背風區 的英文怎麼說

中文拼音 [bēifēngqū]
背風區 英文
sous le vent dist
  • 背 : 背動詞1. （用脊背馱） carry on the back 2. （擔負） bear; shoulder
  • 風 : Ⅰ名詞1 （空氣流動） wind 2 （風氣; 風俗） practice; atmosphere; custom 3 （景象） scene; view 4 ...
  • 區 : 區名詞（姓氏） a surname
  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. ( 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。
  3. However, with the impact of housing loan guarantee, and gradual opening of chinese financial market, renovating residential mortgage loan insurance is imperative under the situation. deep study is done on residential mortgage loan insurance by this thesis, and there are four sections : the first section expatiates background and significance of the study on residential mortgage loan insurance, makes a clean definition of this insurance, points out that precondition of residential mortgage loan insurance is existence of risks, and sets force functions of residential mortgage loan insurance

    在此背景下，本論文對個人住房抵押貸款保險進行了深入研究，全文分為四個部分：第一部分闡釋了個人住房抵押貸款保險研究的背景及其意義，指出風險的存在是個人住房抵押貸款保險存在的前提，對個人住房抵押貸款保險進行了定義，闡述了個人住房抵押貸款保險的基本職能及派生職能，並指出了住房置業擔保與個人住房抵押貸款保險之間的區別與聯系。
  4. It is found that the climatological mean of wind speed and air - sea humidity difference are both large, the variation of wind speed are almost in phase with air - sea humidity difference, yielding much larger or smaller latent heat flux. so the ocean release the most latent heat in its own winter of the two hemispheres when both wind speed and air - sea humidity difference are large

    發現在南北兩信風區，風速和海氣濕度差的變化幾乎是同位相的，平均背景風速和海氣濕度差都較大，他們互相加強彼此對潛熱通量變化的貢獻，所以海洋潛熱損失最大是發生信風南北兩區的各自風速和海氣濕度差都較大的冬季。
  5. Data used in this work are north pacific ssta, 160 stations precipitation of china, and ncep reanalysis data. main results are as follow : ( 1 ) it is found that a apparent transition of north pacific ssta in later 1970 ' s : eastern and middle - equatorial pacific ssta turns from cold to warm with area extending, and mid - latitude pacific ( west wind drift zone ) turns from warm to cold. during this transition of ssta, different characters also appear in el nino and la nina : before 1976, la nina happens more frequently, and its duration is longer, el nino zone develops from negative ssta in the early stage ; after 1976, el nino happens a little bit frequent and longer with more intensity than before, el nino zone develops from positive ssta in the early stage ; the course of ssta variation has an enso cycle of 2 - 6 years, annual oscillation of 8 - 9 years, and decadal variation of about 22 years

    本文採用1950 - 1999年北太平洋海表溫度（ sst ） 、中國160站夏季降水和ncep再分析的歐亞500hpa高度場等資料，利用eof 、 svd 、小波分析、合成分析和相關分析等方法，在分析北太平洋海溫時空分佈特徵的基礎上，著重探討了海溫異常及其年代際變化對我國東部降水的影響，並對降水、高度場和海溫三者之間的關系進行了分析，以試圖尋找三者異常之間可能的聯系，主要結論如下： （ 1 ） 1976年前後，北太平洋海溫經歷了一次明顯的轉變，赤道中、東太平洋厄爾尼諾海區由冷轉暖，暖水范圍增大，中緯度西風漂流區海溫由暖轉冷；在這樣的年代際背景下，厄爾尼諾、拉尼娜事件在不同的時期也有不同的特徵：在76年前，拉尼娜事件發生頻率高，持續時間長，事件起始於負海溫距平；而76年後，則是厄爾尼諾事件發生頻率略高，持續時間長，強度增大，事件起始於正海溫距平。
  6. ( 5 ) the spring greenland sea - ice extent is larger ( smaller ) : then during the following summer the high of the japanese sea is stronger ( weaker ), and the low of the asian land is stronger ( weaker ), which make the pattern of low west and high east easily ( uneasily ) form ; the ascending movement over north china is strengthened ( weakened ) ; the summer monsoon of east asia is stronger ( weaker ), then the southeastern, warm and damp airflow towards the north china is stronger ( weaker ), and the cold airflow of the high level over the north china is also stronger ( weaker ), which make the convergence of the cold and warm air over north china easily ( uneasily ) form ; the sst of the east pacific ocean is lower ( higher ), while the sst of west wind drift is higher ( lower )

