水汽輸送 的英文怎麼說

中文拼音 [shuǐqìshūsòng]
水汽輸送 英文
transport of moisture
  • 水 : 名詞1 （由兩個氫原子和一個氧原子結合而成的液體） water 2 （河流） river 3 （指江、河、湖、海、洋...
  • 汽 : 名詞1. （由液體或某些固體變成的氣體） vapour2. （水蒸氣） steam
  • 輸 : Ⅰ動詞1 （運輸; 運送） transport; convey 2 [書面語] （捐獻） contribute money; donate 3 （失敗） l...
  • 送 : 動詞1 （運送; 傳送） deliver; carry 2 （贈送） give as a present; give 3 （伴送; 送別） see sb of...
  • 輸送 : deliver; supply; carry; transport; convey; feed; transmit; transfer; transportation; delivery
  1. Climatological characteristics, which can provide some drought or flood years with large - scale background, are investigated for large - scale water vapor transport over asian - australian monsoon region based on vertically integrated water vapor flux by pentad from 1980 to 1997. at the same time, the differences of moisture transport over the yangtze river basin between drought and flood and the moisture budgets over eastern china from april to september are examined. major results are as follows : i

    使用1980 ? 1997年垂直積分的整層水汽輸送通量資料，從氣候平均的角度分析了亞澳季風區大尺度水汽輸送演變和偏南風水汽輸送在東亞地區推進的氣候特徵，為研究異常年份旱澇事件的產生提供了相應的大尺度背景；同時還討論了長江流域旱澇年水汽輸送的差異以及4 - 9月我國東部各區域的水分收支情況。
  2. In drought ( flood ) years over the yangtze river basin, the southerly moisture transport with the summer monsoon can shift to northern ( southern ) than the normal, the southeasterly water vapor from south

    雨季建立之前和雨季結束之後，華北和東北地區西邊界的偏西風水汽輸入占絕對優勢;雨季中南邊界的偏南風水汽輸送對華北最為重要，東北地區雨季期間南邊界的水汽輸入和與來自西邊界的水汽輸入貢獻相當。
  3. The southerly water vapor can progress to 50 n near north - east in china -, the southeasterly water vapor from south side of the west pacific subtropical high and north side of the monsoon trough can march westward to 100 e near south - east part of gansu in summer

    東亞夏季偏南風水汽輸送所能到達的北界為50 n附近的東北北部。西太平洋副高南側、亞洲季風槽北側的東南風水汽輸送在夏季可向西擴展到甘肅東南部地區（ 100 e附近） 。
  4. ( 3 ) the polar eddy, the west circumfluence on 500hpa medium latitudinal region ands subtropic circumfluence are the key systems of tpnes floods precipitation and, the wet years have abundant vapor, moreover, the omga is positive in all atmosphere

    （ 3 ）極渦、中高緯西風環流系統和副熱帶系統是影響青藏高原東北側區汛期降水的大尺度環流背景關鍵系統。同時，多雨年的主要流場特點是有利於水汽輸送，且整層大氣始終表現為上升運動。
  5. Based on the analysis mentioned above, a conceptual diagram explaining the physical process is put forward : stronger ( weaker ) convective activities in tropical areas stronger upward ( downward ) vertical anomaly stream in tropical areas more ( less ) moisture transports from " key regions " to shandong stronger ( weaker ) hadley and walker circulation stronger ( weaker ) east asian summer monsoon eap ( negative eap ) in 500hpa upward ( downward ) vertical anomaly stream rise in shandong subtropical high abnormally located northward ( southward ) more ( less ) rain in shandong province

    弱季風年與山東夏旱年則相反。通過分析山東夏季降水與東亞夏季風以及大氣環流異常的物理過程，得出了如下物理概念模型:熱帶印度洋以及南海-熱帶西太平洋地區對流加強（減弱）吟熱帶地區垂直上升（下沉）氣流增強崢熱帶印度洋和南海一西太平洋地區水汽輸送通量增加。
  6. The results of eof show that there are three rainfall patterns in china in summer such as midst rainfall pattern, south rainfall pattern and north rainfall pattern. the relations between the three rainfall patterns and three patterns of water vapor transport are discussed by projection, and influencing areas of different vapor inflow corridors are located by correlation

    Eof分析表明，夏季中國東部存在三類異常雨型：中間型、南方型和北方型，用投影法討論了三類異常雨型與異常水汽輸送的關系，並通過相關分析找出了不同水汽通道的影響范圍。
  7. It was found that the " key regions " from which moisture transports influenced shandong summer rainfall lies in tropical india ocean, south china sea to tropical west pacific, china mainland to japan sea and the upstream area in westerly belt by analysis of svd method on water vapor transport

    夏旱年則相反。通過對旱澇年水汽輸送與山東夏季降水的相關分析，山東夏季降水和水汽輸送svd分析，發現：影響山東夏季降水的水汽輸送「關鍵區」主要位於熱帶印度洋、南海-西太平洋、中國大陸-日本海以及山東上游西風帶地區。
  8. The climate characteristics of global water vapor transport and global water balance are analyzed by using the ncep / ncar reanalysis data set from 1958 to 1998

    利用ncep / ncar1958 1998年再分析資料分析了全球水汽輸送時空分佈的氣候特徵和全球水分平衡。
  9. In order to study the anomaly pattern of summer rainfall in north china and the cause responsible for the anomaly, the climate characteristics of summer rainfall in north china and related circulation pattern, water vapor transport and outgoing long - wave radiation ( olr ) were analyzed in detail in this paper. more attention was paid on studying the relationship between sea surface temperature anomaly ( ssta ) over the north pacific and summer precipitation anomaly in north china and an agcm was utilized to confirm the affection of ssta on the summer rainfall of the north china

