wind field in equaroral mid - pacific is results of air - sea interaction ; however, when time comes into summer, the instance status of ocean is different from the last winter to next early springtime, the sea surface temperature turn into the definitive factor, so the increase of heat flux in may to jun month which is realized by absorbing more heat from the sun radiation results in the decrease of sst in kuroshio in the season of jun - jul. finally, during the aug to dec season of next year, the sst of kuroshio is increasing again

    最後分析了黑潮海溫與夏季東亞大氣環流及我國降水的時滯關系，發現：當前冬黑潮區域海溫異常偏高時，後期夏季亞洲低壓的強度減弱，西北太平洋副熱帶高壓強度加強，而且位置西伸、偏北，梅雨鋒位置偏南，長江中下游地區降水偏多，北太平洋冬季海域的海溫分佈呈+ 、 - 、 +趨勢（順序為赤道中東太平洋、西北太平洋、我國近海） ；反之亦然。
  13. As a result, we find that in winter when the kuroshio is cooler than the normal, at following summer, the continental cyclone deepen and the east asia monsoon strengthen, that the mid - latitude blocking high weaken and zonal circulation develop, the east asia teleconnection of " - + - " is stired up, so that subtropical high weaken and diminish, and tend to east north, tropical monsoon trough strengthen and mei - yu front weaken, and tend to north, meanwhile south asia high weaken and diminish, and tend to eastvnorth, is easy to form eastern region type

    結果發現當黑潮海溫冷異常時，後期夏季大陸熱低壓加深，東亞夏季風偏強。中緯度阻塞高壓減弱，東亞地區緯向環流發展，在東亞-西太平洋地區激發「 - + - 」的東亞遙相關型，從而西太平洋副高強度偏弱，面積偏小，位置偏東、偏北，東亞梅雨鋒也偏弱，季風槽則變強，位置偏北。同時南亞高壓偏弱，位置偏北、偏東，易形成東部型。
  14. The tbb ( black - body temperature ) analysis depicts that several meso - p - scale cloud clusters and convective cells are embedded and alternately developed within a mcc

    （ 2 ）梅雨鋒中的mcc內嵌有若干個中-雲團，對流體此生彼消十分活躍。
  15. 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。
  16. At the same time, the effects of dragging force from fall of hydrometeors and latent - heat release from phase transfer are tested. from the analyses we conclude that the distributing of the cloud particles relates with temperature closely. huanan heavy rainfall and mei - yu front heavy rainfall have mixed - phase process with vapor phase, liquid phase and ice phase

    詳細分析了形成降水的雲物理過程，探討了源匯項對水凝物的貢獻，並通過敏感性試驗，考察了雲物理過程對降水熱力動力過程的反饋作用，研究結果表明：華南暖區暴雨和長江梅雨鋒暴雨的雲物理過程具有汽、水、冰三相混合雲特徵。
  17. Storm flood analysis for taihu lake basin during plum rain period of

    1999年梅雨期太湖暴雨洪水分析
  18. Extremely heavy meiyu over the yangtze and huaihe valleies in

    1931年江淮異常梅雨
  19. Sunspot qbo effect on meiyu precipitation in hangzhou

    對杭州地區梅雨的影響
  20. 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。
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