雨回波 的英文怎麼說

中文拼音 [yǔhuíbō]
雨回波 英文
rain echo
  • 雨 : 雨名詞（從雲層中降向地面的水） rain
  • 回 : 回構詞成分。
  • 波 : Ⅰ名詞1 （波浪） wave 2 [物理學] （振動傳播的過程） wave 3 （意外變化） an unexpected turn of even...
  1. The various colours significant of various degrees of vitality white, yellow, crimson, vermilion, cinnabar : their degrees of brilliancy : their magnitudes revealed up to and including the 7th : their positions : the waggoner s star : walsingham way : the chariot of david : the annular cinctures of saturn : the condensation of spiral nebulae into suns : the interdependent gyrations of double suns : the independent synchronous discoveries of galileo, simon marius, piazzi, le verrier, herschel, galle : the systematisations attempted by bode and kepler of cubes of distances and squares of times of revolution : the almost infinite compressibility of hirsute comets and their vast elliptical egressive and reentrant orbits from perihelion to aphelion : the sidereal origin of meteoric stones : the libyan floods on mars about the period of the birth of the younger astroscopist : the annual recurrence of meteoric showers about the period of the feast of s. lawrence martyr, 10 august : the monthly recurrence known as the new moon with the old moon in her arms : the posited influence of celestial on human bodies : the appearance of a star 1st magnitude of exceeding brilliancy dominating by night and day a new luminous sun generated by the collision and amalgamation in incandescence of two nonluminous exsuns about the period of the birth of william shakespeare over delta in the recumbent neversetting constellation of cassiopeia and of a star 2nd magnitude of similar origin but lesser brilliancy which had appeared in and disappeared from the constellation of the corona septentrionalis about the period of the birth of leopold bloom and of other stars of presumably similar origin which had effectively or presumably appeared in and disappeared from the constellation of andromeda about the period of the birth of stephen dedalus, and in and from the constellation of auriga some years after the birth and death of rudolph bloom, junior, and in and from other constellations some years before or after the birth or death of other persons : the attendant phenomena of eclipses, solar and lunar, from immersion to emersion, abatement of wind, transit of shadow, taciturnity of winged creatures, emergence of nocturnal or crepuscular animals, persistence of infernal light, obscurity of terrestrial waters, pallor of human beings

    顯示出不同程度之生命力的繽紛色彩白淺黃深紅朱紅銀朱諸星之亮度一直包括到七等星以等級標志的諸星之大小諸星的位置御夫座沃爾辛厄姆路172大衛的戰車173土星光環螺旋星雲凝固后形成有衛星的恆星群兩重大陽相互依存的旋轉運動伽利略西蒙馬里烏斯174皮亞175勒威耶赫歇耳加勒176等人各自獨立地同時所做的發現波得和開普勒所嘗試的距離的立方與回轉次數的平方的體系化177多毛的眾彗星178那幾殆無限的被壓縮性，以及自近日點至遠日點那廣漠的遠心的重返大氣層的橢圓軌道隕石的恆星之起源年紀較輕的天體觀測者誕生的那個時期火星上所出現的「暗波」現象179每年在聖勞倫斯節殉教者，八月十日前後降落的隕石雨每月都發生的所謂「新月抱舊月」現象180關于天體對人體的影響的假定威廉莎士比亞出生的時期，在斜倚卻永不沒落的仙后座那三角形上端，一顆不分晝夜散發著極亮光彩的星辰一等星出現了181這是兩個無光死滅了的太陽因相撞並汞合為白熱體而形成的燦爛的新太陽大約在利奧波德布盧姆出生時，出現在七星花冠星座里而後又消失了的一顆同一起源亮度卻稍遜的星宿二等星182還有約於斯蒂芬迪達勒斯出生時，出現在仙女座中之後又消失，小魯道爾夫布盧姆出生與夭折數年後出現于御夫座后又消失，以及另外一些人出生或去世前前後後出現在許許多多其他星座中而又消失了的假定是同一起源的實際存在或假定存在的星斗183 。
  2. First, in order to verify the correct of this retrieval month, by using the data of three - dimensional wind field, raininess field and temperature field that are output by mm5 numerical simulation, we climate the radial velocity field and echo intention field in the in - phase observation area of dual - doppler radar, then, on the base of the upwards retrieval theory and using the radial velocity field and echo intention field in the in - phase observation area of dual - doppler radar, we retrieve the atmospheric three - dimensional wind field