    為了揭示華北夏季降水異常規律及其成因，本文詳細分析了華北夏季降水的氣候特徵及有關的環流特徵、水汽輸送特徵和向外長波輻射（ olr ）特徵，著重研究了北太平洋海溫異常與華北夏季降水異常的關系，並應用大氣環流模式初步驗證了北太平洋海溫異常對華北夏季降水的影響。
  10. The above analysis showed that this heavy rainfall event took on obvious meso - scale characters and was the combination of the three flows, so we can deduce : ( 1 ) surface southeasterly wind and topography may play the main role in this event ; ( 2 ) the easterly cold air rushing into the southern shaanxi province in the lower troposphere was strongly relative to the form of surface cold - front type of occlusion ; ( 3 ) there were two reasons for the secondary circulation ' s strengthen in the evening, one was the effect of a mountain - valley wind and the other may be latent heat leading to ascending motion ; ( 4 ) the shape of potential instability stratification corresponded well with the development of the warm - moisture advection ; and ( 5 ) the vapor providing essential thermodynamics was transported by a southwesterly low - level jet from the bay of bengal and the south china sea. furthermore, with the effect of terrain, the southern shaanxi province became the center of this extremely heavy rain process

    中尺度結構分析表明，本次暴雨具有明顯的中尺度特徵，是由三支氣流共同作用的結果，分析發現（ 1 ）地面東南風和地形在這次大暴雨過程起主要作用； （ 2 ）東路冷空氣主要是通過中低層侵入陜南地區的，並與地面冷式錮囚鋒的形成密不可分； （ 3 ）夜博士論文:中尺度地形對陜南暴雨的影響研究間垂直次級環流發展加強可能有兩個原因，一個是由於地形山谷風的作用，另一個是降水的潛熱釋放激發了上升運動: （ 4 ）位勢不穩定層結的形成與低層暖濕平流的發展有很好的對應關系; （ 5 ）本次暴雨的水汽主要靠偏南風急流將孟加拉灣和中國南海的水汽輸送至西北地區東部，為暴雨的發生提供了必要熱力條件。
  11. Seasonal variations of water vapor transport over east asia monsoon region are studied, especially that in summer season. the results indicate that there are four vapor inflow corridors to fetch china : southwest corridor, south china sea corridor, southeast corridor and northwest corridor. it shows impact of south asia monsoon, south china sea monsoon, subtropical monsoon and middle latitude westerly belt on summer rainfall anomaly over china, respectively

    分析了東亞季風區水汽輸送的季節變化，並著重研究了夏季東亞季風區的水汽輸送特徵，指出夏季東亞季風區水汽輸送有四條通道到達中國大陸：西南通道、南海通道、東南通道和西北通道，分別體現了南亞季風、南海季風、副熱帶季風和中緯度西風帶對中國夏季降水的影響。
  12. The strong convergence areas, which are coincide to the big rain belt, mostly lie in the planetary - scale water vapor transport. iii

    夏季垂直積分的水汽輸送通量強輻合區大多位於行星尺度水汽輸送大值帶中，和降水大值區之間有很好的對應關系。
  13. Big scope south airflow and vapor transport and convergence brought by meso - scale jet, offer vapor condition which rainstorm occur and develop

    大范圍偏南氣流及其中的中尺度急流帶來的水汽輸送及輻合，為暴雨天氣的發生、發展提供了低層水汽條件。
  14. Study on heat and water vapour transport during a rainstorm process in south china

    一次華南暴雨過程中水汽輸送和熱量的研究
  15. In may and june, the moisture transports from " key regions " are all important to shandong summer rainfall

    5 6月來自上述「關鍵區」水汽輸送對山東夏季降水異常均有貢獻。
  16. The change of transport pattern from winter to summer closely relates with the change of the direction of the cross equatorial moisture transports, especially nearl 05 e and 45 e. ii

    水汽輸送形勢的季節轉變跟南北半球間的越赤道輸送的轉向密切相關，尤其是在105 e 、 45 e附近。
  17. ( 2 ) the yearly vapor water transport in northwest china is mainly consist of the west - southly air stream from the center - west of qinghai - xizang plateau and the east - southly air stream from the south of shanxi province

    （ 2 ）西北地區全年水汽輸送主要來自與其南面相鄰的青藏高原中西部的西南暖濕氣流以及陜西南部的東南暖濕氣流。
  18. It is hard to satisfy the conditions of cold air and vapor together for torrent rainfall, in particularly the transportation of vapor in low atmosphere, f ). it is one of the main reasons for the arid climate in ningxia

    寧夏特殊的地理位置和地形特徵造成了水汽輸送的阻礙，且冷空氣與水汽難以配合，這也是寧夏降水不足、氣候乾旱的天氣學根本原因之一。
  19. The northward march of the southerly moisture transport with the summer monsoon transport over the east asian ( 110 - 130 e ) shows the feature of staged jumps. each jump relates with the large - scale important weather incident in china

    （ 2 ）氣候平均狀態下，夏季偏南風水汽輸送在東亞地區（ 110 ? 130 e ）的向北推進有階段式跳躍的特點，每次跳躍均與影響我國的大型天氣事件相聯系。
  20. The 1st time coefficient shows the staged feature of the progression of the moisture transport over asian - australian monsoon region, which relates with the large - scale important weather incidents in asian - australian monsoon region. iv

    第一特徵向量對應的時間系數圖表現了亞澳季風區4 - 9月份的水汽輸送階段性的時間演變特徵，可反映夏季亞澳季風區的大型天氣事件的發生變化過程。
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