雨期 的英文怎麼說

中文拼音 [yǔqī]
雨期 英文
rain spell; pluvial
  • 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
  1. Berms are mainly built during storms.

    浪堤主要是在暴風雨期間造成的。
  2. 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。
  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. I was in a small boat during the storm, but it stopped after half an hour and i was able to breathe again

    暴風雨期間我正呆在一隻小船上。但半小時后暴風雨就停了，我這才鬆了一口氣。
  5. 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
  6. The boat was torn from its moorings during the storm

    那艘船在暴風雨期間脫離了避風港。
  7. The late 1940s - early 1960s and early 1970s to middle 1980s is wet period. the early 1960s to early 1970s is dry period. the significant decrease of rainfall began in the 1990s

    40年代末至60年代初期及70年代初期至80年代中期為多雨期， 60年代初期到70年代初期為少雨期， 90年代初期以後又有明顯的下降。
  8. The study on the time series of global land average seasonal precipitation points out that the interannual and interdecadal fluctuations of the rainfall are clear. the late 1940s - late 1960s and the 1980s - 1990s corresponds to wet period and dry period respectively, and the 1970s expresses a apparent interannual variation of rainfall

    指出降水有明顯的年際和年代際尺度的振蕩， 1940s末至1960s末為多雨期， 1980s至今降水多為負距平； 1970s降水的年際變化比較大。
  9. Result shows that summer precipitation in north china has gone through four major dry - damp phases, richer periods from 1900 to 1915 and from 1946 to 1978, less periods from 1916 to 1945 and from 1979 to 2001, and has obvious inter - decadal variations, and has about 60a, 20 - 30a, 10a major periods and has twice abrupt changes in 1953 and 1979

    結果表明：華北夏季降水經歷了四個主要干濕階段，即1900 1915年和1946 1978年為多雨期， 1916 1945年和1979 2001年為少雨期，具有明顯的年代際變化，主要有約60年、 20 30年和10年左右的周期，並在1953年和1979年發生了兩次氣候突變。
  10. Analysis shows that when summer precipitation in north china is richer ( less ), tropical east pacific ssta is colder ( warmer ) phase, and slp and 500hpa geo - potential height are negative ( positive ) anomaly over the asia, west pacific sub - high is northerner ( southerner ), and block high in mid - highs latitude happens less ( more ) than normal, east monsoon is stronger ( weaker )

    分析表明華北夏季多（少）雨期，赤道中東太平洋ssta處于冷（暖）位相，在非洲大陸上slp利500hpa位勢高度均為負（正）異常，西北太平洋副高位置偏北（南） ，中緯度阻塞高壓發生頻率較低（高） ，東亞夏季風偏強（弱） 。
  11. 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。
  12. 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。
  13. ( 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。
  14. 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） 。
  15. 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。
  16. 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。
  17. 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。
  18. 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。
  19. 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。
  20. 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。
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