暴雨中心 的英文怎麼說

中文拼音 [bàoyǔzhōngxīn]
暴雨中心 英文
centroid of storm rainfall
  • 暴 : Ⅰ形容詞1 （突然而且猛烈） sudden and violent 2 （兇狠; 殘酷） harsh and tyrannical; cruel; fierce...
  • 雨 : 雨名詞（從雲層中降向地面的水） rain
  • 暴雨 : torrential rain; rainstorm; hard rain; intense fall; squall; downpour; gush暴雨放大 storm maximiz...
  1. Most of the heavy rain occurs near the storm centre and along these spiral rainbands

    大雨大部份在風暴中心附近及螺旋雨帶中發生。
  2. The topographic influences in the southwest of central shandong are in favor of the formation of the low - level cell, which amplified the rainfall intensity and resulted in the precipitation center there

    魯中山區西南側有利地形促使了低層氣旋環流的形成，對暴雨具有明顯的增幅作用，是該地區出現暴雨中心的重要原因。
  3. In such risings of fire and risings of sea - the firm earth shaken by the rushes of an angry ocean which had now no ebb, but was always on the flow, higher and higher, to the tenor and wonder of the beholders on the shore - three years of tempest were consumed

    三年的疾風暴雨就在這樣的烈火熊熊人潮洶涌中過去了一一憤怒的海洋一浪高過一浪，沖擊著堅實的地面，永遠向前奔騰，從不後退，讓岸上的入看得心驚膽戰，目眩神駭。
  4. The main relative systems of heavy - hard rainfall in northeast plateau are western pacific subtropical high, south asia high, low latitude systems, upper level jet ( ulj ), low level greater wind speed axes, westerly trough and plateau trough, low level vortex, cold frontal, occluded front in qinghai lake, mesoscale low pressure, heat low - pressure in qinghai, shear line and convergence line, mesoscale cloud cluster, etc. the west subsidiary model of south asia high is the main circulation type of heavy - hard rainfall in this area

    3 、西太平洋副高、南亞高壓、低緯系統、高空急流、低空大風速軸；西風槽和高原槽、低渦、冷鋒、青海湖錮囚鋒以及中尺度低壓、青海熱低壓、切變線與輻合線、中尺度雲團等系統是高原東北部地區大到暴雨的主要相關系統。 100hpa上的南亞高壓中心強度加強，位置東西擺動預示高原地區將有降水產生，中心強度減弱，降水過程結束。南亞高壓西部副型是高原東北部地區大到暴雨的主要流型。
  5. ( 2 ) the increase of rainfall is closely associated with the increase of the disturbance wind which often can be found before the increase of rainfall, so the increase of the nonlinear subcritical symmetric instability can make the rainfall increase. ( 3 ) heavy precipitation often occurs between the south of axis of upper jet at 200hpa and the north of axis of low jet at 850hpa

    （ 3 ）降水區和暴雨中心主要位於200hpa高空急流軸南側和85ohpa低空急流軸北側之間;非線性亞臨界對稱不穩定與高空急流關系密切，它可能觸發高空急流核的形成;它與低空急流關系也很密切，它的出現可能引起低空急流的出現。
  6. Heavy precipitation often forms in the place between the source of high - disturbance wind field at 200hpa, especially of low - disturbance wind field at 850hpa. ( 2 ) the temporal and spatial scale about e - reflection index of nonlinear subcritical symmetric instability disturbance is 5 - 8hours and 200 - 300km respectively

    非線性亞臨界對稱不穩定使線性對稱穩定的大氣變為不穩定。降水區和暴雨中心主要位於高層200hpa和中層500hpa擾動風場極大值南側與低層850hpa擾動風場極大值北側之間。
  7. You raise me up when i am down and, oh my soul, so weary when troubles come and my heart burdened be then i am still and wait here in the silence until you come and sit awhile with me you raise me up, so i can stand on mountains you raise me up, to walk on stormy seas i am strong, when i am on your shoulders you raise me up … to more than i can be you raise me up, so i can stand on mountains you raise me up, to walk on stormy seas i am strong, when i am on your shoulders you raise me up … to more than i can be there is no life ? no life without its hunger each restless heart beats so imperfectly but when you come and i am filled with wonder sometimes, i think i glimpse eternity you raise me up, so i can stand on mountains you raise me up, to walk on stormy seas i am strong, when i am on your shoulders you raise me up … to more than i can be