    （ 5 ）春季格陵蘭海冰面積偏大（小） ：後期夏季日本海高壓偏強（弱） ，而大陸上低壓也偏強（弱） ，易（不易）形成西低東阻的形勢；華北地區的上升運動增強（減弱） ；東亞夏季風偏強（弱） ，向華北地區輸送的西南暖濕氣流偏強（弱） ，而對應高空華北地區上空冷空氣活動偏強（弱） ，利於（不利於）華北上空冷暖空氣的交匯；夏季赤道東太平洋海溫偏低（高） ，西風漂流區海溫偏高（低） 。在以上的環流背景下，華北夏季降水偏多（少） ，易澇（旱） 。
  7. The analysis of the large - scale synoptic situation shows that strong precipitation is closely related to the explosion of monsoon and the intensification of cross - equatorial flow which bring a lot of vapor and meet with cold masses at the eastern of northwest district on 8th, june causing extremely heavy rainfall ; that subtropical high - level jet at 200hpa, subtropical high at 500hpa and low - level jet at 850hpa are the weather backgrounds favorable to strong precipitation ; that the pattern of eastern highs and western lows and the establishment of a low - level jet and the coupling between upper - and low - level patterns that determine that the rain occurred in the east of the northwest china ( on average, this is the rainy season for the south of china, but not for the northwest china ) ; that water vapor comes from southerly and easterly flow which converge at the eastern of northwest district with convergence mainly in lower levels and pbl ; that the high value of the whole - level apparent heat source < q1 > is near the area of large rainfall in the direction of northeasterly - southwesterly agreeable to shear line very well and the condensation latent heat releasing is main heat source with vertical advection item playing key role in q1 and q2 ; that there is a vertical secondary circulation crossing low - lever jet whose ascending branch is at the area of large rainfall ; that the construction of convection instability and conditional symmetry instability results that there is not only deep thermal instability, but also moisture influx and triggering mechanism of thermal instability causing strong torrential rain

    作為對比，本文還對2002年6月24 - 25日發生在北京地區的強地形雨進行了分析，並討論陜南、北京地區兩地暴雨的異同點以及地形作用的共性和個性，為兩地暴雨預報提供有益的參考，得出了一些很有意義的結果： 1大尺度環流背景分析表明： （ 1 ） 「 02 . 6 」強降水與6月上旬越赤道氣流和季風爆發密切相關，攜帶大量水汽的偏南氣流與冷空氣於6月8日交匯在西北地區東部，導致了這次強降水的發生； （ 2 ） 200hpa的副熱帶西風急流、 500hpa副高以及850hpa的低空急流的配置非常有利於本文分析之陜西強降水的發展與維持。大尺度形勢分析表明，東高西低形勢場、低空急流的建立和高低空形勢的配置決定了這場降雨出現在西北地區東部。與暴雨區相聯系，存在一支橫越低空急流的經向垂直環流，暴雨區處于該垂直環流的上升支； （ 3 ）偏南和偏東氣流水汽通道在西北地區東部交匯，水汽的輻合積聚主要在對流層低層和行星邊界層內完成； （ 4 ）整層的視熱源< q _ 1 >高值區在暴雨區附近呈東北-西南向分佈，與切變線走向非常一致，降水產生的凝結潛熱釋放是強降水區大氣的主要熱源。
  8. The calculated mean diameter, mean square - root diameter, mean cube - root diameter and liquid water content are all well matched with the observational results ; in the paper two examples have been analyzed by using the seeding region data and the possible affecting region data in leeward region. it is found that f - 100, 2dc, and 2dp ' s particle concentrations increase in leeward region, but rising extent is different, which is likely to be due to difference of seeding effect time

    擬合值和觀測值吻合的較好，計算出的平均直徑、均方根直徑、均立方根直徑和粒子濃度與觀測值也比較吻合；本文對兩組個例的催化影響區域及可能採集到相應值的下風方區域進行了分析，催化下風向影響區的f - 100 、 2dc 、 2dp的粒子濃度比背景值都有所增加，但是增加的幅度不同，應該是催化響應時間的原因。
  9. The thesis deals with catholic churches in chongqing area built from mid - 19th century on, including its historical and social background, development process, locations, building styles, and art achievement, especially its creative treatments, in western - chinese style combination. systematical field investigation and analysis reveal that catholic church as built in chongqing area in 19and early 20 centuries, as a part of western architectural culture, developed and changed to yield a variety of architectural form and to become a valuable part of chongqing cultural legacy

