雨狀回波 的英文怎麼說

中文拼音 [yǔzhuànghuíbō]
雨狀回波 英文
rain echo
  • 雨 : 雨名詞（從雲層中降向地面的水） rain
  • 狀 : Ⅰ名詞1 （形狀） form; shape 2 （情況） state; condition; situation; circumstances 3 （陳述事件或...
  • 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 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。
  2. 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。
  3. 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。
  4. 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。
  5. 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） 。
  6. 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。
  7. 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。
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