    你鼓舞了我當我失落的時候我的靈魂，感到多麼的疲倦當有困難時，我的心背負著重擔然後，我會在寂靜中等待直到你的到來，並與我小坐片刻你鼓舞了我，所以我能站在群山頂端你鼓舞了我，讓我能走過狂風暴雨的海當我依在你的肩上時，我是堅強的你鼓舞了我…讓我能超越自己你鼓舞了我，所以我能站在群山頂端你鼓舞了我，讓我能走過狂風暴雨的海當我依在你的肩上時，我是堅強的你鼓舞了我…讓我能超越自己沒有一個生命?沒有生命是沒有渴求的每個繹動的心能夠跳動得那麼地完美但是當你來臨的時候，我充滿了驚奇有時候，我覺得我看到了永遠你鼓舞了我，所以我能站在群山頂端你鼓舞了我，讓我能走過狂風暴雨的海當我依在你的肩上時，我是堅強的你鼓舞了我…讓我能超越自己。
  8. They teach you to be proud and unbending in honest failure, but humble and gentle in success ; not to substitute words for action ; not to seek the path of comfort, but to face the stress and spur of difficulty and challenge ; to learn to stand up in the storm, but to have compassion on those who fall ; to master yourself before you seek to master others ; to have a heart that is clean, a goal that is high ; to learn to laugh, yet never forget how to weep ; to reach into the future, yet never neglect the past ; to be serious, yet never take yourself too seriously ; to be modest so that you will remember the simplicity of true greatness ; the open mind of true wisdom, the meekness of true strength

    它們教導你：在光榮失敗時保持尊嚴，不屈不撓，但是在成功時謙卑溫和；不以空言代替行動；不找尋舒適的小徑，而是面對困難的壓力，以及挑戰的鞭策；學習在暴風雨中屹立，但是對跌倒的人寄與同情；在你想控制別人之前，先控制自己；有純潔的心，有高尚的目標；學習歡笑，但永不忘記如何哭泣；伸向未來，但永不忽略過去；嚴肅，但永不把自己看得過于認真；謙虛，以便你能記得真偉大的單純，真智慧的虛心，真力量的溫馴。
  9. Detailed diagnoses is made on a heavy - hard rain in the northeast qinghai - xizang plateau using ncep data of 1 x 1 with 6h intervals, more complete and integrated conventional observational data and the data set of automatic meteorological stations in plateau and new generation doppler radar data and satellite images and etc. the following conclusions can be drawn : 1. the distribution of heavy - hard rain, which is characteristics of valley topography in northeast qinghai - xizang plateau is obviously effected by topography. the distribution of yearly mean precipitation and the frequencies of heavy - hard rain in this area are descending from east to west

    本文首先利用ncep時間間隔為6小時的1 1的格點資料、更全面、更為完整的常規探測資料和高原地區布設的自動氣象站資料、新一代多卜勒天氣雷達資料、衛星雲圖資料等對高原東北部地區大到暴雨的天氣、氣候特徵及大尺度環流背景進行分析，形成對高原暴雨的整體認識，並為以後的數值模擬提供大尺度環流背景及依據，分析中發現： 1 、高原東北部地區大到暴雨的分佈明顯受到地形影響，年降水量和大到暴雨次數自東向西呈階梯性遞減趨勢，分別在高原東北部的外流河谷地區和四川北部地區存在大值中心。
  10. The analysis of dry pv shows that the high pv dominate the area of typhoon, the higher is the center value of pv, the stronger is the typhoon. lt is also shown that the most important reason resulting in rainstorm is the cold air ( high pv ) which spreads to south from the upper troposphere or lower stratosphere and transports into the warm air. the joining situation of upper and lower pv area make vortex develop. pv transpotation reduces static stability, which increases the releasing of instability energy and makes rainstorm amplify

    對干位渦的分析表明：臺風或臺風環流區為高值位渦區，臺風越強，位渦中心值越大；對流層上部或平流層下部冷空氣（高位渦）的擴散南下與暖濕氣流的交匯是造成特大暴雨的重要原因，因為上游斜壓性的發展使對流層頂發生折疊，平流層與對流層相互作用增強，上下位渦區相接的形勢使低層渦旋發展，上升運動加強，位渦的下傳有效地降低了靜力穩定度，有利於位勢不穩定能量的釋放，使得暴雨增幅。
  11. Using the mm5 model to conduct investigation of numerical simulation for this case, it was basically possessed of a capability to reproduce the genesis, development and evolution of the large - scale and mesoscale weather systems

