高雨雲 的英文怎麼說

中文拼音 [gāoyǔyún]
高雨雲 英文
altonimbus
  • 高 : Ⅰ形容詞1 （從下向上距離大; 離地面遠） tall; high 2 （在一般標準或平均程度之上; 等級在上的） above...
  • 雨 : 雨名詞（從雲層中降向地面的水） rain
  • 雲 : Ⅰ動詞[書面語] （說） say Ⅱ名詞1. （雲彩） cloud 2. （雲南） short for yunnan province3. （姓氏） a surname
  1. Under the ceaseless conflagration of lightning that flamed in the skies, everything below stood out in clean - cut and shadowless distinctness : the bending trees, the billowy river, white with foam, the driving spray of spume - flakes, the dim outlines of the high bluffs on the other side, glimpsed through the drifting cloud - rack and the slanting veil of rain

    這時候，天空中風雨閃雷交加，狂暴至極。閃電把天空也照亮了，把天宇下的萬物映襯得分外鮮明被風吹彎的樹木白浪翻騰的大河大片隨風飛舞的泡沫以及河對岸高聳的懸崖峭壁的模糊輪廓，都在那飛渡的亂雲和斜飄的雨幕中乍隱乍現。
  2. Request higher level due to cb and turbulence

    請求上升高度層，因雷雨雲和顛簸。
  3. Thermometers, barometers, raingauges and a ceilometer are set up in a meteorological enclosure near the air traffic control tower to provide temperature, pressure, rainfall and cloud base information for the aerodrome

    航空交通管制塔附近則設置了溫度表、氣壓表、量雨器及雲冪儀以提供機場的氣溫、氣壓、雨量及雲底高度的資料。
  4. The mechanism of the downburst formation was also investigated based on the cloud microphysics of the simulated storm and it was found that this downburst was primarily produced by hail loading, and enhanced by hail melting and rain evaporation. and the loading and the melting of hail played a very important role in producing the downburst. the gale at the surface was caused by the severe downburst

    從雲微物理學角度分析了此次局地性大風的形成原因，認為由高空冰雹粒子的拖曳產生的負浮力作用是促發強下沉氣流產生的主要原因，其次是冰雹的融化和雨水蒸發冷卻對下沉氣流起加速作用，冰雹的拖曳和融化作用對下沉氣流具有決定性的作用。
  5. The simulative cloud image, made from the mixing ratios of cloud liquid water, rain water, ice crystal, snow, graupel which were outputted by the mesoscale model mm5, resemble the gms satellite infrared image very well and also show the cloud evolution of typhoon winnie from tropical cyclone to extratropical cyclone after landing

    利用高解析度中尺度數值模式輸出的大氣中雲水冰水雨水雪水成功地模擬出1997年登陸臺風winnie的雲系結構。模擬雲圖與氣象衛星實際觀測的臺風雲圖非常相似。由於模擬雲圖可以給出大氣中不同形態水物質的三維空間分佈，彌補了衛星只能觀測雲頂表面的不足。
  6. The low latitude systems such as typhoon, etc. affect the rainstorm in plateau through direct and indirect action. the synoptic systems within heavy - hard rainfall stagnated in the most of this area. 4

    4 、高原東北部地區大到暴雨的雲圖特徵大都為不同性質雲系的疊置，可為高原及其鄰近地區的暴雨預報提供重要的依據。
  7. The great bell of saint paul s was striking one in the cleared air, when mr. lorry, escorted by jerry, high - booted. and bearing a lantern, set forth on his return - passage to clerkenwell

    聖保羅大教堂的大鐘在雲收雨散的空中敲了一點，羅瑞先生才在腳穿高統靴手拿風燈的傑瑞陪同下動身回克拉肯威爾去。
  8. The hydrometeors distribution in mcc illustrat that the precipitable ice is dominant which fills in the cloud cluster in almost entire troposphere with maximum cores at the mid - levels. rain water and cloud liquid water are in the middle and lower troposphere, and cloud ice water only scatters at the 8 - 18km upper levels