    首先，為檢驗此種反演方法的可靠性，我們使用mm5數值模式輸出的三維風場、雨強場、溫度場等數據，分別模擬生成兩部雷達同步觀測區的徑向速度場和回波強度場，然後根據以上的反演理論利用模擬的雙多普勒天氣雷達觀測到的徑向速度場和回波強度場反演出大氣三維風場。
  3. The reflected microwave would give the radar a false impression of rain

    這從地面反射回來的回波會使雷達誤以為是降雨。
  4. The mcc is composite of meso -, meso - and meso - scale convective systems which have different structure and motion features. although circularly approximately on the satellite imagery, the mcc shows linear distributions of radar echo, torrential rain, thunderstorm, cumulonimbus and mesoscale physical parameters as a squall line

    它是中、和尺度對流系統組成的復合體，它在雲圖上近似圓形，其雷達回波、暴雨、雷暴、對流雲、中尺度物理量場等卻呈類似颮線的帶狀分佈。
  5. A distant rain area can sometimes show up on the radar image as " second trip echo "

    遙遠的雨區有時能在雷達圖上顯現成二次傳輸回波。
  6. The one is brought by meeting and overlapping of mixed and high level trough moving eastward cloud systems whose echo depth is about 12 km, and the horizontal distance is within 10 ~ 20km and the intensity is up to about 50dbz

    混合雲團與東移的高空槽雲系相遇並疊置的大到暴雨過程，鑲嵌于回波中的對流單體是造成強降水的直接系統，其尺度只有10 ~ 20km 。
  7. In addition, a thought of how to use the mesoscale convergence center, tbb of convective cloud and the radar echo for rainfall rate to predict the mesoscale rain cluster is presented

    提出利用逐時的中尺度輻合中心、衛星紅外雲圖雲頂亮溫及雷達回波降水率做中尺度雨團量級預測思路。
  8. And such zones act as an important dynamic condition for low - level water transfer and also a favorable environmental condition for " seeding - water supply ". there stronger echoes are detected, meaning that bubble convection develops in the precipitating fields of the clouds that are homogeneous in the main, causing centers of > 10 mm / hr surface rainfall to occur and migrate

    這些不穩定區是低層水汽輸送摘要重要的動力條件，也是「播撒一供應」機制發生的有利的濕熱力環境條件，雲系較強降水回波在這里得到發展，使整體均勻的冷鋒層狀雲系降水場有較強回波帶和對流泡發展，帶來地面有> 10mmlh較強降雨中心產生和移動。
  9. The macro characteristics of status cloud systems have been studied by using every 3 - hour sounding data, satellite cloud pictures, radar echoes, synoptic charts, surface rainfall, raindrop size distribution and microwave radiometer. the spatial distribution of precipitation particles and the mechanisms of their formation were studied by one - dimension stratus model. thus, spring stratus precipitation conceptual model was primarily established in henan province

    利用3小時一次的加密探空資料、衛星雲圖、雷達回波圖、天氣圖、地面雨量、雨滴譜、微波輻射計等資料，分析了降水雲系的宏觀特徵，並利用一維層狀雲模式研究了降水粒子的時空分佈和水質粒形成的微物理特徵，由此初步建立了河南省春季層狀雲降水的概念模型。
  10. Echoes captured by the hong kong observatory weather radar at 6 : 18 a. m. on 4 june 1997 when heavy rain associated with an active trough of low pressure was affecting hong kong