    本文以mm5模式模擬分析「雅安天漏」為代表，著重研究了不同邊界層參數化方案對雨量中心強度、雨區分佈的影響以及雅安暴雨時的緯向垂直環流結構。
  12. By mesoanalysis of a precipitation that occurred in the middle reaches of the changjiang river, 8th jul. in 2003, the formation and development of the event, its relation with the meso - microscale system are studied, it is emphasized that the low - level jet would cause favorable thermodynamic, moisture and dynamic conditions for the heavy rainfall in the middle reaches of the changjiang river and that the mesoscale vortex formed in the left of the low - level jet would stimulate strong convective clouds and cause the heavy rain

    摘要通過對2003年7月8日發生在長江中游的一場大暴雨進行中尺度分析，初步研究了暴雨的形成及發展過程，總結了暴雨的產生與中小尺度系統的關系，著重闡述了低空急流在暴雨形成中的作用，以及在低空急流左側強正渦度中心附近形成中尺度渦旋，激發暴雨雲團等。
  13. There are always rain and snow in life, thus we have our internal sunshine of hope in our hearts and everything will be fine

    人生中既有暴雨，也有大雪，但只要自己那博大的心胸中常是一片美麗的晴空，常有希望的太陽般存在，就可以了。 - - - - - - - - - - - （日本）池田大作。
  14. Then it rained - and not just a shower, but a typhoon that lasted for days. " it was very hot already. these pouring rains and high winds came on top of that. it was really easy to get lost in worrying about how hot and wet and exhausted i was - and to wonder what i was missing back home on ally mcbeal that week.

    然後他們一行人還遇到連續數日的臺風，她表示：原本已經快熱壞了，又加上狂風暴雨，拖著疲憊的身軀，很容易讓人只會迷失在擔心自己有多熱多濕又多累之中，有時還會去想我錯過了那個星期艾莉的異想世界ally mcbeal的影集。
  15. Rain becomes persistent and winds violent as the centre of the storm draws near

    當風暴中心移近時，雨勢會變得較持續，而風力亦更趨猛烈。
  16. The centre will be closed when typhoon signal no. 8 or above or the black rainstorm signal is hoisted

    號或以上臺風訊號或黑色暴雨警告訊號，資訊中心將會關閉。若正常關閉時間前少於
  17. Faith is born out of complete trust of predestination and believeness that goodness can always overcome the evil. sun still rises even in the strom

    信念始於內心對機緣深信不疑。信念是心底深信善良能戰勝邪惡，太陽會在暴風雨中升起。
  18. Whether in the aspect of total rain days or total rainfall amount in a year, ya ' an is always an extreme range, which has been called " ya - an - tian - lou " in chinese. the predicted average physical structures in the raining process are as follows : ( l ) positive vortex and convergent center in the lower and middle troposphere and negative vortex and divergent center in upper troposphere ; ( 2 ) the superposition of the low layer zonal - vertical circulation and the up layer zonal - vertical circulation forms a strong upward current

    從6種不同方案對暴雨過程預報的實驗看，不同的邊界層參數化方案對雨帶特徵的模擬都具有一定的能力，同時模式模擬的降水對參數化方案的選取是敏感的，不同的參數化方案模擬出的降水范圍和雨量分佈有所差異，主要表現在降雨量中心強度及雨區分佈上。
  19. Mediologist meteorologist dennis feltgen of the national hurricane center in miami said the storm will cause heavy rains and possible flooding as it moves over mountainess mountainous areas

    位於邁阿密的國家颶風中心的氣象專家d . f .表示暴風將帶來強降雨，在經過山地時可能引發洪災。
  20. In this paper, firstly large - scale air circulation and weather system evolution are analyzed, and get the scale feature and spread process of the meso - scale convective system by analyzing time - space layout of precipitation and satellite cloud maps. the lower resolution of t213 model and less time - space resolution of data were responsible for the above mentioned misforecast. in this study, the event is simulated by mm5v3. 6 with two - way - interaction and triple nested grid

    分析並指出了此次過程中對流降水的演變規律：對流活動引起的高層重力波和邊界層冷涌是對流傳播和觸發大暴雨中心對流活動的主要機制，地面冷空氣的侵入，引起邊界層暖濕空氣的交匯和強烈輻合是對流活動顯著加強的原因。
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