    本文對重慶（巴渝）地區的近代天主教堂建築的社會歷史背景、發展狀況、地域分佈、建築造型風格特點和藝術成就作了較系統的調查研究和分析，由此展示出重慶近代天主教堂作為西方建築文化的一部分在這一地區的發展和演變，結果產生出豐富多樣的建築形態，成為重慶近代建築文化遺產中具有相當價值的組成部分。
  10. At the time, winds were blowing generally from the east, hence the appearance of clouds over the eastern i. e. windward side of luzon. note that the western i. e. lee side of luzon is practically cloud - free

    當時該區普遍吹偏東風，因此在呂宋東面即迎風面出現雲層，而呂宋西面即背風面則晴空無雲。
  11. At the time, winds were blowing generally from the east, hence the appearance of clouds over the eastern ( i. e. windward ) side of luzon. note that the western ( i. e. lee ) side of luzon is practically cloud - free

    當時該區普遍吹偏東風，因此在呂宋東面（即迎風面）出現雲層，而呂宋西面（即背風面）則晴空無雲。
  12. The model simulations indicate that the severe storm is occurred in the pattern high - level of northwest flow, the waterjumping downhill flow form taihang mountain is the key mechanism to initiate the convective, on the other hand, the terrain can induce unbalanced low - level flow, which play an importance role in generating the mesoscale gravity waves ( mgws ) by convergence and divergence in low - level troposphere

    （ 2 ）太行山對華北強對流風暴的發生有重要作用。一方面，地形可引起邊界層風場的變化，包括風垂直切變、下坡氣流和中尺度輻合線，從而對風暴的啟動、組織和移動發揮作用；另一方面，山脈背風波動和地形產生的不平衡氣流，有利於中尺度重力波（ mgws ）的產生和維持，並對下游地區強對流天氣的發展產生影響。
  13. The bridegroom is an elephant trainer luo xiuqiang and bride is tour guide of the scenic spot kong quanyu

    當日，在雲南省西雙版納野象谷風景區，野象谷馴象師羅秀強和景區導游孔全玉舉行一場大象背上的婚禮。
  14. Rss is supposed to be based on xml or xml rdf standards. unfortunately, the famous wild west community behind rss has many renegade elements producing feeds that are not even well - formed xml

    不幸的是， rss背後那個以牛仔作風聞名的社區有很多離經叛道的成分，生成的消息包（ feed ）甚至都不是結構良好的xml 。
  15. Yingbin beach yingbin square is a landmark building for low mountain visitors spreading center - yingbin square, from left to right, followed by the monk - palm " sinian first mountain ", and royal emperor kangxi to three characters " emeishan ", and world heritage signs, our proximity to the national scenic in an article in the visitors center - visitors center and mount emei in sichuan province, one of the museum focus emeishan museum

    迎賓灘是迎賓廣場的標志性建築，面向低山區的遊人集散中心? ?迎賓廣場，從左到右，依次是寶掌和尚所提「震旦第一山」 ，和康熙皇帝御提三個大字「峨眉山」 ，以及世界遺產標志，背靠全國風景區中第一個遊人中心? ?峨眉山遊人中心和四川省重點博物館之一的峨眉山博物館。
  16. In equatorial region, the mean air - sea humidity difference is much smaller, so the variations of air - sea humidity difference under large mean wind speed dominate the variations of latent heat flux. the ocean release the most heat during the period from march to may, when sst is highest in the whole year because sst dominates the variation of air - sea humidity difference

    在赤道冷舌區，平均的背景海氣濕度差比較小，所以平均風速背景下的海氣濕度差的熱帶大西洋海表潛熱和感熱通量的季節和年際變化研究變化主導該區的潛熱通量的變化。
  17. Lean against the provincial scenic spot in the holiday village, it is one that melts production of tea, expression transforming, afforestation and travel in holiday, integrative ecological agriculture demonstration base and travel resort of public welfare forest

    度假村背靠省級風景名勝區，是一個融茶葉生產、神態公益林改造、園林綠化和旅遊度假與一體的生態農業示範基地和旅遊度假村。
  18. One last consideration is that it ' s often the edge of the lee side which is the most dangerous area

    最後要注意的一點，背風區的邊緣往往是最危險的地方。
  19. It ' s often more dangerous to test out the waters by feeling around the edge of the protected area than by flying all the way into it

    人世間最危險的事情莫過于在背風區邊上試水，所謂當斷不斷反受其亂。
  20. If you are completely in the lee, you may be fully protected - but if you ' re at the edge of the protected area, then you may well encounter the maximum amount of turbulence

    如果你整個傘都在背風區內，那麼你會得到很好的保護，如果你在邊緣上晃悠，那麼你會遭遇到該地區最強烈的亂流。
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