    水凝物垂直分佈顯示， mcc中可降水冰含量最大，分佈在幾乎整個對流層，雨水和雲水主要分佈在的對流層中、低層，而雲冰則分佈於高層大氣中。
  9. Three - dimensional high - density space / time soundings serve as the main body of data consisting of 3 - hr interval doppler probings, 10 - 30 min rainfall intensity, surface raindrop sizes sampling and gps - guided flight cloud physics detections with output taken at 2 - sec and 200 - m intervals. and specific systems associated therewith are developed for multiple - way communication and data collection and storage, a platform for analysis, retrieval softwares for dominant items and multi - scale cloud models - all constitute a system of techniques for meso to microscale observations and analysis. 2 ) atmospheric water resource and macroscopic rainfall properties in dry periods of spring and autumn of the target region

    以加密觀測的多普勒雷達、 3小時探空、 10 30分鐘雨強、地面雨滴譜等間隔取樣及在gps引導下的飛機雲物理探測等獲取的三維高時空密度的綜合探測為主體；配合專項設計開發的多路通訊採集存貯系統、多類信息的分析處理平臺、主要觀測項目的分析反演軟體，結合多尺度雲系模式，綜合構成層狀雲系中微尺度探測和分析處理技術方法。
  10. Fig. 7 rain echoes at 3 km above ground level taken from the weather radar at tai mo shan at 3 a. m. on 3 april 2000

    圖七於二零零零年四月三日凌晨3時，大帽山氣象雷達顯示的3千米高空雨雲影像。
  11. Type of medium clouds : ac, as, ns

    -中云云屬：高積雲，高層雲，雨層雲
  12. If the cumulus continues to grow, its top will become very bright in the late stage, looking like a cabbage and reaching a height beyond 10, 000 m. by then it is called cumulonimbus

    若雲塊進一步繼續發展，到了後期，雲的頂部發白炫目，外觀如椰菜花，高度可達一萬米以上，便成為積雨雲。
  13. J. cloud height above msl : few 1500 ft sct 3500 ft bkn 8000 ft tempo few cb 800 ft sct 1200 ft bkn 4000 ft k. visibility : 10 km tempo 3000 m in showers, 1500m in thunderstorms l. 0 deg

    四雲量及雲底高度:少雲1500英尺疏雲3500英尺裂雲8000英尺間中少雲積雨雲800英尺疏雲1200英尺裂雲4000英尺五能見度: 10公里，有驟雨時可低至3000米。
  14. This is mostly due to higher temperatures and reduced cloudiness and precipitation over europe and it leads to a higher number of ozone events exceeding information and warning thresholds

    最大可能原因為高溫、雲量降低及雨量下降而導致臭氧濃度超過標準。
  15. It will use radar, balloons and aircraft to look at the role of another sort of high - altitude cloud : cirrus clouds, which get spun off the tops of storms

    該工程將使用雷達、熱氣球與大氣層飛行器來研究另一種高端雲的作用，其名為捲雲它是在暴風雨出現時從其頂端意外形成的。
  16. Through this web page, the public can get to know how weather elements such as temperature, humidity, pressure, cloud height, rainfall and visibility are measured

    透過這個網頁，市民可了解天文臺如何測量風溫度、濕度、氣壓、雲高、雨量、能見度等氣象元素。
  17. Because of the existence of meiyu precipitating cloud band the temperature dv is faint inside the meiyu trough and on account of large - scale prominent terrain available, significant temperature dv occurs on both sides of the trough, leading to the reinforcement of the subtropical high and middle latitude transformed high, and the deepening and narrowing of the trough in the night with the result that the relative intensity and precipitating function of the meiyu frontal rainfall system are changed at day and night, resulting in precipitation dv

    由於梅雨雲帶的存在，梅雨鋒低壓槽內溫度日變化很微弱；由於梅雨系統四圍高大地形的存在，梅雨鋒低壓槽南北兩側溫度日變化非常明顯，使南海副高和中緯度變性高壓在夜間增強，梅雨鋒低壓槽也在夜間變深、變窄，改變了早、晚時刻梅雨系統的相對強度和降水功能，導致降水日變化。
  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. A cumulonimbus cloud typically covers an area of a few kilometres in diameter with a vertical extent of ten kilometres or more, like a tower hanging in the sky

    每塊積雨雲覆蓋范圍一般直徑只有數公里，高度約十餘公里，遠看就如空中的一座塔。
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