梅雨期 的英文怎麼說

中文拼音 [méiyǔqī]
梅雨期 英文
bai-u rainy period
  • 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
  • 期 : 期名詞[書面語]1. （一周年） a full year; anniversary 2. （一整月） a full month
  • 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. 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。
  5. 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。
  6. 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
  7. After the disaster caused by continual heavy rainstorm during the huaihe ' s meiyu period since 1991, the abnormal rainstorm weathers during the meiyu period occur again in june and july, 2003

    淮河流域梅雨期繼1991年出現持續性大暴雨造成嚴重洪澇災害后， 2003年6月7月又出現了持續性梅雨暴雨異常天氣過程。
  8. A strong decadal change of the meiyu periods in the mid - lower yangtze basin occurred in late 1970s since 1885 : a weak meiyu stage in 1959 - 1978 abruptly transformed into the strong one during 1979 - 1999

    摘要1885年以來長江中下游梅雨期在70年代末發生了一次強年代際突變：從1958 - 1978年的弱梅雨時段突變為1979 - 1999年的強梅雨時段。
  9. ( 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。
  10. When south indian ocean in southern hemisphere - zonal ( meridional ) circulation developing in middle latitude and in high latitude of australian, the precipitation in middle and lower reaches of yangtze river rather big ( small ) after some relative process affecting

    當南半球南印度洋?澳大利亞中高緯度地區緯向（經向）環流發展時，通過一系列的環流過程影響，長江中下游梅雨期降水偏多（偏少） 。
  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. In this article, the essential characteristic during meiyu and how to improve the criterion of meiyu, the effect process of circulation during meiyu, the characteristic of precipitation ' s distributing and the character between the precipitation and height are construed

    文章著重探討分析了梅雨期的系統特徵及如何改進梅雨標準、梅雨期大氣環流的影響過程、梅雨期的降水場分佈特點以及梅雨期降水場與高度場的相關特徵。
  13. 2 ) there is three basic precipitation regions in middle and lower reaches of yangtze river. they have visible homologous relationship with the period of meiyu in the temporal variation, in the late 1980 ' s, the characteristic of precipitation in midd le and lower reaches of yangtze river begins to altering

    2 ）長江中下游梅雨期的降水主要存在三個基本地區，且在時間變化上與梅雨期的出現有著明顯對應關系， 80年代末，長江中下游梅雨的降水特點發生了改變。
  14. A durative heavy rainfall process occurred on the middle and lower reaches of yangtze river in lat junl999. lt was just during the period of the operation of hubex experiment which provided a great deal of intensive rainfall data and upper - air sounding data. so it is a good chance for us to do research on the mei - yu front and low

    1999年6月下旬在長江中下游出現了梅雨期的持續性暴雨，並且正值hubex試驗期間，獲得了很多加密觀測降水及探空資料，為我們提供了良好的研究梅雨鋒和低渦的機會。
  15. The gps data from gps networks in yangtze delta is explored to investigate the improvement of mm5 simulation on rainfall event occurred over meiyu period in 2002 with the aid of initial humidity fields reanalysis and assimulation

    利用建立在長江三角洲地區gps觀測網中gps資料，針對2002年梅雨期間影響長江三角洲地區的降水過程進行了gps資料在mm5中尺度數值預報模式中的應用研究。
  16. Using the daily rainfall data of 740 stations over china and ncep daily up - ai data from 1971 to 2000, we analyzed the average mei - yu climate field. based on the climate field and mei - yu intensity index, we confirm that the year of 1999 is a typical mei - yu. besides, the intensity of mei - yu rainfall in 1999 is the highest since we had record, so the analysis of mei - yu in 1999 can present the common characteristics of mei - yu

    本文利用1971 - 2000年中國740站的日平均降水資料和ncep的日平均高空資料分析了梅雨氣候場，利用梅雨的氣候場及中國氣象局氣候診斷預測室的梅雨強度綜合指數，確定了1999年是一個非常典型的梅雨年，並且1999年梅雨期間的降水強度是歷史以來的最高值，因此我們對1999年梅雨進行的分析有很大的代表性。
  17. 4 ) during the meiyu, the precipitation in middle and lower reaches of yangtze river has the relationship with southern hemisphere circulation in early april and may. when the meridional circulation in middle and high latitude of south pacific in april and may is rather obvious and the south pole eddy is rather strong, the precipitation in middle and lower reaches of yangtze river may be bigger than ever

    4 ）梅雨期長江中下游降水多寡與前期4 、 5月南半球環流存在聯系，當4 、 5月南太平洋中高緯度地區經向環流較為明顯，南極渦偏強時，長江中下游地區梅雨期降水易偏多；反之，當4 、 5月南太平洋中高緯度地區緯向氣流較為明顯，高緯度西風較弱，南極渦偏弱時，長江中下游地區梅雨期降水易偏少。
  18. Based on case study and climate analysis, this work arrives at the central cause of dv of the meiyu rainfall, which lies in the regional difference in dv of the lower - level temperature field of east asia, and the cause relates essentially to 1 ) distinct topography in this region and 2 ) a particular cloud pattern during the wet season

    本文通過實例分析、氣候比較和數值模擬認為：梅雨降水日變化的根本原因是東亞低層大氣溫度場日變化的區域性差異，造成這種差異的基本原因又包括兩個方面，一是東亞特殊的地形構造，二是梅雨期內特殊的雲區分佈。
  19. Dynamical diagnosis, numerical simulation and theory analysis are done on genesis condition, structure, propagation and development mechanism of a mesoscale convective complex ( mcc ) which caused the first torrential rain in the meiyu period of yangtze river and huaihe river basins in june 22 - 23, 2003

    對造成2003年6月22 - 23日梅雨期首場暴雨的影響系統? ?中尺度對流復合體（ mcc ）的環境條件、結構、運動和發生發展機理進行了動力診斷、數值模擬和理論研究，探討了預報失敗的原因和改進預報的思路。
  20. 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 ）梅雨鋒低渦的結構及其與降水關系分析1999年在梅雨鋒上有三個梅雨鋒低渦相繼在其上產生，冰箱東北方向移動，分別對應著長江中下游的三次強降水過程：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。低渦之所以產生這么大的降水和降水強度是因為低渦在移動過程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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