    天文臺氣象雷達於一九九七年六月四日上午六時十八分錄得的雷達回波圖像，當時香港正受一道活躍低壓槽影響而下著大雨。
  11. 5. the heavy - hard rainfall in transitional season is brought by mixed cloud systems whose movements are slow and less, and the echo depth are about 5 km and horizontal distance of strong echo are within 10km

    5 、過渡季節產生的大到暴雨過程大都為混合雲系造成，混合雲系移速慢，位置少動，強回波頂高度skm左右，強回波的水平距離在10km以內。
  12. The radar image upper figure shows that second trip echoes in the form of strips were in fact caused by rain at a distance beyond 400 kilometres to our south lower figure

    雷達圖像上圖顯示二次傳輸回波呈條帶狀，但這實際上是由本港以南400公裡外的一個雨區所引致的見下圖。
  13. The radar image ( upper figure ) shows that second trip echoes in the form of strips were in fact caused by rain at a distance beyond 400 kilometres to our south ( lower figure )

    雷達圖像（上圖）顯示二次傳輸回波呈條帶狀，但這實際上是由本港以南400公裡外的一個雨區所引致的（見下圖） 。
  14. The bottom image of reflectivity which provides estimation of the rain intensity depicts the hook - shaped characteristic of the storm. this is another typical signature of tornado

    下圖為反射率表示估計的降雨強度圖像，顯示出該風暴出現了狀回波，這是卷風另一典型特徵。
  15. The bottom image of reflectivity ( which provides estimation of the rain intensity ) depicts the hook - shaped characteristic of the storm. this is another typical signature of tornado

    下圖為反射率（表示估計的降雨強度）圖像，顯示出該風暴出現了?狀回波，這是龍卷風另一典型特徵。
  16. In figure 8, a vertical cross - section of the intense rain echoes to the immediate west of chek lap kok corresponding to a vertical cut from point a to point b in figure 7 indicates that the rainstorm extended to as high as 14 km above the ground level

    圖八顯示赤角西側強勁回波的垂直切面對應圖七a點至b點的垂直切面，可見暴雨的對流發展高至14千米高空。
  17. In figure 8, a vertical cross - section of the intense rain echoes to the immediate west of chek lap kok ( corresponding to a vertical cut from point a to point b in figure 7 ) indicates that the rainstorm extended to as high as 14 km above the ground level

    圖八顯示赤?角西側強勁回波的垂直切面（對應圖七a點至b點的垂直切面） ，可見暴雨的對流發展高至14千米高空。
  18. Figure 7 depicts a radar image of rain echoes at 3 km above ground level taken from the weather radar at tai mo shan at 3 a. m. it revealed a broad band of rain lying across the territory with intense rain echoes in yellow and red covering chek lap kok and the new territories

    圖七是大帽山氣象雷達于凌晨3時顯示的3千米高空雨雲影像。圖中可見香港被一條廣闊的雨帶幅蓋，其中赤角和新界上空的回波尤其強勁以黃色和紅色顯示。
  19. Figure 7 depicts a radar image of rain echoes at 3 km above ground level taken from the weather radar at tai mo shan at 3 a. m. it revealed a broad band of rain lying across the territory with intense rain echoes ( in yellow and red ) covering chek lap kok and the new territories

    圖七是大帽山氣象雷達于凌晨3時顯示的3千米高空雨雲影像。圖中可見香港被一條廣闊的雨帶幅蓋，其中赤?角和新界上空的回波尤其強勁（以黃色和紅色顯示） 。
  20. Thirdly, two location data sets of rain - gauge networks have been analyzed by fractal theory. the results show that the increase in the measuring capability of a network must occur through its enlargement resulting in the fractal dimension increase

    第二部分用分形理論討論了雨量站分佈的不規則性，並對雷達回波的分維數計算進行了初步探討。
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