cumulonimbus 中文意思是什麼
cumulonimbus
解釋
n. 名詞 【氣象學】積雨雲。-
Cumulonimbus confirm. barometric no hazard
積雨雲已確認。氣壓沒有問題。 -
Becoming between 0600 utc to 0800 utc, scattered cloud at 1500 feet including cumulonimbus cloud and broken cloud at 2000 feet
在0600utc至0800utc之間雲層逐漸轉變,轉變后1500尺有零散雲層,包括積雨雲, 2000尺有疏鬆雲層 -
Temporarily between 0800 utc and 1200 utc surface wind direction 170 degree ( south - southeasterly winds ) ; wind speed 25 knots gusting to 40 knots ; visibility 1000 m in thunderstorm with moderate rain ; scattered cloud at 1000 feet including cumulonimbus cloud and broken cloud at 2000 feet
在0800utc至1200utc之間,地面風向間中為170度(東南偏南風) ,風速25海里小時,陣風達40海里小時;能見度在雷暴及和緩雨勢中為1000米; 1000尺有零散雲層,包括積雨雲, 2000尺有疏鬆雲層 -
Cumulonimbus clouds - their development and dissipation
積雨雲-它的發展及消散 -
Confirm cumulonimbus on the near path. over.
確認附近航線間的積雨雲。完畢。 -
The cumulonimbus formations about which you speak.
你說的這種積雨雲. . -
Most thunderstorms form in cumulonimbus cloud
大多數雷暴由積雨雲組成。 -
The cumulonimbus formations about which you speak
你說的這種積雨雲 -
Mary : that is what ' s called cumulonimbus
瑪麗:那叫積雨雲。 -
Distribution of positive and negative charges inside a cumulonimbus cloud
積雨雲內的正負電荷分佈情況 -
The typical life span of a cumulonimbus cloud is a couple of hours
單塊積雨雲的壽命一般只有一兩小時。 -
Please click here to view pictures of development into a cumulonimbus cloud
請按此處瀏覽積雨雲的發展圖片 -
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。 -
Cumulonimbus capillatus cloud
鬃狀積雨雲 -
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。 -
Occasionally, cumulonimbus clouds merge to form severe thunderstorms called supercells
有些積雨雲更會結合形成特大的強雷暴。 -
Development into a cumulonimbus cloud
積雨雲的發展 -
They are formed in well - developed cumulonimbus clouds associated with thunderstorms, mainly in spring
雹在雷暴中充分發展的積雨雲內生成,主要在春天出現。 -
An unstable atmosphere is favourable for the development of cumulonimbus and hence thunderstorms
不穩定的大氣有利於積雨雲的發展及雷暴的形成。 -
Temporarily between 0800 utc and 1200 utc surface wind direction 170 degree south - southeasterly winds ; wind speed 25 knots gusting to 40 knots ; visibility 1000 m in thunderstorm with moderate rain ; scattered cloud at 1000 feet including cumulonimbus cloud and broken cloud at 2000 feet
在0800 utc至1200 utc之間,地面風向間中為170度東南偏南風,風速25海里小時,陣風達40海里小時能見度在雷暴及和緩雨勢中為1000米1000尺有零散雲層,包括積雨雲, 2000尺有疏鬆雲層
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